<?xml version='1.0' encoding='UTF-8'?><?xml-stylesheet href="http://www.blogger.com/styles/atom.css" type="text/css"?><feed xmlns='http://www.w3.org/2005/Atom' xmlns:openSearch='http://a9.com/-/spec/opensearchrss/1.0/' xmlns:georss='http://www.georss.org/georss'><id>tag:blogger.com,1999:blog-1010569638007681966</id><updated>2009-09-22T03:12:38.936-07:00</updated><title type='text'>FUNOLOGY</title><subtitle type='html'></subtitle><link rel='http://schemas.google.com/g/2005#feed' type='application/atom+xml' href='http://priyameena.blogspot.com/feeds/posts/default'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/1010569638007681966/posts/default'/><link rel='alternate' type='text/html' href='http://priyameena.blogspot.com/'/><link rel='hub' href='http://pubsubhubbub.appspot.com/'/><author><name>priyanka gupta</name><uri>http://www.blogger.com/profile/03282159976818127425</uri><email>noreply@blogger.com</email></author><generator version='7.00' uri='http://www.blogger.com'>Blogger</generator><openSearch:totalResults>17</openSearch:totalResults><openSearch:startIndex>1</openSearch:startIndex><openSearch:itemsPerPage>25</openSearch:itemsPerPage><entry><id>tag:blogger.com,1999:blog-1010569638007681966.post-5018120355868809930</id><published>2008-08-26T00:55:00.000-07:00</published><updated>2008-08-26T00:56:49.490-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='internet hacking'/><category scheme='http://www.blogger.com/atom/ns#' term='hacking crime'/><category scheme='http://www.blogger.com/atom/ns#' term='hacking'/><category scheme='http://www.blogger.com/atom/ns#' term='hackers'/><title type='text'>What is hacking?</title><content type='html'>HACKING !&lt;br /&gt;&lt;br /&gt;&lt;br /&gt;What is hacking?&lt;br /&gt;Hacking can be defined as the process of gaining unauthorised access to a computer or computerised system and the information it contains. Both corporate and home users can be at risk of hacking.&lt;br /&gt;What are the risks to home users?The risk to home users from hacking is growing. Until recently, the use of conventional dial-up modems meant that users tended to be connected to the Internet for relatively short periods of time. However, broadband and cable connections, through which systems can be permanently connected to the Internet, make it easier for hackers to be aware of your presence online and attempt to gain access to your system. Faster connections can also make it easier to transfer information from your system very quickly. Some viruses are known as ‘Trojan Horses’ or ‘Trojans’. Once installed these will open a ‘back door’ to your computer and notify the sender. The sender can then access your computer and open, delete or copy files from it without your knowledge.&lt;br /&gt;In addition, an increasing number of programmes, such as real-time chat applications, act as servers to exchange information online. Your system needs to 'open up' more of its resources to the Internet to do this, which can make it more vulnerable.&lt;br /&gt;What can home users do?There are several steps you can take to help protect your computer and the information it contains:&lt;br /&gt;Use a "firewall", a piece of hardware or software that blocks unauthorised access to your system. Software versions can be found on the Internet, and many computer magazines feature software in their cover CDs.&lt;br /&gt;Don’t leave any files that contain sensitive information – for example, your bank details - where they could easily be found by someone hacking your system.&lt;br /&gt;Make sure you are running the latest versions of any software that acts as a server.&lt;br /&gt;Remember as long as your system is switched on and connected to the Internet, it could be at risk of being hacked. You don’t have to actively be using your system for it to be vulnerable.&lt;br /&gt;As with other Internet crimes, the best cure is prevention. If you have been the victim of a hacker you may not realise until any sensitive information stored on your system has been put to use.&lt;br /&gt;Corporate, business and public sector usersThe risk to businesses and the public sector is high, as the sensitive nature of information held on their computer systems makes them an attractive target for hackers. This makes the use of security technology paramount. Companies should consider the use of dedicated firewall hardware as well as software. They should look at the ways in which the outside can gain access to their network, and ensure that their systems are not using installed default system passwords etc. Organisations dealing with this area include:&lt;br /&gt;Local police forces, who now work in conjunction with the &lt;a onclick="disclaimer()" href="http://www.nationalcrimesquad.police.uk/nhtuc/nhtcu.html" target="_blank"&gt;National High-Tech Crime Unit&lt;/a&gt; (NHTCU)&lt;br /&gt;&lt;a onclick="disclaimer()" href="http://www.uniras.gov.uk/index.html" target="_blank"&gt;Unified Incident Reporting and Alert Scheme&lt;/a&gt; (UNIRAS). This scheme's purpose is to ensure the integrity of government, public service and infrastructure-related systems. However, its alerts and briefings are also available to users outside the UNIRAS community, which also welcomes reports of significant threats and vulnerabilities.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/1010569638007681966-5018120355868809930?l=priyameena.blogspot.com'/&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://priyameena.blogspot.com/feeds/5018120355868809930/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='https://www.blogger.com/comment.g?blogID=1010569638007681966&amp;postID=5018120355868809930' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/1010569638007681966/posts/default/5018120355868809930'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/1010569638007681966/posts/default/5018120355868809930'/><link rel='alternate' type='text/html' href='http://priyameena.blogspot.com/2008/08/what-is-hacking.html' title='What is hacking?'/><author><name>priyanka gupta</name><uri>http://www.blogger.com/profile/03282159976818127425</uri><email>noreply@blogger.com</email><gd:extendedProperty xmlns:gd='http://schemas.google.com/g/2005' name='OpenSocialUserId' value='11703516926278611720'/></author><thr:total xmlns:thr='http://purl.org/syndication/thread/1.0'>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-1010569638007681966.post-2620409670036208769</id><published>2008-08-26T00:50:00.000-07:00</published><updated>2008-08-26T00:52:25.618-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='internet hacking'/><category scheme='http://www.blogger.com/atom/ns#' term='hacking'/><category scheme='http://www.blogger.com/atom/ns#' term='hackers'/><title type='text'>INTERNET HACKING .</title><content type='html'>INTERNET HACKING .&lt;br /&gt;Netspionage Costing Billions.&lt;br /&gt;&lt;br /&gt;Two years ago, a fifteen-year-old boy logged onto the Internet under the alias 'Comrade'. To some of us, our idea of hacking might include breaking into an email account or viewing confidential company information. However, no one expected that 'Comrade' would cause a three-week shutdown at NASA, steal government email passwords, intercept over 3000 emails and download close to $2 million worth of software used to operate the international space station. If that was not shocking enough, he had twice gained access to the computers used by the Pentagon to monitor threats of nuclear and biological warfare.&lt;br /&gt;Computer hacking has been around for as long as we can remember - certainly as long as we have had a World Wide Web. Occasionally, the news speaks of silly pranks which imply nothing more than a temporary shutdown of a website, although 'Comrades' hack forced a three-week shutdown for repairs and cost the U.S. government $41,000.Recently, the case of the hackers tampering with the CIA's website, changing the title to 'Central Stupidity Agency' and filling it with obscenities was merely a nuisance for the agency. It posed no real threat because the CIA's files are inaccessible via that Internet site. Undoubtedly, there are some who see humour in this - a civilian, probably not even a professional, outwitting an elite US agency. Then there are more serious crimes, which are no laughing matter.In one case of corporate espionage, two 'heavy manufacturing' firms were bidding on a $900 million contract; one outbid the other by a fraction of a percent.This was no co-incidence as the losing company later discovered that someone had broken into the company's computer network and accessed files that contained bidding strategy information.In another case, authorities are chasing an individual who regularly hires U.S. teens to access confidential documents. One young hacker was paid $1,000 - and promised $10,000 more - for stealing design documents for kitchen appliances from U.S. firms.Beyond selling the trade secrets to a company's competition, some hackers resort to extortion of the company. In Sweden, a 15 and 17 year old tried to extort $2 million from a cellular company to destroy information they had illegally downloaded.Like most cases of extortion, the criminal's identity is especially difficult to trace and is magnified because of the nature of the Net.When the Internet was gaining immense popularity, businesses were scrambling to secure domain names and using the technology to expand their market. Seeing e-commerce as an untapped goldmine, many were eagerly diving headfirst into a slew of problems, including security breaches.Companies like eBay, Buy.com, Yahoo! Amazon and Excite were not prepared when 'Mafiaboy' decided to strike. The 16-year-old Montreal teen crippled their sites last year when he bombarded them with thousands of simultaneous messages, preventing legitimate users from gaining access. His five-day tirade caused an estimated $1.7 billion in damages.These malicious and insidious attacks threaten security and cost companies and organizations billions of dollars. A survey of the Fortune 1000 companies in 1999 estimates a loss of $45 billion from information theft.Of course, many organizations are taking extra security measures, including the usage of firewalls (a security mechanism that allows limited access to sites from the Internet).Still, hackers will gain access. If a fifteen year old can shutdown NASA, what hope is there?Recently, Ernst &amp;amp; Young, a major consulting and accounting firm, set up computer labs across North America which allow information security consultants to perform 'ethical hacks' to assess the strengths and weaknesses of a client's networks and systems.By using existing hacker tools, they're fighting fire with fire.'Ethical hackers' are being paid thousands of dollars to provide clients with clear evidence of how vulnerable their networks are to attacks that could compromise their most sensitive information.This is proving an effective way of gauging the level of security within a system.Hacking has become so prevalent that it is almost synonymous with the computer subculture. This "computer geek" culture is portrayed on television (X-files, the Lone Gunmen) and in movies (Hackers, Anti-Trust) as cynical and often self-righteous.With that, there is a sense of rebellion against big business; the proverbial David struggling against a corporate Goliath. In many of these crimes, people do them to defy corporations or the government; money is not always the motive. However, it is an act that is still unacceptable that victimizes all who use the Internet. Viruses, shutdowns, crashes and email hacking will be the burden of the user, a company's money lost to theft will be the burden of its customers and a government's money spent on security will be the burden of its citizens.Is there anyone not affected by Internet crime? Nope.&lt;br /&gt;AntiVirus software is a good start to protecting yourself and your data&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/1010569638007681966-2620409670036208769?l=priyameena.blogspot.com'/&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://priyameena.blogspot.com/feeds/2620409670036208769/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='https://www.blogger.com/comment.g?blogID=1010569638007681966&amp;postID=2620409670036208769' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/1010569638007681966/posts/default/2620409670036208769'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/1010569638007681966/posts/default/2620409670036208769'/><link rel='alternate' type='text/html' href='http://priyameena.blogspot.com/2008/08/internet-hacking.html' title='INTERNET HACKING .'/><author><name>priyanka gupta</name><uri>http://www.blogger.com/profile/03282159976818127425</uri><email>noreply@blogger.com</email><gd:extendedProperty xmlns:gd='http://schemas.google.com/g/2005' name='OpenSocialUserId' value='11703516926278611720'/></author><thr:total xmlns:thr='http://purl.org/syndication/thread/1.0'>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-1010569638007681966.post-8929885857639108968</id><published>2008-08-26T00:36:00.000-07:00</published><updated>2008-08-26T00:45:55.922-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='mobile hazard'/><category scheme='http://www.blogger.com/atom/ns#' term='handset'/><category scheme='http://www.blogger.com/atom/ns#' term='mobile phone'/><category scheme='http://www.blogger.com/atom/ns#' term='iphone'/><category scheme='http://www.blogger.com/atom/ns#' term='hacking'/><title type='text'>Death from the mailroom – iPhone hacks your company from the inside.</title><content type='html'>Death from the mailroom – iPhone hacks your company from the inside.&lt;br /&gt;&lt;a title="PDF" onclick="window.open('http://www.tgdaily.com/index2.php?option=com_content&amp;amp;do_pdf=1&amp;amp;id=38814','win2','status=no,toolbar=no,scrollbars=yes,titlebar=no,menubar=no,resizable=yes,width=640,height=480,directories=no,location=no'); return false;" href="http://www.tgdaily.com/index2.php?option=com_content&amp;amp;do_pdf=1&amp;amp;id=38814" target="_blank"&gt;&lt;/a&gt;&lt;br /&gt;Las Vegas (NV) – The Apple iPhone is great for phone calls and viewing YouTube videos, but it can also be turned into one heck of a wireless hacking tool capable of wrecking havoc on almost any company or government organization from the inside.  In a talk at the Defcon security convention, Robert Graham and David Maynor of Errata Security explained how they could defeat firewalls, intrusion detection systems and even armed security guards by Fedexing a modified iPhone to a fictitious employee.   The phone calls home every hour and can then be instructed to sniff network traffic, discover nearby wireless devices and even download information.&lt;br /&gt;Robert Graham, co-founder and CTO of Errata Security&lt;br /&gt;Graham and Maynor first came up with the idea of the hacking iPhone when a client wanted them to perform a wireless penetration test at a faraway facility.  Graham told TG Daily that such a test would have required costly travel and losing nearly a day sitting in airports and on a plane.  The simpler way seemed to send them an iPhone with special scanning tools installed.Installing the software wasn’t the biggest problem as you can pretty much do anything to the phone after you jailbreak it.  Graham and Maynor had to figure out how to power the phone for several days as it crisscrossed the United States.  They also had to figure out how to control the phone from anywhere in the United States because the phone’s IP address would constantly change as it traversed cell towers and wireless access points on its journey.An APC extended battery pack fixed the power issue by providing approximately five days of power in a deck of cards form factor.  Graham and Maynor solved the control issue by having the phone call home every hour with an SSH connection.  Once connected, the pair could instruct the phone to launch wireless sniffing tools like Graham’s Ferret which enumerates nearby computers and all the hotspots they’ve connected to recently.The phone and the APC battery fit inside the original iPhone box which worked out great for Maynor as he walked to the local UPS store to ship the unit.  “I just told people that someone won an eBay auction for an iPhone,” he joked.In initial runs, the iPhone’s scanning showed some interesting results.  Graham told the audience that the phone would just sit in a receiving facility, usually a mailroom, for a long time.  Fedex and UPS generally will deliver numerous boxes in a shipment and then a secretary or internal mailman (in larger companies) will then sort everything to its final destination.  But if the package is addressed to someone who doesn’t work at the company, then employees will have no real urge to move it.  Calls need to be made to verify that the employee doesn’t exist and then someone will finally call the shipping company to pick the package – this all takes time, time that the phone can use to scan the internal network.Once the phone was inside a business, Graham said most of the wireless networks were wide open.  This should probably come as no surprise as companies usually trust employees and anyone’s who has made it past the front door must be friendly.While the notion of an iPhone attack may seem a bit too Hollywood-ish to some, Graham and Maynor say the idea is much better than a hacker sitting outside of a company sniffing for wireless traffic.  They say police and even average citizens are quite suspicious of people sitting in their cars with glowing computers screens.  Furthermore sending a company an iPhone means you can completely anonymous with a jailbroken iPhone and a third-party SIM card.Companies typically spend thousands even millions of dollars on physical and network security, but Maynor said their iphone can foil all of that by “getting past all the firewalls and crap that they’re buying.”  He added that many organizations have armed guards that will stop any intruders, yet they let in the Fedex guy at 10 AM every morning.Graham was scheduled to demonstrate the sniffing software and promises to release it as open source in the near future.  Unfortunately Graham and Maynor weren’t able to demonstrate the software because they accidentally left the prototype in a Las Vegas cab.  “Some cabbie now has the power to take down the CIA,” Graham joked.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/1010569638007681966-8929885857639108968?l=priyameena.blogspot.com'/&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://priyameena.blogspot.com/feeds/8929885857639108968/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='https://www.blogger.com/comment.g?blogID=1010569638007681966&amp;postID=8929885857639108968' title='1 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/1010569638007681966/posts/default/8929885857639108968'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/1010569638007681966/posts/default/8929885857639108968'/><link rel='alternate' type='text/html' href='http://priyameena.blogspot.com/2008/08/death-from-mailroom-iphone-hacks-your.html' title='Death from the mailroom – iPhone hacks your company from the inside.'/><author><name>priyanka gupta</name><uri>http://www.blogger.com/profile/03282159976818127425</uri><email>noreply@blogger.com</email><gd:extendedProperty xmlns:gd='http://schemas.google.com/g/2005' name='OpenSocialUserId' value='11703516926278611720'/></author><thr:total xmlns:thr='http://purl.org/syndication/thread/1.0'>1</thr:total></entry><entry><id>tag:blogger.com,1999:blog-1010569638007681966.post-8834272539576533945</id><published>2008-08-26T00:26:00.000-07:00</published><updated>2008-08-26T00:36:17.831-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='mobile hazard'/><category scheme='http://www.blogger.com/atom/ns#' term='handset'/><category scheme='http://www.blogger.com/atom/ns#' term='mobile phone'/><category scheme='http://www.blogger.com/atom/ns#' term='iphone'/><title type='text'>Nine Hacks That Will Make You the Master of Your IPhone.</title><content type='html'>Nine Hacks That Will Make You the Master of Your IPhone.&lt;br /&gt;&lt;br /&gt;Only a few days after the iPhone went on sale, hackers were already kicking the wheels and checking under the hood to see if they could pimp out Apple's locked-down smartphone. After a month, they've made surprising progress. Below, we detail some of the milestone hacks for what has been called "the most significant consumer electronics product ever."&lt;br /&gt;Department of Continuous Improvement&lt;br /&gt;Corrections? Additions? Edit this article in the &lt;a href="http://howto.wired.com/wiredhowtos/index.cgi?page_name=nine_hacks_that" action="'display;category="&gt;Wired How To Wiki&lt;/a&gt;.&lt;br /&gt;Most of the hacks that have been publicized so far are aimed at controlling or enhancing your own iPhone, but a darker side has emerged too. A security firm announced a possible Wi-Fi-based &lt;a href="http://blog.wired.com/gadgets/2007/07/attack-hack-com.html"&gt;browser exploit&lt;/a&gt;, which could give hackers access to an iPhone's microphone, surfing history and contact information -- and possibly website and e-mail passwords stored on the phone, too. Make no mistake: The iPhone is a magnet for hackers, both good and bad.&lt;br /&gt;The hacks below run the gamut from easy hacks almost anyone can do to advanced mods that require serious hardware and software skills. Proceed at your own risk: With any hack, there is a chance you could permanently damage your iPhone or render it unusable, and you're almost certainly voiding your warranty if you try most of these hacks. You have been warned.&lt;br /&gt;Activate the IPhone Without AT&amp;amp;T Ordinarily, the iPhone needs to be activated from within iTunes and registered with the carrier, AT&amp;amp;T, before it can be used for anything except telling the time and calling 911. Jon Lech Johansen (aka "DVD Jon"), who is notorious for cracking the CSS protection scheme on DVDs, took only five days to write a program that can bypass the activation step. It's called Phone Activation Server 1.0. Of course, if you don't have an AT&amp;amp;T account, the phone part won't work, but this hack does get you Wi-Fi, web surfing, e-mail and music capabilities. Difficulty: Medium Details: &lt;a href="http://blog.wired.com/gadgets/2007/07/dvd-jon-hacks-i.html"&gt;DVD Jon Hacks iPhone: No Activation Required&lt;/a&gt;&lt;br /&gt;Use the IPhone with a Business or Prepaid Account Once the iPhone has been activated, it is possible to substitute the supplied AT&amp;amp;T SIM with another AT&amp;amp;T or Cingular SIM. Why would you do this? If you already have an account with AT&amp;amp;T, you can transfer it to your iPhone by dropping in your old phone's SIM card. This hack will let you use a business account (otherwise not available for the iPhone) or a pre-paid account with your iPhone. Another way to get a prepaid account for your iPhone is to fake bad credit. Here's how: During activation, keep entering a bogus Social Security number and eventually iTunes will give up and offer you a pre-pay account. Sweet. (The same trick also works if you actually do have bad credit and use your real Social Security number.) Difficulty: Beginner Details: &lt;a href="http://www.reghardware.co.uk/2007/07/20/iphone_unlocked/"&gt;Hackers Saw Through IPhone AT&amp;amp;T Shackles&lt;/a&gt;&lt;br /&gt;Play Tilt Tilt is a game which takes advantage of the iPhone's tilt sensors, the things which cause the display to flip when you change the orientation of the handset. Developer Joe Hewitt &lt;a href="http://www.xeodesign.com/tiltstory.html"&gt;created Tilt&lt;/a&gt; at iPhoneDev Camp, and the game involves tilting the phone to control the main character, Flip, and help him eat falling leaves and butterflies. It's no Wii Tennis, but it is a nice demonstration of the iPhone's innovative controls. Difficulty: Beginner Details: &lt;a href="http://www.xeodesign.com/games/tilt/"&gt;Play Tilt on your iPhone&lt;/a&gt;&lt;br /&gt;Store Files on Your IPhone IPhoneDrive is a graphical file transfer tool for the iPhone. Just hook the phone up to your Mac and you can drag and drop files to and from the iPhone, using it as an external hard drive the way God intended. Why on earth Apple didn't include this feature from the start is a mystery, since every other iPod already has a similar capability. IPhoneDrive costs $10. Difficulty: Beginner Details: &lt;a href="http://ecamm.com/mac/iphonedrive/"&gt;iPhoneDrive Product Page&lt;/a&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/1010569638007681966-8834272539576533945?l=priyameena.blogspot.com'/&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://priyameena.blogspot.com/feeds/8834272539576533945/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='https://www.blogger.com/comment.g?blogID=1010569638007681966&amp;postID=8834272539576533945' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/1010569638007681966/posts/default/8834272539576533945'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/1010569638007681966/posts/default/8834272539576533945'/><link rel='alternate' type='text/html' href='http://priyameena.blogspot.com/2008/08/nine-hacks-that-will-make-you-master-of.html' title='Nine Hacks That Will Make You the Master of Your IPhone.'/><author><name>priyanka gupta</name><uri>http://www.blogger.com/profile/03282159976818127425</uri><email>noreply@blogger.com</email><gd:extendedProperty xmlns:gd='http://schemas.google.com/g/2005' name='OpenSocialUserId' value='11703516926278611720'/></author><thr:total xmlns:thr='http://purl.org/syndication/thread/1.0'>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-1010569638007681966.post-8877076296103247086</id><published>2008-05-13T08:07:00.000-07:00</published><updated>2008-05-13T08:18:46.548-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='earth earthquake tsunami'/><title type='text'>EARTHQUAKE</title><content type='html'>EARTHQUAKE&lt;br /&gt;&lt;br /&gt;This article is about the natural seismic phenomenon. For other uses, see &lt;a title="Earthquake (disambiguation)" href="http://en.wikipedia.org/wiki/Earthquake_%28disambiguation%29"&gt;Earthquake (disambiguation)&lt;/a&gt;.&lt;br /&gt;An earthquake is the result of a sudden release of energy in the &lt;a title="Earth" href="http://en.wikipedia.org/wiki/Earth"&gt;Earth&lt;/a&gt;'s &lt;a title="Crust (geology)" href="http://en.wikipedia.org/wiki/Crust_%28geology%29"&gt;crust&lt;/a&gt; that creates &lt;a title="Seismic wave" href="http://en.wikipedia.org/wiki/Seismic_wave"&gt;seismic waves&lt;/a&gt;. Earthquakes are recorded with a &lt;a title="Seismometer" href="http://en.wikipedia.org/wiki/Seismometer"&gt;seismometer&lt;/a&gt;, also known as a seismograph. The &lt;a title="Moment magnitude scale" href="http://en.wikipedia.org/wiki/Moment_magnitude_scale"&gt;moment magnitude&lt;/a&gt; of an earthquake is conventionally reported, or the related and mostly obsolete &lt;a title="Richter magnitude scale" href="http://en.wikipedia.org/wiki/Richter_magnitude_scale"&gt;Richter&lt;/a&gt; magnitude, with magnitude 3 or lower earthquakes being mostly imperceptible and magnitude 7 causing serious damage over large areas. Intensity of shaking is measured on the modified &lt;a title="Mercalli intensity scale" href="http://en.wikipedia.org/wiki/Mercalli_intensity_scale"&gt;Mercalli scale&lt;/a&gt;.&lt;br /&gt;At the Earth's surface, earthquakes manifest themselves by a shaking and sometimes displacement of the ground. When a large earthquake &lt;a title="Epicenter" href="http://en.wikipedia.org/wiki/Epicenter"&gt;epicenter&lt;/a&gt; is located offshore, the seabed sometimes suffers sufficient displacement to cause a &lt;a title="Tsunami" href="http://en.wikipedia.org/wiki/Tsunami"&gt;tsunami&lt;/a&gt;. The shaking in earthquakes can also trigger landslides and occasionally volcanic activity.&lt;br /&gt;In its most generic sense, the word earthquake is used to describe any seismic event—whether a natural &lt;a title="Phenomenon" href="http://en.wikipedia.org/wiki/Phenomenon"&gt;phenomenon&lt;/a&gt; or an event caused by humans—that generates &lt;a title="Seismic wave" href="http://en.wikipedia.org/wiki/Seismic_wave"&gt;seismic waves&lt;/a&gt;. Earthquakes are caused mostly by rupture of geological faults, but also by volcanic activity, landslides, mine blasts, and nuclear experiments.&lt;br /&gt;An earthquake's point of initial rupture is called its &lt;a class="mw-redirect" title="Focus (earthquake)" href="http://en.wikipedia.org/wiki/Focus_%28earthquake%29"&gt;focus&lt;/a&gt; or &lt;a title="Hypocenter" href="http://en.wikipedia.org/wiki/Hypocenter"&gt;hypocenter&lt;/a&gt;. The term &lt;a title="Epicenter" href="http://en.wikipedia.org/wiki/Epicenter"&gt;epicenter&lt;/a&gt; means the point at ground level directly above this.&lt;br /&gt;&lt;a class="image" title="Global earthquake epicenters, 1963–1998" href="http://en.wikipedia.org/wiki/Image:Quake_epicenters_1963-98.png"&gt;&lt;/a&gt;&lt;br /&gt;&lt;a class="internal" title="Enlarge" href="http://en.wikipedia.org/wiki/Image:Quake_epicenters_1963-98.png"&gt;&lt;/a&gt;Global earthquake &lt;a title="Epicenter" href="http://en.wikipedia.org/wiki/Epicenter"&gt;epicenters&lt;/a&gt;, 1963–1998&lt;br /&gt;&lt;a class="image" title="Global plate tectonic movement" href="http://en.wikipedia.org/wiki/Image:Global_plate_motion_2008-04-17.jpg"&gt;&lt;/a&gt;&lt;br /&gt;&lt;a class="internal" title="Enlarge" href="http://en.wikipedia.org/wiki/Image:Global_plate_motion_2008-04-17.jpg"&gt;&lt;/a&gt;Global plate tectonic movement&lt;br /&gt;Contents[&lt;a class="internal" id="togglelink" href="javascript:toggleToc()"&gt;hide&lt;/a&gt;]&lt;br /&gt;&lt;a href="http://en.wikipedia.org/wiki/Earthquake#Naturally_occurring_earthquakes"&gt;1 Naturally occurring earthquakes&lt;/a&gt;&lt;br /&gt;&lt;a href="http://en.wikipedia.org/wiki/Earthquake#Size_and_frequency_of_occurrence"&gt;2 Size and frequency of occurrence&lt;/a&gt;&lt;br /&gt;&lt;a href="http://en.wikipedia.org/wiki/Earthquake#Effects.2Fimpacts_of_earthquakes"&gt;3 Effects/impacts of earthquakes&lt;/a&gt;&lt;br /&gt;&lt;a href="http://en.wikipedia.org/wiki/Earthquake#Shaking_and_ground_rupture"&gt;3.1 Shaking and ground rupture&lt;/a&gt;&lt;br /&gt;&lt;a href="http://en.wikipedia.org/wiki/Earthquake#Landslides_and_avalanches"&gt;3.2 Landslides and avalanches&lt;/a&gt;&lt;br /&gt;&lt;a href="http://en.wikipedia.org/wiki/Earthquake#Fires"&gt;3.3 Fires&lt;/a&gt;&lt;br /&gt;&lt;a href="http://en.wikipedia.org/wiki/Earthquake#Soil_liquefaction"&gt;3.4 Soil liquefaction&lt;/a&gt;&lt;br /&gt;&lt;a href="http://en.wikipedia.org/wiki/Earthquake#Tsunami"&gt;3.5 Tsunami&lt;/a&gt;&lt;br /&gt;&lt;a href="http://en.wikipedia.org/wiki/Earthquake#Human_impacts"&gt;3.6 Human impacts&lt;/a&gt;&lt;br /&gt;&lt;a href="http://en.wikipedia.org/wiki/Earthquake#Preparation_for_earthquakes"&gt;4 Preparation for earthquakes&lt;/a&gt;&lt;br /&gt;&lt;a href="http://en.wikipedia.org/wiki/Earthquake#Specific_fault_articles"&gt;5 Specific fault articles&lt;/a&gt;&lt;br /&gt;&lt;a href="http://en.wikipedia.org/wiki/Earthquake#Major_earthquakes"&gt;6 Major earthquakes&lt;/a&gt;&lt;br /&gt;&lt;a href="http://en.wikipedia.org/wiki/Earthquake#Pre-20th_century"&gt;6.1 Pre-20th century&lt;/a&gt;&lt;br /&gt;&lt;a href="http://en.wikipedia.org/wiki/Earthquake#20th_century"&gt;6.2 20th century&lt;/a&gt;&lt;br /&gt;&lt;a href="http://en.wikipedia.org/wiki/Earthquake#21st_century"&gt;6.3 21st century&lt;/a&gt;&lt;br /&gt;&lt;a href="http://en.wikipedia.org/wiki/Earthquake#Earthquakes_in_mythology_and_religion"&gt;7 Earthquakes in mythology and religion&lt;/a&gt;&lt;br /&gt;&lt;a href="http://en.wikipedia.org/wiki/Earthquake#See_also"&gt;8 See also&lt;/a&gt;&lt;br /&gt;&lt;a href="http://en.wikipedia.org/wiki/Earthquake#References"&gt;9 References&lt;/a&gt;&lt;br /&gt;&lt;a href="http://en.wikipedia.org/wiki/Earthquake#External_links"&gt;10 External links&lt;/a&gt;&lt;br /&gt;&lt;a href="http://en.wikipedia.org/wiki/Earthquake#Educational"&gt;10.1 Educational&lt;/a&gt;&lt;br /&gt;&lt;a href="http://en.wikipedia.org/wiki/Earthquake#Seismological_data_centers"&gt;10.2 Seismological data centers&lt;/a&gt;&lt;br /&gt;&lt;a href="http://en.wikipedia.org/wiki/Earthquake#Europe"&gt;10.2.1 Europe&lt;/a&gt;&lt;br /&gt;&lt;a href="http://en.wikipedia.org/wiki/Earthquake#Japan"&gt;10.2.2 Japan&lt;/a&gt;&lt;br /&gt;&lt;a href="http://en.wikipedia.org/wiki/Earthquake#United_States"&gt;10.2.3 United States&lt;/a&gt;&lt;br /&gt;&lt;a href="http://en.wikipedia.org/wiki/Earthquake#Seismic_scales"&gt;10.3 Seismic scales&lt;/a&gt;&lt;br /&gt;&lt;a href="http://en.wikipedia.org/wiki/Earthquake#Scientific_information"&gt;10.4 Scientific information&lt;/a&gt;&lt;br /&gt;&lt;a href="http://en.wikipedia.org/wiki/Earthquake#Miscellaneous"&gt;10.5 Miscellaneous&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;a id="Naturally_occurring_earthquakes" name="Naturally_occurring_earthquakes"&gt;&lt;/a&gt;&lt;br /&gt;Naturally occurring earthquakes&lt;br /&gt;&lt;a class="image" title="Fault types" href="http://en.wikipedia.org/wiki/Image:Fault_types.png"&gt;&lt;/a&gt;&lt;br /&gt;&lt;a class="internal" title="Enlarge" href="http://en.wikipedia.org/wiki/Image:Fault_types.png"&gt;&lt;/a&gt;Fault types&lt;br /&gt;Most naturally occurring earthquakes are related to the tectonic nature of the &lt;a title="Earth" href="http://en.wikipedia.org/wiki/Earth"&gt;Earth&lt;/a&gt;. Such earthquakes are called tectonic earthquakes. The Earth's &lt;a title="Lithosphere" href="http://en.wikipedia.org/wiki/Lithosphere"&gt;lithosphere&lt;/a&gt; is a patchwork of plates in slow but constant motion caused by the release to space of the heat in the Earth's mantle and core. The heat causes the rock in the Earth to flow on geological timescales, so that the plates move slowly but surely. &lt;a title="Plate tectonics" href="http://en.wikipedia.org/wiki/Plate_tectonics"&gt;Plate&lt;/a&gt; boundaries lock as the plates move past each other, creating frictional &lt;a title="Stress (physics)" href="http://en.wikipedia.org/wiki/Stress_%28physics%29"&gt;stress&lt;/a&gt;. When the frictional stress exceeds a critical value, called local strength, a sudden failure occurs. The boundary of tectonic plates along which failure occurs is called the &lt;a class="mw-redirect" title="Fault plane" href="http://en.wikipedia.org/wiki/Fault_plane"&gt;fault plane&lt;/a&gt;. When the failure at the fault plane results in a violent displacement of the Earth's &lt;a title="Crust (geology)" href="http://en.wikipedia.org/wiki/Crust_%28geology%29"&gt;crust&lt;/a&gt;, energy is released as a combination of radiated elastic &lt;a title="Strain (materials science)" href="http://en.wikipedia.org/wiki/Strain_%28materials_science%29"&gt;strain&lt;/a&gt; &lt;a class="mw-redirect" title="Seismic waves" href="http://en.wikipedia.org/wiki/Seismic_waves"&gt;seismic waves&lt;/a&gt;, frictional heating of the fault surface, and cracking of the rock, thus causing an earthquake. This process of gradual build-up of strain and stress punctuated by occasional sudden earthquake failure is referred to as the &lt;a title="Elastic-rebound theory" href="http://en.wikipedia.org/wiki/Elastic-rebound_theory"&gt;Elastic-rebound theory&lt;/a&gt;. It is estimated that only 10 percent or less of an earthquake's total energy is radiated as seismic energy. Most of the earthquake's energy is used to power the earthquake &lt;a title="Fracture (geology)" href="http://en.wikipedia.org/wiki/Fracture_%28geology%29"&gt;fracture&lt;/a&gt; growth or is converted into heat generated by friction. Therefore, earthquakes lower the Earth's available elastic potential energy and raise its temperature, though these changes are negligible compared to the conductive and convective flow of heat out from the Earth's deep interior.&lt;a title="" href="http://en.wikipedia.org/wiki/Earthquake#cite_note-USGS1-0"&gt;[1]&lt;/a&gt;&lt;br /&gt;The majority of tectonic earthquakes originate at depths not exceeding tens of kilometers. In &lt;a title="Subduction" href="http://en.wikipedia.org/wiki/Subduction"&gt;subduction zones&lt;/a&gt;, where older and colder &lt;a title="Oceanic crust" href="http://en.wikipedia.org/wiki/Oceanic_crust"&gt;oceanic crust&lt;/a&gt; descends beneath another tectonic plate, &lt;a title="Deep focus earthquake" href="http://en.wikipedia.org/wiki/Deep_focus_earthquake"&gt;Deep focus earthquakes&lt;/a&gt; may occur at much greater depths (up to seven hundred kilometers). These seismically active areas of subduction are known as &lt;a title="Wadati-Benioff zone" href="http://en.wikipedia.org/wiki/Wadati-Benioff_zone"&gt;Wadati-Benioff zones&lt;/a&gt;. These are earthquakes that occur at a depth at which the subducted &lt;a title="Lithosphere" href="http://en.wikipedia.org/wiki/Lithosphere"&gt;lithosphere&lt;/a&gt; should no longer be brittle, due to the high temperature and pressure. A possible mechanism for the generation of deep focus earthquakes is faulting caused by &lt;a title="Olivine" href="http://en.wikipedia.org/wiki/Olivine"&gt;olivine&lt;/a&gt; undergoing a &lt;a title="Phase transition" href="http://en.wikipedia.org/wiki/Phase_transition"&gt;phase transition&lt;/a&gt; into a &lt;a title="Spinel" href="http://en.wikipedia.org/wiki/Spinel"&gt;spinel&lt;/a&gt; structure.&lt;a title="" href="http://en.wikipedia.org/wiki/Earthquake#cite_note-olivine-1"&gt;[2]&lt;/a&gt;&lt;br /&gt;Earthquakes also often occur in volcanic regions and are caused there, both by tectonic faults and by the movement of &lt;a title="Magma" href="http://en.wikipedia.org/wiki/Magma"&gt;magma&lt;/a&gt; in &lt;a title="Volcano" href="http://en.wikipedia.org/wiki/Volcano"&gt;volcanoes&lt;/a&gt;. Such earthquakes can serve as an early warning of volcanic eruptions.&lt;br /&gt;Sometimes a series of earthquakes occur in a sort of &lt;a title="Earthquake storm" href="http://en.wikipedia.org/wiki/Earthquake_storm"&gt;earthquake storm&lt;/a&gt;, where the earthquakes strike a fault in clusters, each triggered by the shaking or stress redistribution of the previous earthquakes. Similar to &lt;a title="Aftershock" href="http://en.wikipedia.org/wiki/Aftershock"&gt;aftershocks&lt;/a&gt; but on adjacent segments of fault, these storms occur over the course of years, and with some of the later earthquakes as damaging as the early ones. Such a pattern was observed in the sequence of about a dozen earthquakes that struck the &lt;a title="North Anatolian Fault" href="http://en.wikipedia.org/wiki/North_Anatolian_Fault"&gt;North Anatolian Fault&lt;/a&gt; in Turkey in the 20th century, the half dozen large earthquakes in &lt;a title="New Madrid, Missouri" href="http://en.wikipedia.org/wiki/New_Madrid%2C_Missouri"&gt;New Madrid&lt;/a&gt; in 1811-1812, and has been inferred for older anomalous clusters of large earthquakes in the Middle East and in the Mojave Desert.&lt;br /&gt;&lt;a id="Size_and_frequency_of_occurrence" name="Size_and_frequency_of_occurrence"&gt;&lt;/a&gt;&lt;br /&gt;[&lt;a title="Edit section: Size and frequency of occurrence" href="http://en.wikipedia.org/w/index.php?title=Earthquake&amp;amp;action=edit&amp;amp;section=2"&gt;edit&lt;/a&gt;] Size and frequency of occurrence&lt;br /&gt;&lt;a class="image" title="Globe icon" href="http://en.wikipedia.org/wiki/Image:Ambox_globe_content.svg"&gt;&lt;/a&gt;&lt;br /&gt;This article may not provide &lt;a title="Wikipedia:WikiProject Countering systemic bias" href="http://en.wikipedia.org/wiki/Wikipedia:WikiProject_Countering_systemic_bias"&gt;balanced geographical coverage&lt;/a&gt; on a region.An editor has expressed concern that this article is biased. Please &lt;a class="external text" title="http://en.wikipedia.org/w/index.php?title=" action="edit" href="http://en.wikipedia.org/w/index.php?title=Earthquake&amp;amp;action=edit" rel="nofollow"&gt;improve this article&lt;/a&gt; or discuss the issue on the &lt;a title="Talk:Earthquake" href="http://en.wikipedia.org/wiki/Talk:Earthquake"&gt;talk page&lt;/a&gt;.&lt;br /&gt;&lt;a class="image" title="Unbalanced scales" href="http://en.wikipedia.org/wiki/Image:Unbalanced_scales.svg"&gt;&lt;/a&gt;&lt;br /&gt;Minor earthquakes occur nearly constantly around the world in places like &lt;a title="California" href="http://en.wikipedia.org/wiki/California"&gt;California&lt;/a&gt; and &lt;a title="Alaska" href="http://en.wikipedia.org/wiki/Alaska"&gt;Alaska&lt;/a&gt; in the U.S., as well as in &lt;a title="Chile" href="http://en.wikipedia.org/wiki/Chile"&gt;Chile&lt;/a&gt;, &lt;a title="Peru" href="http://en.wikipedia.org/wiki/Peru"&gt;Peru&lt;/a&gt;, &lt;a title="Indonesia" href="http://en.wikipedia.org/wiki/Indonesia"&gt;Indonesia&lt;/a&gt;, &lt;a title="Iran" href="http://en.wikipedia.org/wiki/Iran"&gt;Iran&lt;/a&gt;, &lt;a title="India" href="http://en.wikipedia.org/wiki/India"&gt;India&lt;/a&gt; the &lt;a title="Azores" href="http://en.wikipedia.org/wiki/Azores"&gt;Azores&lt;/a&gt; in &lt;a title="Portugal" href="http://en.wikipedia.org/wiki/Portugal"&gt;Portugal&lt;/a&gt;, &lt;a title="New Zealand" href="http://en.wikipedia.org/wiki/New_Zealand"&gt;New Zealand&lt;/a&gt;, &lt;a title="Greece" href="http://en.wikipedia.org/wiki/Greece"&gt;Greece&lt;/a&gt;, &lt;a title="Italy" href="http://en.wikipedia.org/wiki/Italy"&gt;Italy&lt;/a&gt;, and &lt;a title="Japan" href="http://en.wikipedia.org/wiki/Japan"&gt;Japan&lt;/a&gt;,&lt;a title="" href="http://en.wikipedia.org/wiki/Earthquake#cite_note-2"&gt;[3]&lt;/a&gt; Larger earthquakes occur less frequently, the relationship being &lt;a title="Gutenberg-Richter law" href="http://en.wikipedia.org/wiki/Gutenberg-Richter_law"&gt;exponential&lt;/a&gt;; for example, roughly ten times as many earthquakes larger than magnitude 4 occur in a particular time period than earthquakes larger than magnitude 5. In the (low seismicity) &lt;a title="United Kingdom" href="http://en.wikipedia.org/wiki/United_Kingdom"&gt;United Kingdom&lt;/a&gt;, for example, it has been calculated that the average recurrences are:&lt;br /&gt;an earthquake of 3.7 - 4.6 every year&lt;br /&gt;an earthquake of 4.7 - 5.5 every 10 years&lt;br /&gt;an earthquake of 5.6 or larger every 100 years.&lt;br /&gt;The number of seismic stations has increased from about 350 in 1931 to many thousands today. As a result, many more earthquakes are reported than in the past because of the vast improvement in instrumentation (not because the number of earthquakes has increased). The &lt;a class="mw-redirect" title="USGS" href="http://en.wikipedia.org/wiki/USGS"&gt;USGS&lt;/a&gt; estimates that, since 1900, there have been an average of 18 major earthquakes (magnitude 7.0-7.9) and one great earthquake (magnitude 8.0 or greater) per year, and that this average has been relatively stable.&lt;a title="" href="http://en.wikipedia.org/wiki/Earthquake#cite_note-3"&gt;[4]&lt;/a&gt; In fact, in recent years, the number of major earthquakes per year has actually decreased, although this is likely a statistical fluctuation. More detailed statistics on the size and frequency of earthquakes is available from the USGS.&lt;a title="" href="http://en.wikipedia.org/wiki/Earthquake#cite_note-4"&gt;[5]&lt;/a&gt;&lt;br /&gt;Most of the world's earthquakes (90%, and 81% of the largest) take place in the 40,000-km-long, horseshoe-shaped zone called the &lt;a title="Pacific Ring of Fire" href="http://en.wikipedia.org/wiki/Pacific_Ring_of_Fire"&gt;circum-Pacific seismic belt&lt;/a&gt;, also known as the &lt;a title="Pacific Ring of Fire" href="http://en.wikipedia.org/wiki/Pacific_Ring_of_Fire"&gt;Pacific Ring of Fire&lt;/a&gt;, which for the most part bounds the &lt;a title="Pacific Plate" href="http://en.wikipedia.org/wiki/Pacific_Plate"&gt;Pacific Plate&lt;/a&gt;.&lt;a title="" href="http://en.wikipedia.org/wiki/Earthquake#cite_note-5"&gt;[6]&lt;/a&gt;&lt;a title="" href="http://en.wikipedia.org/wiki/Earthquake#cite_note-6"&gt;[7]&lt;/a&gt; Massive earthquakes tend to occur along other plate boundaries, too, such as along the &lt;a class="mw-redirect" title="Himalayan Mountains" href="http://en.wikipedia.org/wiki/Himalayan_Mountains"&gt;Himalayan Mountains&lt;/a&gt;.&lt;br /&gt;With the rapid growth of &lt;a title="Megacity" href="http://en.wikipedia.org/wiki/Megacity"&gt;mega-cities&lt;/a&gt; such as &lt;a title="Mexico City" href="http://en.wikipedia.org/wiki/Mexico_City"&gt;Mexico City&lt;/a&gt;, &lt;a title="Tokyo" href="http://en.wikipedia.org/wiki/Tokyo"&gt;Tokyo&lt;/a&gt; or &lt;a title="Tehran" href="http://en.wikipedia.org/wiki/Tehran"&gt;Tehran&lt;/a&gt;, in areas of high seismic risk, some seismologists are warning that a single quake may claim the lives of up to 3 million people.&lt;a title="" href="http://en.wikipedia.org/wiki/Earthquake#cite_note-7"&gt;[8]&lt;/a&gt;&lt;a title="" href="http://en.wikipedia.org/wiki/Earthquake#cite_note-8"&gt;[9]&lt;/a&gt;&lt;a title="" href="http://en.wikipedia.org/wiki/Earthquake#cite_note-9"&gt;[10]&lt;/a&gt;&lt;br /&gt;&lt;a id="Effects.2Fimpacts_of_earthquakes" name="Effects.2Fimpacts_of_earthquakes"&gt;&lt;/a&gt;&lt;br /&gt;Effects/impacts of earthquakes&lt;br /&gt;&lt;a class="image" title="1755 copper engraving depicting Lisbon in ruins and in flames after the 1755 Lisbon earthquake. A tsunami overwhelms the ships in the harbor." href="http://en.wikipedia.org/wiki/Image:1755_Lisbon_earthquake.jpg"&gt;&lt;/a&gt;&lt;br /&gt;&lt;a class="internal" title="Enlarge" href="http://en.wikipedia.org/wiki/Image:1755_Lisbon_earthquake.jpg"&gt;&lt;/a&gt;1755 copper engraving depicting &lt;a title="Lisbon" href="http://en.wikipedia.org/wiki/Lisbon"&gt;Lisbon&lt;/a&gt; in ruins and in flames after the &lt;a title="1755 Lisbon earthquake" href="http://en.wikipedia.org/wiki/1755_Lisbon_earthquake"&gt;1755 Lisbon earthquake&lt;/a&gt;. A &lt;a title="Tsunami" href="http://en.wikipedia.org/wiki/Tsunami"&gt;tsunami&lt;/a&gt; overwhelms the ships in the harbor.&lt;br /&gt;&lt;a class="image" title="Smoldering after the 1906 San Francisco earthquake." href="http://en.wikipedia.org/wiki/Image:Sanfranciscoearthquake1906.jpg"&gt;&lt;/a&gt;&lt;br /&gt;&lt;a class="internal" title="Enlarge" href="http://en.wikipedia.org/wiki/Image:Sanfranciscoearthquake1906.jpg"&gt;&lt;/a&gt;Smoldering after the &lt;a title="1906 San Francisco earthquake" href="http://en.wikipedia.org/wiki/1906_San_Francisco_earthquake"&gt;1906 San Francisco earthquake&lt;/a&gt;.&lt;br /&gt;&lt;a class="image" title="Earthquake damage in Anchorage, Alaska (1964)." href="http://en.wikipedia.org/wiki/Image:AlaskaQuake-FourthAve.jpg"&gt;&lt;/a&gt;&lt;br /&gt;&lt;a class="internal" title="Enlarge" href="http://en.wikipedia.org/wiki/Image:AlaskaQuake-FourthAve.jpg"&gt;&lt;/a&gt;Earthquake damage in &lt;a title="Anchorage" href="http://en.wikipedia.org/wiki/Anchorage"&gt;Anchorage&lt;/a&gt;, &lt;a title="Alaska" href="http://en.wikipedia.org/wiki/Alaska"&gt;Alaska&lt;/a&gt; (1964).&lt;br /&gt;&lt;a class="image" title="Earthquake damage in Mexico City (1985)." href="http://en.wikipedia.org/wiki/Image:Tlatelolco.PNG"&gt;&lt;/a&gt;&lt;br /&gt;&lt;a class="internal" title="Enlarge" href="http://en.wikipedia.org/wiki/Image:Tlatelolco.PNG"&gt;&lt;/a&gt;Earthquake damage in &lt;a title="Mexico City" href="http://en.wikipedia.org/wiki/Mexico_City"&gt;Mexico City&lt;/a&gt; (1985).&lt;br /&gt;&lt;a class="image" title="Earthquake damage in Armenia (1988)." href="http://en.wikipedia.org/wiki/Image:Spitakear.jpg"&gt;&lt;/a&gt;&lt;br /&gt;&lt;a class="internal" title="Enlarge" href="http://en.wikipedia.org/wiki/Image:Spitakear.jpg"&gt;&lt;/a&gt;Earthquake damage in &lt;a title="Armenia" href="http://en.wikipedia.org/wiki/Armenia"&gt;Armenia&lt;/a&gt; (1988).&lt;br /&gt;&lt;a class="image" title="A section of the Cypress viaduct collapsed during the Loma Prieta Earthquake (1989)." href="http://en.wikipedia.org/wiki/Image:Cypress_structure.jpeg"&gt;&lt;/a&gt;&lt;br /&gt;&lt;a class="internal" title="Enlarge" href="http://en.wikipedia.org/wiki/Image:Cypress_structure.jpeg"&gt;&lt;/a&gt;A section of the Cypress viaduct collapsed during the &lt;a class="mw-redirect" title="Loma Prieta Earthquake" href="http://en.wikipedia.org/wiki/Loma_Prieta_Earthquake"&gt;Loma Prieta Earthquake&lt;/a&gt; (1989).&lt;br /&gt;&lt;a class="image" title="Kaiser Permanente Building destroyed in the Northridge Earthquake (1994)." href="http://en.wikipedia.org/wiki/Image:Kaiser_Permanente_Building_After_Northridge_Earthquake.jpg"&gt;&lt;/a&gt;&lt;br /&gt;&lt;a class="internal" title="Enlarge" href="http://en.wikipedia.org/wiki/Image:Kaiser_Permanente_Building_After_Northridge_Earthquake.jpg"&gt;&lt;/a&gt;Kaiser Permanente Building destroyed in the &lt;a class="mw-redirect" title="Northridge Earthquake" href="http://en.wikipedia.org/wiki/Northridge_Earthquake"&gt;Northridge Earthquake&lt;/a&gt; (1994).&lt;br /&gt;&lt;a class="image" title="Damage in Great Hanshin earthquake (1995) in Kobe, Japan." href="http://en.wikipedia.org/wiki/Image:%E9%98%AA%E7%A5%9E%E6%B7%A1%E8%B7%AF%E5%A4%A7%E9%9C%87%E7%81%BD343.jpg"&gt;&lt;/a&gt;&lt;br /&gt;&lt;a class="internal" title="Enlarge" href="http://en.wikipedia.org/wiki/Image:%E9%98%AA%E7%A5%9E%E6%B7%A1%E8%B7%AF%E5%A4%A7%E9%9C%87%E7%81%BD343.jpg"&gt;&lt;/a&gt;Damage in &lt;a title="Great Hanshin earthquake" href="http://en.wikipedia.org/wiki/Great_Hanshin_earthquake"&gt;Great Hanshin earthquake&lt;/a&gt; (1995) in &lt;a title="Kobe" href="http://en.wikipedia.org/wiki/Kobe"&gt;Kobe&lt;/a&gt;, Japan.&lt;br /&gt;&lt;a class="image" title="Chūetsu earthquake (2004)." href="http://en.wikipedia.org/wiki/Image:Chuetsu_earthquake-earthquake_liquefaction1.jpg"&gt;&lt;/a&gt;&lt;br /&gt;&lt;a class="internal" title="Enlarge" href="http://en.wikipedia.org/wiki/Image:Chuetsu_earthquake-earthquake_liquefaction1.jpg"&gt;&lt;/a&gt;&lt;a title="2004 Chūetsu earthquake" href="http://en.wikipedia.org/wiki/2004_Ch%C5%ABetsu_earthquake"&gt;Chūetsu earthquake&lt;/a&gt; (2004).&lt;br /&gt;&lt;a class="image" title="Wiki letter w.svg" href="http://en.wikipedia.org/wiki/Image:Wiki_letter_w.svg"&gt;&lt;/a&gt;&lt;br /&gt;Please help &lt;a class="external text" title="http://en.wikipedia.org/w/index.php?title=" action="edit" href="http://en.wikipedia.org/w/index.php?title=Earthquake&amp;amp;action=edit" rel="nofollow"&gt;improve this section&lt;/a&gt; by expanding it.Further information might be found on the &lt;a title="Talk:Earthquake" href="http://en.wikipedia.org/wiki/Talk:Earthquake"&gt;talk page&lt;/a&gt; or at &lt;a title="Wikipedia:Requests for expansion" href="http://en.wikipedia.org/wiki/Wikipedia:Requests_for_expansion"&gt;requests for expansion&lt;/a&gt;.&lt;br /&gt;There are many effects of earthquakes including, but not limited to the following:&lt;br /&gt;&lt;a id="Shaking_and_ground_rupture" name="Shaking_and_ground_rupture"&gt;&lt;/a&gt;&lt;br /&gt;[&lt;a title="Edit section: Shaking and ground rupture" href="http://en.wikipedia.org/w/index.php?title=Earthquake&amp;amp;action=edit&amp;amp;section=4"&gt;edit&lt;/a&gt;] Shaking and ground rupture&lt;br /&gt;Shaking and ground rupture are the main effects created by earthquakes, principally resulting in more or less severe damage to buildings or other rigid structures. The severity of the local effects depends on the complex combination of the earthquake &lt;a title="Richter magnitude scale" href="http://en.wikipedia.org/wiki/Richter_magnitude_scale"&gt;magnitude&lt;/a&gt;, the distance from &lt;a title="Epicenter" href="http://en.wikipedia.org/wiki/Epicenter"&gt;epicenter&lt;/a&gt;, and the local geological and geomorphological conditions, which may amplify or reduce &lt;a title="Wave propagation" href="http://en.wikipedia.org/wiki/Wave_propagation"&gt;wave propagation&lt;/a&gt;. The ground-shaking is measured by ground &lt;a title="Acceleration" href="http://en.wikipedia.org/wiki/Acceleration"&gt;acceleration&lt;/a&gt;.&lt;br /&gt;Specific local geological, geomorphological, and geostructural features can induce high levels of shaking on the ground surface even from low-intensity earthquakes. This effect is called site or local amplification. It is principally due to the transfer of the &lt;a class="mw-redirect" title="Seismic" href="http://en.wikipedia.org/wiki/Seismic"&gt;seismic&lt;/a&gt; motion from hard deep soils to soft superficial soils and to effects of seismic energy focalization owing to typical geometrical setting of the deposits.&lt;br /&gt;Ground rupture is a visible breaking and displacement of the earth's surface along the trace of the fault, which may be of the order of few metres in the case of major earthquakes. Ground rupture is a major risk for large engineering structures such as &lt;a class="mw-redirect" title="Dams" href="http://en.wikipedia.org/wiki/Dams"&gt;dams&lt;/a&gt;, &lt;a title="Bridges" href="http://en.wikipedia.org/wiki/Bridges"&gt;bridges&lt;/a&gt; and &lt;a class="mw-redirect" title="Nuclear power stations" href="http://en.wikipedia.org/wiki/Nuclear_power_stations"&gt;nuclear power stations&lt;/a&gt; and requires careful mapping of existing faults to identify any likely to break the ground surface within the life of the structure.&lt;br /&gt;&lt;a id="Landslides_and_avalanches" name="Landslides_and_avalanches"&gt;&lt;/a&gt;&lt;br /&gt;[&lt;a title="Edit section: Landslides and avalanches" href="http://en.wikipedia.org/w/index.php?title=Earthquake&amp;amp;action=edit&amp;amp;section=5"&gt;edit&lt;/a&gt;] Landslides and avalanches&lt;br /&gt;Earthquakes can cause &lt;a title="Landslide" href="http://en.wikipedia.org/wiki/Landslide"&gt;landslides&lt;/a&gt; and &lt;a title="Avalanche" href="http://en.wikipedia.org/wiki/Avalanche"&gt;avalanches&lt;/a&gt;, which may cause damage in hilly and mountainous areas.&lt;br /&gt;&lt;a id="Fires" name="Fires"&gt;&lt;/a&gt;&lt;br /&gt;[&lt;a title="Edit section: Fires" href="http://en.wikipedia.org/w/index.php?title=Earthquake&amp;amp;action=edit&amp;amp;section=6"&gt;edit&lt;/a&gt;] Fires&lt;br /&gt;Following an earthquake, &lt;a title="Fire" href="http://en.wikipedia.org/wiki/Fire"&gt;fires&lt;/a&gt; can be generated by break of the &lt;a title="Electric power" href="http://en.wikipedia.org/wiki/Electric_power"&gt;electrical power&lt;/a&gt; or gas lines. In the event of water mains rupturing and a loss of pressure, it may also become difficult to stop the spread of a fire once it has started.&lt;br /&gt;&lt;a id="Soil_liquefaction" name="Soil_liquefaction"&gt;&lt;/a&gt;&lt;br /&gt;[&lt;a title="Edit section: Soil liquefaction" href="http://en.wikipedia.org/w/index.php?title=Earthquake&amp;amp;action=edit&amp;amp;section=7"&gt;edit&lt;/a&gt;] Soil liquefaction&lt;br /&gt;Soil &lt;a class="mw-redirect" title="Earthquake liquefaction" href="http://en.wikipedia.org/wiki/Earthquake_liquefaction"&gt;liquefaction&lt;/a&gt; occurs when, because of the shaking, water-saturated &lt;a class="mw-redirect" title="Granular" href="http://en.wikipedia.org/wiki/Granular"&gt;granular&lt;/a&gt; material temporarily loses its strength and transforms from a &lt;a title="Solid" href="http://en.wikipedia.org/wiki/Solid"&gt;solid&lt;/a&gt; to a &lt;a title="Liquid" href="http://en.wikipedia.org/wiki/Liquid"&gt;liquid&lt;/a&gt;. Soil liquefaction may cause rigid structures, as buildings or bridges, to tilt or sink into the liquefied deposits.&lt;br /&gt;&lt;a id="Tsunami" name="Tsunami"&gt;&lt;/a&gt;&lt;br /&gt;[&lt;a title="Edit section: Tsunami" href="http://en.wikipedia.org/w/index.php?title=Earthquake&amp;amp;action=edit&amp;amp;section=8"&gt;edit&lt;/a&gt;] Tsunami&lt;br /&gt;Undersea earthquakes and earthquake-triggered landslides into the sea, can cause &lt;a title="Tsunami" href="http://en.wikipedia.org/wiki/Tsunami"&gt;Tsunami&lt;/a&gt;. See, for example, the &lt;a title="2004 Indian Ocean earthquake" href="http://en.wikipedia.org/wiki/2004_Indian_Ocean_earthquake"&gt;2004 Indian Ocean earthquake&lt;/a&gt;.&lt;br /&gt;&lt;a id="Human_impacts" name="Human_impacts"&gt;&lt;/a&gt;&lt;br /&gt;[&lt;a title="Edit section: Human impacts" href="http://en.wikipedia.org/w/index.php?title=Earthquake&amp;amp;action=edit&amp;amp;section=9"&gt;edit&lt;/a&gt;] Human impacts&lt;br /&gt;Earthquakes may result in &lt;a title="Disease" href="http://en.wikipedia.org/wiki/Disease"&gt;disease&lt;/a&gt;, lack of basic necessities, loss of life, higher insurance premiums, general property damage, road and bridge damage, and collapse of buildings or destabilization of the base of buildings which may lead to collapse in future earthquakes.&lt;br /&gt;&lt;a id="Preparation_for_earthquakes" name="Preparation_for_earthquakes"&gt;&lt;/a&gt;&lt;br /&gt;[&lt;a title="Edit section: Preparation for earthquakes" href="http://en.wikipedia.org/w/index.php?title=Earthquake&amp;amp;action=edit&amp;amp;section=10"&gt;edit&lt;/a&gt;] Preparation for earthquakes&lt;br /&gt;&lt;a title="Earthquake preparedness" href="http://en.wikipedia.org/wiki/Earthquake_preparedness"&gt;Earthquake preparedness&lt;/a&gt;&lt;br /&gt;&lt;a title="Household seismic safety" href="http://en.wikipedia.org/wiki/Household_seismic_safety"&gt;Household seismic safety&lt;/a&gt;&lt;br /&gt;&lt;a title="HurriQuake" href="http://en.wikipedia.org/wiki/HurriQuake"&gt;HurriQuake&lt;/a&gt; nail (for resisting hurricanes and earthquakes)&lt;br /&gt;&lt;a title="Seismic retrofit" href="http://en.wikipedia.org/wiki/Seismic_retrofit"&gt;Seismic retrofit&lt;/a&gt;&lt;br /&gt;&lt;a title="Seismic hazard" href="http://en.wikipedia.org/wiki/Seismic_hazard"&gt;Seismic hazard&lt;/a&gt;&lt;br /&gt;&lt;a title="Mitigation of seismic motion" href="http://en.wikipedia.org/wiki/Mitigation_of_seismic_motion"&gt;Mitigation of seismic motion&lt;/a&gt;&lt;br /&gt;Earthquake prediction&lt;br /&gt;Pre-20th century&lt;br /&gt;&lt;a title="Pompeii" href="http://en.wikipedia.org/wiki/Pompeii"&gt;Pompeii&lt;/a&gt; (62).&lt;br /&gt;&lt;a title="1138 Aleppo earthquake" href="http://en.wikipedia.org/wiki/1138_Aleppo_earthquake"&gt;Aleppo Earthquake&lt;/a&gt; (1138).&lt;br /&gt;&lt;a class="mw-redirect" title="Basel earthquake" href="http://en.wikipedia.org/wiki/Basel_earthquake"&gt;Basel earthquake&lt;/a&gt; (1356). Major earthquake that struck Central Europe in 1356.&lt;br /&gt;&lt;a title="Carniola" href="http://en.wikipedia.org/wiki/Carniola"&gt;Carniola&lt;/a&gt; earthquake (1511). A major earthquake that shook a large portion of South-&lt;a title="Central Europe" href="http://en.wikipedia.org/wiki/Central_Europe"&gt;Central Europe&lt;/a&gt;. Its epicenter was around the town of &lt;a title="Idrija" href="http://en.wikipedia.org/wiki/Idrija"&gt;Idrija&lt;/a&gt;, in today's &lt;a title="Slovenia" href="http://en.wikipedia.org/wiki/Slovenia"&gt;Slovenia&lt;/a&gt;. It caused great damage to structures all over &lt;a title="Carniola" href="http://en.wikipedia.org/wiki/Carniola"&gt;Carniola&lt;/a&gt;, including &lt;a title="Ljubljana" href="http://en.wikipedia.org/wiki/Ljubljana"&gt;Ljubljana&lt;/a&gt;, and in western &lt;a title="Duchy of Carinthia" href="http://en.wikipedia.org/wiki/Duchy_of_Carinthia"&gt;Carinthia&lt;/a&gt;, particularly in &lt;a title="Villach" href="http://en.wikipedia.org/wiki/Villach"&gt;Villach&lt;/a&gt; and &lt;a class="mw-redirect" title="Klagenfurt" href="http://en.wikipedia.org/wiki/Klagenfurt"&gt;Klagenfurt&lt;/a&gt; which were almost completely destroyed. There was some minor damage in &lt;a title="Venice" href="http://en.wikipedia.org/wiki/Venice"&gt;Venice&lt;/a&gt; and other cities, too.&lt;br /&gt;&lt;a class="mw-redirect" title="Shaanxi Earthquake" href="http://en.wikipedia.org/wiki/Shaanxi_Earthquake"&gt;Shaanxi Earthquake&lt;/a&gt; (1556). Deadliest known earthquake in history, estimated to have killed 830,000 in &lt;a title="China" href="http://en.wikipedia.org/wiki/China"&gt;China&lt;/a&gt;.&lt;br /&gt;&lt;a title="Dover Straits earthquake of 1580" href="http://en.wikipedia.org/wiki/Dover_Straits_earthquake_of_1580"&gt;Dover Straits earthquake of 1580&lt;/a&gt; (1580).&lt;br /&gt;&lt;a class="new" title="Dubrovnik earthquake (page does not exist)" href="http://en.wikipedia.org/w/index.php?title=Dubrovnik_earthquake&amp;amp;action=edit&amp;amp;redlink=1"&gt;Dubrovnik earthquake&lt;/a&gt; (1667). Disastrous earthquake in &lt;a title="Dubrovnik" href="http://en.wikipedia.org/wiki/Dubrovnik"&gt;Dubrovnik&lt;/a&gt;, &lt;a title="Croatia" href="http://en.wikipedia.org/wiki/Croatia"&gt;Croatia&lt;/a&gt; killed about 3/5 of the population.&lt;br /&gt;&lt;a title="Port Royal" href="http://en.wikipedia.org/wiki/Port_Royal"&gt;Port Royal&lt;/a&gt; Earthquake (1692). An earthquake on &lt;a title="June 7" href="http://en.wikipedia.org/wiki/June_7"&gt;June 7&lt;/a&gt;, &lt;a title="1692" href="http://en.wikipedia.org/wiki/1692"&gt;1692&lt;/a&gt;, largely destroyed &lt;a title="Port Royal" href="http://en.wikipedia.org/wiki/Port_Royal"&gt;Port Royal&lt;/a&gt;, a safe harbor for &lt;a class="mw-redirect" title="Pirates" href="http://en.wikipedia.org/wiki/Pirates"&gt;pirates&lt;/a&gt;, causing two thirds of the city to sink into the &lt;a title="Caribbean Sea" href="http://en.wikipedia.org/wiki/Caribbean_Sea"&gt;Caribbean Sea&lt;/a&gt;.&lt;br /&gt;&lt;a title="Sicilian Baroque" href="http://en.wikipedia.org/wiki/Sicilian_Baroque#Earthquake_and_patrons"&gt;The great Sicilian earthquake&lt;/a&gt; (1693). As many as 100,000 may have died.&lt;br /&gt;&lt;a class="mw-redirect" title="Cascadia Earthquake" href="http://en.wikipedia.org/wiki/Cascadia_Earthquake"&gt;Cascadia Earthquake&lt;/a&gt; (1700).&lt;br /&gt;&lt;a title="Tokyo" href="http://en.wikipedia.org/wiki/Tokyo"&gt;Tokyo&lt;/a&gt; earthquake (1703). 37,000 died.&lt;br /&gt;&lt;a title="Kamchatka earthquakes" href="http://en.wikipedia.org/wiki/Kamchatka_earthquakes"&gt;Kamchatka earthquakes&lt;/a&gt; (1737) The third biggest earthquake on record measuring 9.3 on the richter scale.&lt;br /&gt;&lt;a title="1755 Lisbon earthquake" href="http://en.wikipedia.org/wiki/1755_Lisbon_earthquake"&gt;Lisbon earthquake&lt;/a&gt; (1755), one of the most destructive and deadly earthquakes in history, killing between 60,000 and 100,000 people and causing a major &lt;a title="Tsunami" href="http://en.wikipedia.org/wiki/Tsunami"&gt;tsunami&lt;/a&gt; that affected parts of &lt;a title="Europe" href="http://en.wikipedia.org/wiki/Europe"&gt;Europe&lt;/a&gt;, &lt;a title="North Africa" href="http://en.wikipedia.org/wiki/North_Africa"&gt;North Africa&lt;/a&gt; and the &lt;a title="Caribbean" href="http://en.wikipedia.org/wiki/Caribbean"&gt;Caribbean&lt;/a&gt;.&lt;br /&gt;&lt;a class="new" title="Calabria earthquake (page does not exist)" href="http://en.wikipedia.org/w/index.php?title=Calabria_earthquake&amp;amp;action=edit&amp;amp;redlink=1"&gt;Calabria earthquake&lt;/a&gt; (1783). Series of 6 earthquakes in &lt;a title="Calabria" href="http://en.wikipedia.org/wiki/Calabria"&gt;Calabria&lt;/a&gt;, &lt;a title="Italy" href="http://en.wikipedia.org/wiki/Italy"&gt;Italy&lt;/a&gt; killed 50,000.&lt;a title="" href="http://en.wikipedia.org/wiki/Earthquake#cite_note-10"&gt;[11]&lt;/a&gt;&lt;br /&gt;&lt;a title="Quito" href="http://en.wikipedia.org/wiki/Quito"&gt;Quito&lt;/a&gt; earthquake. (1797) &lt;a title="Quito" href="http://en.wikipedia.org/wiki/Quito"&gt;Quito&lt;/a&gt;, &lt;a title="Viceroyalty of Peru" href="http://en.wikipedia.org/wiki/Viceroyalty_of_Peru"&gt;Viceroyalty of Peru&lt;/a&gt;, now the capital of &lt;a title="Ecuador" href="http://en.wikipedia.org/wiki/Ecuador"&gt;Ecuador&lt;/a&gt;, was devastated by an earthquake. 40,000 died.&lt;br /&gt;&lt;a class="mw-redirect" title="New Madrid Earthquake" href="http://en.wikipedia.org/wiki/New_Madrid_Earthquake"&gt;New Madrid Earthquake&lt;/a&gt; (1811), and another tremor (1812) that also struck the small Missouri town, was reportedly the strongest ever in &lt;a title="North America" href="http://en.wikipedia.org/wiki/North_America"&gt;North America&lt;/a&gt; and made the &lt;a title="Mississippi River" href="http://en.wikipedia.org/wiki/Mississippi_River"&gt;Mississippi River&lt;/a&gt; temporarily change its direction and permanently altered its course in the region.&lt;br /&gt;&lt;a title="Fort Tejon earthquake" href="http://en.wikipedia.org/wiki/Fort_Tejon_earthquake"&gt;Fort Tejon Earthquake&lt;/a&gt; (1857). Estimated Richter Scale above 8, said the strongest earthquake in Southern California history.&lt;br /&gt;&lt;a title="Great Neapolitan Earthquake" href="http://en.wikipedia.org/wiki/Great_Neapolitan_Earthquake"&gt;Great Neapolitan Earthquake&lt;/a&gt; (1857). Estimated Richter Scale of 6.9. 11,000 dead.&lt;br /&gt;&lt;a title="1872 Lone Pine earthquake" href="http://en.wikipedia.org/wiki/1872_Lone_Pine_earthquake"&gt;1872 Lone Pine earthquake&lt;/a&gt; (1872). Might been strongest ever measured in California with an estimated Richter Scale of 8.1 said &lt;a class="mw-redirect" title="Seismologists" href="http://en.wikipedia.org/wiki/Seismologists"&gt;seismologists&lt;/a&gt;.&lt;br /&gt;&lt;a title="Charleston earthquake" href="http://en.wikipedia.org/wiki/Charleston_earthquake"&gt;Charleston earthquake&lt;/a&gt; (1886). Largest earthquake in the southeastern United States, killed 100.&lt;br /&gt;&lt;a title="Ljubljana earthquake" href="http://en.wikipedia.org/wiki/Ljubljana_earthquake"&gt;Ljubljana earthquake&lt;/a&gt; (14. IV. 1895), a series of powerful quakes that ultimately had a vital impact on the city of &lt;a title="Ljubljana" href="http://en.wikipedia.org/wiki/Ljubljana"&gt;Ljubljana&lt;/a&gt;, being a &lt;a class="mw-redirect" title="Catalyst" href="http://en.wikipedia.org/wiki/Catalyst"&gt;catalyst&lt;/a&gt; of its urban renewal.&lt;br /&gt;&lt;a class="mw-redirect" title="Assam earthquake of 1897" href="http://en.wikipedia.org/wiki/Assam_earthquake_of_1897"&gt;Assam earthquake of 1897&lt;/a&gt; (1897). Large earthquake that destroyed all masonry structures, measuring more than 8 on the Richter scale.&lt;br /&gt;&lt;a name="20th_century"&gt;&lt;/a&gt;&lt;br /&gt;20th century&lt;br /&gt;&lt;a class="mw-redirect" title="1906 San Francisco Earthquake" href="http://en.wikipedia.org/wiki/1906_San_Francisco_Earthquake"&gt;San Francisco Earthquake&lt;/a&gt; (1906). Between 7.7 and 8.3 magnitudes; killed approximately 3,000 people and caused around $400 million in damage; most devastating earthquake in California and U.S. history.&lt;br /&gt;&lt;a class="mw-redirect" title="Messina Earthquake" href="http://en.wikipedia.org/wiki/Messina_Earthquake"&gt;Messina Earthquake&lt;/a&gt; (1908). Killed about 60,000 people.&lt;br /&gt;&lt;a class="new" title="Gansu earthquake (page does not exist)" href="http://en.wikipedia.org/w/index.php?title=Gansu_earthquake&amp;amp;action=edit&amp;amp;redlink=1"&gt;Gansu earthquake&lt;/a&gt; (1920). Killed 200,000 in &lt;a title="Gansu" href="http://en.wikipedia.org/wiki/Gansu#History"&gt;Gansu&lt;/a&gt; province, &lt;a title="China" href="http://en.wikipedia.org/wiki/China"&gt;China&lt;/a&gt;.&lt;a title="" href="http://en.wikipedia.org/wiki/Earthquake#cite_note-11"&gt;[12]&lt;/a&gt;&lt;br /&gt;&lt;a class="mw-redirect" title="1923 Great Kanto earthquake" href="http://en.wikipedia.org/wiki/1923_Great_Kanto_earthquake"&gt;Great Kantō earthquake&lt;/a&gt; (1923). On the Japanese island of &lt;a title="Honshū" href="http://en.wikipedia.org/wiki/Honsh%C5%AB"&gt;Honshū&lt;/a&gt;, killing over 140,000 in &lt;a title="Tokyo" href="http://en.wikipedia.org/wiki/Tokyo"&gt;Tokyo&lt;/a&gt; and environs.&lt;br /&gt;&lt;a title="1931 Hawke's Bay earthquake" href="http://en.wikipedia.org/wiki/1931_Hawke%27s_Bay_earthquake"&gt;1931 Hawke's Bay earthquake&lt;/a&gt;. Occurred in the &lt;a class="mw-redirect" title="Hawkes Bay" href="http://en.wikipedia.org/wiki/Hawkes_Bay"&gt;Hawkes Bay&lt;/a&gt; in the &lt;a title="North Island" href="http://en.wikipedia.org/wiki/North_Island"&gt;North Island&lt;/a&gt; of &lt;a title="New Zealand" href="http://en.wikipedia.org/wiki/New_Zealand"&gt;New Zealand&lt;/a&gt; leaving 256 dead.&lt;br /&gt;&lt;a title="1933 Long Beach earthquake" href="http://en.wikipedia.org/wiki/1933_Long_Beach_earthquake"&gt;1933 Long Beach earthquake&lt;/a&gt;&lt;br /&gt;&lt;a title="1935 Balochistan earthquake" href="http://en.wikipedia.org/wiki/1935_Balochistan_earthquake"&gt;1935 Balochistan earthquake&lt;/a&gt; at Quetta, Pakistan measuring 7.7 on the Richter scale. Anywhere from 30,000 to 60,000 people died&lt;br /&gt;&lt;a title="1939 Erzincan earthquake" href="http://en.wikipedia.org/wiki/1939_Erzincan_earthquake"&gt;1939 Erzincan earthquake&lt;/a&gt; at &lt;a title="Erzincan" href="http://en.wikipedia.org/wiki/Erzincan"&gt;Erzincan&lt;/a&gt;, &lt;a title="Turkey" href="http://en.wikipedia.org/wiki/Turkey"&gt;Turkey&lt;/a&gt; measuring 7.9 on the Richter scale.&lt;br /&gt;&lt;a class="new" title="Ashgabat earthquake (page does not exist)" href="http://en.wikipedia.org/w/index.php?title=Ashgabat_earthquake&amp;amp;action=edit&amp;amp;redlink=1"&gt;Ashgabat earthquake&lt;/a&gt; (1948). Earthquake in &lt;a title="Ashgabat" href="http://en.wikipedia.org/wiki/Ashgabat"&gt;Ashgabat&lt;/a&gt;, &lt;a title="Soviet Union" href="http://en.wikipedia.org/wiki/Soviet_Union"&gt;Soviet Union&lt;/a&gt; measuring 7.3 on the Richter scale killed over 110,000 (2/3 the population of the city).&lt;a title="" href="http://en.wikipedia.org/wiki/Earthquake#cite_note-12"&gt;[13]&lt;/a&gt;&lt;br /&gt;&lt;a class="mw-redirect" title="Assam earthquake of 1950" href="http://en.wikipedia.org/wiki/Assam_earthquake_of_1950"&gt;Assam earthquake of 1950&lt;/a&gt; (1950). Earthquake in &lt;a title="Assam" href="http://en.wikipedia.org/wiki/Assam"&gt;Assam&lt;/a&gt;, India measures 8.6M.&lt;br /&gt;&lt;a title="Kamchatka earthquakes" href="http://en.wikipedia.org/wiki/Kamchatka_earthquakes"&gt;Kamchatka earthquakes&lt;/a&gt; (1952 and 1737), measuring &gt;9.0.&lt;br /&gt;Great &lt;a title="Kern County earthquake" href="http://en.wikipedia.org/wiki/Kern_County_earthquake"&gt;Kern County earthquake&lt;/a&gt; (1952). This was second strongest tremor in Southern California history, epicentered 60 miles North of Los Angeles. Major damage in &lt;a title="Bakersfield, California" href="http://en.wikipedia.org/wiki/Bakersfield%2C_California"&gt;Bakersfield, California&lt;/a&gt; and &lt;a title="Kern County, California" href="http://en.wikipedia.org/wiki/Kern_County%2C_California"&gt;Kern County, California&lt;/a&gt;, while it shook the Los Angeles area.&lt;br /&gt;&lt;a title="1959 Yellowstone earthquake" href="http://en.wikipedia.org/wiki/1959_Yellowstone_earthquake"&gt;1959 Yellowstone earthquake&lt;/a&gt;, formed &lt;a title="Quake Lake" href="http://en.wikipedia.org/wiki/Quake_Lake"&gt;Quake Lake&lt;/a&gt; in southern Montana, USA&lt;br /&gt;&lt;a class="mw-redirect" title="Great Chilean Earthquake" href="http://en.wikipedia.org/wiki/Great_Chilean_Earthquake"&gt;Great Chilean Earthquake&lt;/a&gt; (1960). Strongest earthquake ever recorded,&lt;a title="" href="http://en.wikipedia.org/wiki/Earthquake#cite_note-13"&gt;[14]&lt;/a&gt; 9.5 on Moment magnitude scale, and generated &lt;a title="Tsunami" href="http://en.wikipedia.org/wiki/Tsunami"&gt;tsunamis&lt;/a&gt; throughout the Pacific ocean. It measured 9.6 on the &lt;a class="mw-redirect" title="Richter scale" href="http://en.wikipedia.org/wiki/Richter_scale"&gt;Richter scale&lt;/a&gt;. &lt;a title="" href="http://en.wikipedia.org/wiki/Earthquake#cite_note-14"&gt;[15]&lt;/a&gt;&lt;br /&gt;&lt;a title="1960 Agadir earthquake" href="http://en.wikipedia.org/wiki/1960_Agadir_earthquake"&gt;1960 Agadir earthquake&lt;/a&gt;, &lt;a title="Morocco" href="http://en.wikipedia.org/wiki/Morocco"&gt;Morocco&lt;/a&gt; with around 15,000 casualties.&lt;br /&gt;&lt;a title="1963 Skopje earthquake" href="http://en.wikipedia.org/wiki/1963_Skopje_earthquake"&gt;1963 Skopje earthquake&lt;/a&gt;, measuring 6.1 on the Richter scale kills 1,800 people, leaves another 120,000 homeless, and destroys 80% of the city.&lt;br /&gt;&lt;a title="Good Friday Earthquake" href="http://en.wikipedia.org/wiki/Good_Friday_Earthquake"&gt;Good Friday Earthquake&lt;/a&gt; (1964) In Alaska, it was the fourth biggest earthquake recorded,&lt;a title="" href="http://en.wikipedia.org/wiki/Earthquake#cite_note-15"&gt;[16]&lt;/a&gt; measuring 9.2M. and generated tsunamis throughout the Pacific ocean.&lt;br /&gt;&lt;a title="1970 Ancash earthquake" href="http://en.wikipedia.org/wiki/1970_Ancash_earthquake"&gt;Ancash earthquake&lt;/a&gt; (1970). Caused a &lt;a title="Landslide" href="http://en.wikipedia.org/wiki/Landslide"&gt;landslide&lt;/a&gt; that buried the town of &lt;a title="Yungay, Peru" href="http://en.wikipedia.org/wiki/Yungay%2C_Peru"&gt;Yungay, Peru&lt;/a&gt;; killed over 40,000 people.&lt;br /&gt;&lt;a class="mw-redirect" title="Sylmar earthquake" href="http://en.wikipedia.org/wiki/Sylmar_earthquake"&gt;Sylmar earthquake&lt;/a&gt; (1971). Caused great and unexpected destruction of freeway bridges and flyways in the &lt;a title="San Fernando Valley" href="http://en.wikipedia.org/wiki/San_Fernando_Valley"&gt;San Fernando Valley&lt;/a&gt;, leading to the first major &lt;a title="Seismic retrofit" href="http://en.wikipedia.org/wiki/Seismic_retrofit"&gt;seismic retrofits&lt;/a&gt; of these types of structures, but not at a sufficient pace to avoid the next California freeway collapse in 1989.&lt;br /&gt;&lt;a class="new" title="Managua earthquake (page does not exist)" href="http://en.wikipedia.org/w/index.php?title=Managua_earthquake&amp;amp;action=edit&amp;amp;redlink=1"&gt;Managua earthquake&lt;/a&gt; (1972), which killed more than 10,000 people and destroyed 90% of the city. The earthquake took place on &lt;a title="December 23" href="http://en.wikipedia.org/wiki/December_23"&gt;December 23&lt;/a&gt;, &lt;a title="1972" href="http://en.wikipedia.org/wiki/1972"&gt;1972&lt;/a&gt; at midnight.&lt;br /&gt;&lt;a title="Friuli" href="http://en.wikipedia.org/wiki/Friuli"&gt;Friuli&lt;/a&gt; earthquake (1976), Which killed more than 2.000 people in Northeastern &lt;a title="Italy" href="http://en.wikipedia.org/wiki/Italy"&gt;Italy&lt;/a&gt; and in the &lt;a title="Slovenian Littoral" href="http://en.wikipedia.org/wiki/Slovenian_Littoral"&gt;Slovenian Littoral&lt;/a&gt; on the 6th of May&lt;br /&gt;&lt;a title="1976 Tangshan earthquake" href="http://en.wikipedia.org/wiki/1976_Tangshan_earthquake"&gt;Tangshan earthquake&lt;/a&gt; (1976). The most destructive earthquake of modern times. The official death toll was 255,000, but many experts believe that two or three times that number died.&lt;br /&gt;&lt;a title="Guatemala" href="http://en.wikipedia.org/wiki/Guatemala"&gt;Guatemala&lt;/a&gt; &lt;a class="mw-redirect" title="Guatemala 1976 earthquake" href="http://en.wikipedia.org/wiki/Guatemala_1976_earthquake"&gt;1976 earthquake&lt;/a&gt; (1976). Causing 23,000 deaths, 77,000 injuries and the destruction of more than 250,000 homes.&lt;br /&gt;&lt;a class="new" title="Coalinga, California earthquake (page does not exist)" href="http://en.wikipedia.org/w/index.php?title=Coalinga%2C_California_earthquake&amp;amp;action=edit&amp;amp;redlink=1"&gt;Coalinga, California earthquake&lt;/a&gt; (1983). 6.5 on the Richter scale on a section of the San Andreas Fault. Six people killed, downtown &lt;a title="Coalinga, California" href="http://en.wikipedia.org/wiki/Coalinga%2C_California"&gt;Coalinga, California&lt;/a&gt; devastated and oil field blazes.&lt;br /&gt;&lt;a title="1985 Mexico City earthquake" href="http://en.wikipedia.org/wiki/1985_Mexico_City_earthquake"&gt;Great Mexican Earthquake&lt;/a&gt; (1985). Killed over 6,500 people, according to official Mexican government reports,[&lt;a title="Wikipedia:Citation needed" href="http://en.wikipedia.org/wiki/Wikipedia:Citation_needed"&gt;citation needed&lt;/a&gt;] but as many as 30,000 people are thought to have been killed (they disappeared and never reappeared after the initial Earthquakes).&lt;br /&gt;&lt;a title="Great San Salvador Earthquake" href="http://en.wikipedia.org/wiki/Great_San_Salvador_Earthquake"&gt;Great San Salvador Earthquake&lt;/a&gt; (&lt;a title="October 10" href="http://en.wikipedia.org/wiki/October_10"&gt;October 10&lt;/a&gt;, &lt;a title="1986" href="http://en.wikipedia.org/wiki/1986"&gt;1986&lt;/a&gt;). Killed over 1,500 people.&lt;br /&gt;&lt;a class="mw-redirect" title="Whittier Narrows earthquake" href="http://en.wikipedia.org/wiki/Whittier_Narrows_earthquake"&gt;Whittier Narrows earthquake&lt;/a&gt; (1987).&lt;br /&gt;&lt;a title="1989 Newcastle earthquake" href="http://en.wikipedia.org/wiki/1989_Newcastle_earthquake"&gt;1989 Newcastle earthquake&lt;/a&gt;, Australia&lt;br /&gt;&lt;a class="mw-redirect" title="Leninakan Earthquake" href="http://en.wikipedia.org/wiki/Leninakan_Earthquake"&gt;Armenian earthquake&lt;/a&gt; (1988). Killed over 25,000.&lt;br /&gt;&lt;a class="mw-redirect" title="Loma Prieta earthquake" href="http://en.wikipedia.org/wiki/Loma_Prieta_earthquake"&gt;Loma Prieta earthquake&lt;/a&gt; (1989). Severely affecting &lt;a title="Santa Cruz, California" href="http://en.wikipedia.org/wiki/Santa_Cruz%2C_California"&gt;Santa Cruz&lt;/a&gt;, &lt;a class="mw-redirect" title="San Francisco" href="http://en.wikipedia.org/wiki/San_Francisco"&gt;San Francisco&lt;/a&gt;, &lt;a title="San Jose, California" href="http://en.wikipedia.org/wiki/San_Jose%2C_California"&gt;San Jose&lt;/a&gt; and &lt;a title="Oakland, California" href="http://en.wikipedia.org/wiki/Oakland%2C_California"&gt;Oakland&lt;/a&gt; in &lt;a title="California" href="http://en.wikipedia.org/wiki/California"&gt;California&lt;/a&gt;. This is also called the &lt;a title="World Series" href="http://en.wikipedia.org/wiki/World_Series"&gt;World Series&lt;/a&gt; Earthquake. It struck as Game 3 of the &lt;a title="1989 World Series" href="http://en.wikipedia.org/wiki/1989_World_Series"&gt;1989 World Series&lt;/a&gt; was just getting underway at &lt;a class="mw-redirect" title="Candlestick Park" href="http://en.wikipedia.org/wiki/Candlestick_Park"&gt;Candlestick Park&lt;/a&gt; in &lt;a class="mw-redirect" title="San Francisco" href="http://en.wikipedia.org/wiki/San_Francisco"&gt;San Francisco&lt;/a&gt;. Revealed necessity of accelerated seismic retrofit of road and bridge structures.&lt;br /&gt;&lt;a title="1990 Iran earthquake" href="http://en.wikipedia.org/wiki/1990_Iran_earthquake"&gt;Iran Earthquake&lt;/a&gt; (1990). 7.7 on the Richter scale. Killed over 35,000 in &lt;a class="mw-redirect" title="Gilan Province" href="http://en.wikipedia.org/wiki/Gilan_Province"&gt;Gilan Province&lt;/a&gt;, southwest of &lt;a class="mw-redirect" title="Caspian sea" href="http://en.wikipedia.org/wiki/Caspian_sea"&gt;Caspian sea&lt;/a&gt;.&lt;a title="" href="http://en.wikipedia.org/wiki/Earthquake#cite_note-16"&gt;[17]&lt;/a&gt;&lt;br /&gt;&lt;a title="1990 Luzon earthquake" href="http://en.wikipedia.org/wiki/1990_Luzon_earthquake"&gt;Luzon Earthquake&lt;/a&gt; (1990). On &lt;a title="July 16" href="http://en.wikipedia.org/wiki/July_16"&gt;16 July&lt;/a&gt; &lt;a title="1990" href="http://en.wikipedia.org/wiki/1990"&gt;1990&lt;/a&gt;, an earthquake measuring 7.7 on the Richter scale struck the island of &lt;a class="mw-redirect" title="Luzon, Philippines" href="http://en.wikipedia.org/wiki/Luzon%2C_Philippines"&gt;Luzon, Philippines&lt;/a&gt;.&lt;br /&gt;&lt;a title="Landers, California earthquake" href="http://en.wikipedia.org/wiki/Landers%2C_California_earthquake"&gt;Landers, California earthquake&lt;/a&gt; (1992). Serious damage in the small town of &lt;a title="Yucca Valley, California" href="http://en.wikipedia.org/wiki/Yucca_Valley%2C_California"&gt;Yucca Valley, California&lt;/a&gt; and was felt across 10 states in Western U.S. Another tremor measured 6.4 struck 3 hours later and felt across Southern California.&lt;br /&gt;&lt;a class="mw-redirect" title="August 1993" href="http://en.wikipedia.org/wiki/August_1993"&gt;August 1993&lt;/a&gt; Guam Earthquake, measuring 8.2 on the Richter scale and lasting 60 seconds.&lt;br /&gt;&lt;a class="mw-redirect" title="1994 Northridge Earthquake" href="http://en.wikipedia.org/wiki/1994_Northridge_Earthquake"&gt;Northridge, California earthquake&lt;/a&gt; (1994). Damage showed seismic resistance deficiencies in modern low-rise apartment construction.&lt;br /&gt;&lt;a title="Neftegorsk, Sakhalin Oblast" href="http://en.wikipedia.org/wiki/Neftegorsk%2C_Sakhalin_Oblast"&gt;Sakhalin earthquake&lt;/a&gt; (1995). Measuring 7.6 on the Richter scale, killing over 2,000 people in &lt;a title="Sakhalin" href="http://en.wikipedia.org/wiki/Sakhalin"&gt;Sakhalin&lt;/a&gt;, &lt;a title="Russia" href="http://en.wikipedia.org/wiki/Russia"&gt;Russia&lt;/a&gt;.&lt;a title="" href="http://en.wikipedia.org/wiki/Earthquake#cite_note-17"&gt;[18]&lt;/a&gt;&lt;br /&gt;&lt;a title="Great Hanshin earthquake" href="http://en.wikipedia.org/wiki/Great_Hanshin_earthquake"&gt;Great Hanshin earthquake&lt;/a&gt; (1995). Killed over 6,400 people in and around &lt;a title="Kobe" href="http://en.wikipedia.org/wiki/Kobe"&gt;Kobe&lt;/a&gt;, &lt;a title="Japan" href="http://en.wikipedia.org/wiki/Japan"&gt;Japan&lt;/a&gt;.&lt;br /&gt;1998 Afghanistan earthquake (1998). 6.9 on the Richter scale. Some 125 villages were damaged and 4000 people killed.&lt;a title="" href="http://en.wikipedia.org/wiki/Earthquake#cite_note-18"&gt;[19]&lt;/a&gt;&lt;br /&gt;&lt;a class="new" title="Athens earthquake (page does not exist)" href="http://en.wikipedia.org/w/index.php?title=Athens_earthquake&amp;amp;action=edit&amp;amp;redlink=1"&gt;Athens earthquake&lt;/a&gt; (1999). 5.9 on the Richter scale, it hit &lt;a title="Athens" href="http://en.wikipedia.org/wiki/Athens"&gt;Athens&lt;/a&gt; on &lt;a title="September 7" href="http://en.wikipedia.org/wiki/September_7"&gt;September 7&lt;/a&gt;. Epicentered 10 miles north of the Greek capital, it claimed 143 lives.&lt;br /&gt;&lt;a class="mw-redirect" title="Chi-Chi earthquake" href="http://en.wikipedia.org/wiki/Chi-Chi_earthquake"&gt;Chi-Chi earthquake&lt;/a&gt; (1999) Also called the 921 earthquake. Struck &lt;a title="Taiwan" href="http://en.wikipedia.org/wiki/Taiwan"&gt;Taiwan&lt;/a&gt; on &lt;a title="September 21" href="http://en.wikipedia.org/wiki/September_21"&gt;September 21&lt;/a&gt;, &lt;a title="1999" href="http://en.wikipedia.org/wiki/1999"&gt;1999&lt;/a&gt;. Over 2,000 people killed, destroyed or damaged over ten thousand buildings. Caused world computer prices to rise sharply.&lt;br /&gt;&lt;a title="Armenia, Colombia" href="http://en.wikipedia.org/wiki/Armenia%2C_Colombia"&gt;Armenia, Colombia&lt;/a&gt; (1999) 6.2 on the Richter scale, Killed over 2,000 in the Colombian Coffee Grown Zone.&lt;br /&gt;1999 &lt;a title="1999 İzmit earthquake" href="http://en.wikipedia.org/wiki/1999_%C4%B0zmit_earthquake"&gt;İzmit earthquake&lt;/a&gt; measuring 7.5 on the Richter scale and killed over 17,000 in northwestern Turkey.&lt;br /&gt;&lt;a title="Hector Mine" href="http://en.wikipedia.org/wiki/Hector_Mine"&gt;Hector Mine earthquake&lt;/a&gt; (1999). 7.1 on the Richter scale, epicentered 30 miles east of &lt;a title="Barstow, California" href="http://en.wikipedia.org/wiki/Barstow%2C_California"&gt;Barstow, California&lt;/a&gt;, widely felt in California and &lt;a title="Nevada" href="http://en.wikipedia.org/wiki/Nevada"&gt;Nevada&lt;/a&gt;.&lt;br /&gt;1999 &lt;a class="mw-redirect" title="Düzce earthquake" href="http://en.wikipedia.org/wiki/D%C3%BCzce_earthquake"&gt;Düzce earthquake&lt;/a&gt; at &lt;a title="Düzce" href="http://en.wikipedia.org/wiki/D%C3%BCzce"&gt;Düzce&lt;/a&gt;, &lt;a title="Turkey" href="http://en.wikipedia.org/wiki/Turkey"&gt;Turkey&lt;/a&gt; measuring 7.2 on the Richter scale.&lt;br /&gt;&lt;a title="2000 Baku earthquake" href="http://en.wikipedia.org/wiki/2000_Baku_earthquake"&gt;Baku earthquake&lt;/a&gt; (2000).&lt;br /&gt;&lt;a name="21st_century"&gt;&lt;/a&gt;&lt;br /&gt;[&lt;a title="Edit section: 21st century" href="http://en.wikipedia.org/w/index.php?title=Earthquake&amp;amp;action=edit&amp;amp;section=15"&gt;edit&lt;/a&gt;] 21st century&lt;br /&gt;&lt;a class="mw-redirect" title="Nisqually Earthquake" href="http://en.wikipedia.org/wiki/Nisqually_Earthquake"&gt;Nisqually Earthquake&lt;/a&gt; (2001).&lt;br /&gt;&lt;a title="2001 El Salvador earthquakes" href="http://en.wikipedia.org/wiki/2001_El_Salvador_earthquakes"&gt;El Salvador earthquakes&lt;/a&gt; (2001). 7.9 (&lt;a title="January 13" href="http://en.wikipedia.org/wiki/January_13"&gt;13 January&lt;/a&gt;) and 6.6 (&lt;a title="February 13" href="http://en.wikipedia.org/wiki/February_13"&gt;13 February&lt;/a&gt;) magnitudes, killed more than 1,100 people.&lt;br /&gt;&lt;a class="mw-redirect" title="2001 Gujarat Earthquake" href="http://en.wikipedia.org/wiki/2001_Gujarat_Earthquake"&gt;Gujarat Earthquake&lt;/a&gt; (&lt;a title="January 26" href="http://en.wikipedia.org/wiki/January_26"&gt;26 January&lt;/a&gt; &lt;a title="2001" href="http://en.wikipedia.org/wiki/2001"&gt;2001&lt;/a&gt;).&lt;br /&gt;&lt;a title="2002 Hindu Kush earthquakes" href="http://en.wikipedia.org/wiki/2002_Hindu_Kush_earthquakes"&gt;Hindu Kush earthquakes&lt;/a&gt; (2002). Over 1,100 killed.&lt;br /&gt;&lt;a title="2002 Molise earthquake" href="http://en.wikipedia.org/wiki/2002_Molise_earthquake"&gt;Molise earthquake&lt;/a&gt; (2002) 26 killed.&lt;br /&gt;&lt;a title="Bam, Iran" href="http://en.wikipedia.org/wiki/Bam%2C_Iran#2003_earthquake"&gt;Bam Earthquake&lt;/a&gt; (2003). Over 40,000 people are reported dead.&lt;br /&gt;&lt;a class="mw-redirect" title="Parkfield earthquake" href="http://en.wikipedia.org/wiki/Parkfield_earthquake"&gt;Parkfield, California earthquake&lt;/a&gt; (2004). Not large (6.0), but the most anticipated and intensely instrumented earthquake ever recorded and likely to offer insights into predicting future earthquakes elsewhere on similar slip-strike fault structures.&lt;br /&gt;&lt;a title="2004 Chūetsu earthquake" href="http://en.wikipedia.org/wiki/2004_Ch%C5%ABetsu_earthquake"&gt;Chūetsu earthquake&lt;/a&gt; (2004).&lt;br /&gt;&lt;a title="2004 Indian Ocean earthquake" href="http://en.wikipedia.org/wiki/2004_Indian_Ocean_earthquake"&gt;Sumatra-Andaman Earthquake&lt;/a&gt; (26 December 2004). By some estimates, the second largest earthquake in recorded history (estimates of magnitude vary between 9.1&lt;a title="" href="http://en.wikipedia.org/wiki/Earthquake#cite_note-19"&gt;[20]&lt;/a&gt; and 9.3). Epicentered off the coast of the &lt;a title="Indonesia" href="http://en.wikipedia.org/wiki/Indonesia"&gt;Indonesian&lt;/a&gt; island of &lt;a title="Sumatra" href="http://en.wikipedia.org/wiki/Sumatra"&gt;Sumatra&lt;/a&gt;, this massive earthquake triggered a series of gigantic &lt;a title="Tsunami" href="http://en.wikipedia.org/wiki/Tsunami"&gt;tsunamis&lt;/a&gt; that smashed onto the shores of a number of nations, causing 230,000 fatalities.&lt;br /&gt;&lt;a class="mw-redirect" title="2005 Sumatran earthquake" href="http://en.wikipedia.org/wiki/2005_Sumatran_earthquake"&gt;Sumatran (Nias) Earthquake&lt;/a&gt; (2005).&lt;br /&gt;&lt;a title="2005 Fukuoka earthquake" href="http://en.wikipedia.org/wiki/2005_Fukuoka_earthquake"&gt;Fukuoka earthquake&lt;/a&gt; (2005).&lt;br /&gt;&lt;a class="new" title="Northern Chile Earthquake (page does not exist)" href="http://en.wikipedia.org/w/index.php?title=Northern_Chile_Earthquake&amp;amp;action=edit&amp;amp;redlink=1"&gt;Northern Chile Earthquake&lt;/a&gt; (2005). 7.9 (&lt;a title="June 13" href="http://en.wikipedia.org/wiki/June_13"&gt;13 June&lt;/a&gt;). Killed only 15 people, but left many poor families homeless.&lt;br /&gt;&lt;a title="2005 Kashmir earthquake" href="http://en.wikipedia.org/wiki/2005_Kashmir_earthquake"&gt;Kashmir earthquake&lt;/a&gt; (2005) (also known as the Great Pakistan earthquake). Killed over 79,000 people; and many more injured.&lt;br /&gt;&lt;a title="2005 Lake Tanganyika earthquake" href="http://en.wikipedia.org/wiki/2005_Lake_Tanganyika_earthquake"&gt;Lake Tanganyika earthquake&lt;/a&gt; (2005).&lt;br /&gt;&lt;a title="May 2006 Java earthquake" href="http://en.wikipedia.org/wiki/May_2006_Java_earthquake"&gt;May 2006 Java earthquake&lt;/a&gt; (2006).&lt;br /&gt;&lt;a title="July 2006 Java earthquake" href="http://en.wikipedia.org/wiki/July_2006_Java_earthquake"&gt;July 2006 7.7 magnitude Java earthquake&lt;/a&gt; which triggered &lt;a title="Tsunami" href="http://en.wikipedia.org/wiki/Tsunami"&gt;tsunamis&lt;/a&gt; (2006).&lt;br /&gt;&lt;a title="2006 Hawaii earthquake" href="http://en.wikipedia.org/wiki/2006_Hawaii_earthquake"&gt;October 2006 6.6 magnitude Kona, Hawaii earthquake&lt;/a&gt; (2006).&lt;br /&gt;&lt;a title="2006 Kuril Islands earthquake" href="http://en.wikipedia.org/wiki/2006_Kuril_Islands_earthquake"&gt;November 2006 8.1 magnitude north of Japan&lt;/a&gt; (2006).&lt;br /&gt;&lt;a title="2006 Hengchun earthquake" href="http://en.wikipedia.org/wiki/2006_Hengchun_earthquake"&gt;December 26, 2006, 7.2 magnitude, southwest of Taiwan&lt;/a&gt; (2006).&lt;br /&gt;&lt;a title="March 2007 Sumatra earthquakes" href="http://en.wikipedia.org/wiki/March_2007_Sumatra_earthquakes"&gt;Sumatra Earthquakes March 06, 2007, 6.4 and 6.3 magnitude, Sumatra, Indonesia&lt;/a&gt; (2007).&lt;br /&gt;&lt;a title="2007 Noto earthquake" href="http://en.wikipedia.org/wiki/2007_Noto_earthquake"&gt;March 25, 2007, 6.9 magnitude, off the west coast of Honshū, Japan&lt;/a&gt; (2007).&lt;br /&gt;&lt;a title="2007 Solomon Islands earthquake" href="http://en.wikipedia.org/wiki/2007_Solomon_Islands_earthquake"&gt;April 1, 2007, 8.1 magnitude, Solomon Islands&lt;/a&gt; (2007).&lt;br /&gt;&lt;a class="mw-redirect" title="2007 Guatemala Earthquake" href="http://en.wikipedia.org/wiki/2007_Guatemala_Earthquake"&gt;2007 Guatemala Earthquake&lt;/a&gt; 6.7 magnitude (2007).&lt;br /&gt;&lt;a class="mw-redirect" title="2007 Niigata earthquake" href="http://en.wikipedia.org/wiki/2007_Niigata_earthquake"&gt;July 16, 2007, 6.6 magnitude, Niigata prefecture, Japan&lt;/a&gt; (2007).&lt;br /&gt;&lt;a title="2007 Peru earthquake" href="http://en.wikipedia.org/wiki/2007_Peru_earthquake"&gt;2007 Peru earthquake&lt;/a&gt; 8.0 magnitude, August 15 (2007)&lt;a title="" href="http://en.wikipedia.org/wiki/Earthquake#cite_note-ECPE-20"&gt;[21]&lt;/a&gt;&lt;br /&gt;&lt;a title="September 2007 Sumatra earthquakes" href="http://en.wikipedia.org/wiki/September_2007_Sumatra_earthquakes"&gt;September 2007 Sumatra earthquakes&lt;/a&gt; 8.0 magnitude September 12 (2007)&lt;a title="" href="http://en.wikipedia.org/wiki/Earthquake#cite_note-21"&gt;[22]&lt;/a&gt;&lt;br /&gt;&lt;a title="2007 Antofagasta earthquake" href="http://en.wikipedia.org/wiki/2007_Antofagasta_earthquake"&gt;November 14, 2007, 7.7 magnitude, Antofagasta, Chile&lt;/a&gt; (2007).&lt;br /&gt;&lt;a class="new" title="November 2007 Caribbean Sea earthquake (page does not exist)" href="http://en.wikipedia.org/w/index.php?title=November_2007_Caribbean_Sea_earthquake&amp;amp;action=edit&amp;amp;redlink=1"&gt;November 29, 2007, 7.4 magnitude, Caribbean Sea&lt;/a&gt; (2007).&lt;br /&gt;&lt;a title="2007 Gisborne earthquake" href="http://en.wikipedia.org/wiki/2007_Gisborne_earthquake"&gt;December 20, 2007 6.8 magnitude, Gisborne, New Zealand&lt;/a&gt; (2007).&lt;br /&gt;&lt;a title="February 20" href="http://en.wikipedia.org/wiki/February_20"&gt;February 20&lt;/a&gt;, &lt;a title="2008" href="http://en.wikipedia.org/wiki/2008"&gt;2008&lt;/a&gt; &lt;a title="Sumatra" href="http://en.wikipedia.org/wiki/Sumatra"&gt;Sumatra&lt;/a&gt; earthquake 7.5 magnitude&lt;a title="" href="http://en.wikipedia.org/wiki/Earthquake#cite_note-22"&gt;[23]&lt;/a&gt;&lt;br /&gt;&lt;a title="February 25" href="http://en.wikipedia.org/wiki/February_25"&gt;February 25&lt;/a&gt;, &lt;a title="2008" href="http://en.wikipedia.org/wiki/2008"&gt;2008&lt;/a&gt; &lt;a title="Sumatra" href="http://en.wikipedia.org/wiki/Sumatra"&gt;Sumatra&lt;/a&gt; earthquake 7.3 magnitude. The quake was centered about 160 km (100 miles) south-southwest of &lt;a title="Padang" href="http://en.wikipedia.org/wiki/Padang"&gt;Padang&lt;/a&gt;. The &lt;a title="Pacific Tsunami Warning Center" href="http://en.wikipedia.org/wiki/Pacific_Tsunami_Warning_Center"&gt;Pacific Tsunami Warning Center&lt;/a&gt; issued a local &lt;a title="Tsunami" href="http://en.wikipedia.org/wiki/Tsunami"&gt;tsunami&lt;/a&gt; watch.&lt;a title="" href="http://en.wikipedia.org/wiki/Earthquake#cite_note-23"&gt;[24]&lt;/a&gt;&lt;br /&gt;&lt;a title="March 21" href="http://en.wikipedia.org/wiki/March_21"&gt;March 21&lt;/a&gt;, &lt;a title="2008" href="http://en.wikipedia.org/wiki/2008"&gt;2008&lt;/a&gt; &lt;a title="China" href="http://en.wikipedia.org/wiki/China"&gt;China&lt;/a&gt; earthquake 7.2 magnitude. The quake happened in &lt;a class="mw-redirect" title="Yutian County, Xinjiang" href="http://en.wikipedia.org/wiki/Yutian_County%2C_Xinjiang"&gt;Yutian County, Xinjiang&lt;/a&gt;, a remote region in the &lt;a title="Kunlun Mountains" href="http://en.wikipedia.org/wiki/Kunlun_Mountains"&gt;Kunlun Mountains&lt;/a&gt; far from any residential areas.&lt;a title="" href="http://en.wikipedia.org/wiki/Earthquake#cite_note-24"&gt;[25]&lt;/a&gt;&lt;br /&gt;&lt;a title="March 29" href="http://en.wikipedia.org/wiki/March_29"&gt;March 29&lt;/a&gt;, &lt;a title="2008" href="http://en.wikipedia.org/wiki/2008"&gt;2008&lt;/a&gt; &lt;a title="Sumatra" href="http://en.wikipedia.org/wiki/Sumatra"&gt;Sumatra&lt;/a&gt; earthquake 6.3 magnitude. The epicenter was about 175 miles (281 kilometers) south of &lt;a title="Banda Aceh" href="http://en.wikipedia.org/wiki/Banda_Aceh"&gt;Banda Aceh&lt;/a&gt; -- in a region hard-hit by the &lt;a title="2004 Indian Ocean earthquake" href="http://en.wikipedia.org/wiki/2004_Indian_Ocean_earthquake"&gt;2004 Indian Ocean earthquake&lt;/a&gt;. It could trigger a &lt;a title="Tsunami" href="http://en.wikipedia.org/wiki/Tsunami"&gt;tsunami&lt;/a&gt; on coasts near its epicenter, the &lt;a title="Pacific Tsunami Warning Center" href="http://en.wikipedia.org/wiki/Pacific_Tsunami_Warning_Center"&gt;Pacific Tsunami Warning Center&lt;/a&gt; told.&lt;a title="" href="http://en.wikipedia.org/wiki/Earthquake#cite_note-25"&gt;[26]&lt;/a&gt;&lt;br /&gt;&lt;a title="April 8" href="http://en.wikipedia.org/wiki/April_8"&gt;April 8&lt;/a&gt;, &lt;a title="2008" href="http://en.wikipedia.org/wiki/2008"&gt;2008&lt;/a&gt; earthquake 7.5 magnitude. The quake was in the southern &lt;a title="Pacific Ocean" href="http://en.wikipedia.org/wiki/Pacific_Ocean"&gt;Pacific Ocean&lt;/a&gt;, about 85 kilometers southwest of &lt;a title="Vanuatu" href="http://en.wikipedia.org/wiki/Vanuatu"&gt;Vanuatu&lt;/a&gt;.&lt;br /&gt;&lt;a title="May 12" href="http://en.wikipedia.org/wiki/May_12"&gt;May 12&lt;/a&gt;, &lt;a title="2008" href="http://en.wikipedia.org/wiki/2008"&gt;2008&lt;/a&gt; &lt;a title="2008 Sichuan earthquake" href="http://en.wikipedia.org/wiki/2008_Sichuan_earthquake"&gt;earthquake 7.9 magnitude&lt;/a&gt; about 60 kilometers northwest of &lt;a title="Chengdu" href="http://en.wikipedia.org/wiki/Chengdu"&gt;Chengdu&lt;/a&gt; in the &lt;a title="Sichuan" href="http://en.wikipedia.org/wiki/Sichuan"&gt;Sichuan&lt;/a&gt; province in &lt;a title="China" href="http://en.wikipedia.org/wiki/China"&gt;China&lt;/a&gt;, killed about 10,000 people, expected to soar.&lt;br /&gt;&lt;a id="Earthquakes_in_mythology_and_religion" name="Earthquakes_in_mythology_and_religion"&gt;&lt;/a&gt;&lt;br /&gt;[&lt;a title="Edit section: Earthquakes in mythology and religion" href="http://en.wikipedia.org/w/index.php?title=Earthquake&amp;amp;action=edit&amp;amp;section=16"&gt;edit&lt;/a&gt;] Earthquakes in mythology and religion&lt;br /&gt;In &lt;a title="Norse mythology" href="http://en.wikipedia.org/wiki/Norse_mythology"&gt;Norse mythology&lt;/a&gt;, earthquakes were explained as the violent struggling of the god &lt;a title="Loki" href="http://en.wikipedia.org/wiki/Loki"&gt;Loki&lt;/a&gt;. When Loki, &lt;a class="mw-redirect" title="Aesir" href="http://en.wikipedia.org/wiki/Aesir"&gt;god&lt;/a&gt; of mischief and strife, murdered &lt;a title="Baldr" href="http://en.wikipedia.org/wiki/Baldr"&gt;Baldr&lt;/a&gt;, god of beauty and light, he was punished by being bound in a cave with a poisonous serpent placed above his head dripping venom. Loki's wife &lt;a title="Sigyn" href="http://en.wikipedia.org/wiki/Sigyn"&gt;Sigyn&lt;/a&gt; stood by him with a bowl to catch the poison, but whenever she had to empty the bowl the poison would drip on Loki's face, forcing him to jerk his head away and thrash against his bonds, causing the earth to tremble.&lt;a title="" href="http://en.wikipedia.org/wiki/Earthquake#cite_note-26"&gt;[27]&lt;/a&gt;&lt;br /&gt;In &lt;a title="Greek mythology" href="http://en.wikipedia.org/wiki/Greek_mythology"&gt;Greek mythology&lt;/a&gt;, &lt;a title="Poseidon" href="http://en.wikipedia.org/wiki/Poseidon"&gt;Poseidon&lt;/a&gt; was the god of earthquakes.&lt;a title="" href="http://en.wikipedia.org/wiki/Earthquake#cite_note-27"&gt;[28]&lt;/a&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/1010569638007681966-8877076296103247086?l=priyameena.blogspot.com'/&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://priyameena.blogspot.com/feeds/8877076296103247086/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='https://www.blogger.com/comment.g?blogID=1010569638007681966&amp;postID=8877076296103247086' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/1010569638007681966/posts/default/8877076296103247086'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/1010569638007681966/posts/default/8877076296103247086'/><link rel='alternate' type='text/html' href='http://priyameena.blogspot.com/2008/05/earthquake.html' title='EARTHQUAKE'/><author><name>priyanka gupta</name><uri>http://www.blogger.com/profile/03282159976818127425</uri><email>noreply@blogger.com</email><gd:extendedProperty xmlns:gd='http://schemas.google.com/g/2005' name='OpenSocialUserId' value='11703516926278611720'/></author><thr:total xmlns:thr='http://purl.org/syndication/thread/1.0'>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-1010569638007681966.post-7498914661504035536</id><published>2008-02-12T21:13:00.000-08:00</published><updated>2008-02-12T21:16:35.449-08:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='mobile hazard'/><category scheme='http://www.blogger.com/atom/ns#' term='hazard'/><category scheme='http://www.blogger.com/atom/ns#' term='commnication'/><title type='text'>Are Mobile Telephone Communication Antennas a Health Hazard?</title><content type='html'>Is the radiation from mobile phone base station antennas a health hazard?&lt;br /&gt;&lt;br /&gt;&lt;br /&gt;Introduction:&lt;br /&gt;There are mobile phone base station antennas on towers and buildings throughout Australia’s metropolitan areas. These antennas are part of the mobile (or cellular) telephone network and they emit radiofrequency (RF) radiation. This fact sheet provides information about the possibility of adverse health effects arising from exposure to this radiation.&lt;br /&gt;Current research indicates that no adverse health effects should be expected from exposure to the RF radiation from mobile phone base station antennas. Read on for more detail.&lt;br /&gt;Antenna Description and Operation&lt;br /&gt;When a call is made from a mobile telephone, RF signals are transmitted between its antenna and the antenna at a nearby base station. The telephone call is then routed through telephone network (cable or radio) to the destination telephone.&lt;br /&gt;Mobile telephones emit signals at the frequency of around 800 MHz for the CDMA (Code Division Multiple Access) network, 900 &amp;amp; 1800 MHz for the GSM (Global System for Mobile Communication) network and 2100 MHz for the 3G network. These signals are picked up by antennas which are on the towers. The signals may also be transmitted between base stations and are in a higher frequency range, 15 to 23 gigahertz, and radiated as a very narrow beam by dish shaped antennas, also mounted near the top of the tower.&lt;br /&gt;Radio Frequency Radiation&lt;br /&gt;RF radiation, as well as ultraviolet radiation, visible light, infrared radiation and power frequency fields, are types of non-ionising radiation. These radiations, together with ionising electromagnetic radiation (X radiation and gamma radiation) make up the electromagnetic spectrum (Download a &lt;a class="docLink" title="A chart of the electromagnetic spectrum" href="http://www.arpansa.gov.au/pubs/emr/spectrum.pdf"&gt;chart (PDF 384kb)&lt;/a&gt; of the electromagnetic spectrum).&lt;br /&gt;When ionising radiations collide with biological material, they create positively and negatively charged particles, which may have adverse effects. Non-ionising radiations cannot create such particles. As far as is currently known, RF radiation, for example, can only cause the molecules in biological material to vibrate and thereby generate heat.&lt;br /&gt;Exposure Levels and Recommended Limits&lt;br /&gt;The exposure levels of RF radiation are measured in microwatts per square centimeter (abbreviated as μW/cm2). One μW is a millionth of a watt. The maximum exposure levels measured adjacent to the base station towers are less than 2 μW/cm2. The exposure level decreases with increasing distance from the base of the tower.&lt;br /&gt;These levels can be compared with 450 μW/cm2, which is the exposure limit at 900MHz for members of the public (that is, unlimited exposure duration) recommended by the &lt;a href="http://www.arpansa.gov.au/Publications/Codes/rps3.cfm"&gt;ARPANSA Radiation Protection Standard - "Maximum exposure levels to radiofrequency fields - 3kHz to 300GHz"&lt;/a&gt;&lt;br /&gt;Health Effects&lt;br /&gt;Current research indicates that, at the exposure levels indicated above, RF radiation is not known to have any adverse health effects.&lt;br /&gt;It is considered that rises in tissue or body temperature of about 1.0 oC or more are required before any adverse effects will occur. In cases of pregnancy, rises in the temperature of the foetus of 2.5 to 5 oC are necessary before defects are seen in the newborn. These temperature rises will not occur unless the exposure level is greatly in excess of the Australian Standard mentioned above. Exposure to the low level of RF radiation emitted from base station antennas will not, in fact, cause any noticeable temperature rise.&lt;br /&gt;There are many reports in the literature of research on non-thermal effects, usually of a subjective nature. Studies that have investigated if RF radiation affects biological cells, other than by heating them, are inconclusive. In addition, the exposure levels used in these studies are higher than those mentioned above.&lt;br /&gt;The present concern that people have about RF exposure is whether these non-thermal effects also include cancer. While human studies to assess the possibility that RF exposure increases the risk of cancer are few in number, laboratory studies do not provide evidence to support the notion that RF fields cause cancer. Review groups evaluating the state of knowledge about possible links between RF exposure and excess risk of cancer have concluded that there is no clear evidence for any links. The Australian Radiation Protection and Nuclear Safety Agency continues to closely monitor the research being conducted in this field.&lt;br /&gt;Conclusion&lt;br /&gt;No adverse health effects are expected from continuous exposure to the RF radiation emitted by the antennas on mobile telephone base station towers.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/1010569638007681966-7498914661504035536?l=priyameena.blogspot.com'/&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://priyameena.blogspot.com/feeds/7498914661504035536/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='https://www.blogger.com/comment.g?blogID=1010569638007681966&amp;postID=7498914661504035536' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/1010569638007681966/posts/default/7498914661504035536'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/1010569638007681966/posts/default/7498914661504035536'/><link rel='alternate' type='text/html' href='http://priyameena.blogspot.com/2008/02/are-mobile-telephone-communication.html' title='Are Mobile Telephone Communication Antennas a Health Hazard?'/><author><name>priyanka gupta</name><uri>http://www.blogger.com/profile/03282159976818127425</uri><email>noreply@blogger.com</email><gd:extendedProperty xmlns:gd='http://schemas.google.com/g/2005' name='OpenSocialUserId' value='11703516926278611720'/></author><thr:total xmlns:thr='http://purl.org/syndication/thread/1.0'>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-1010569638007681966.post-710608941057293615</id><published>2008-02-08T22:08:00.000-08:00</published><updated>2008-02-08T22:11:11.377-08:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='mobile hazard'/><category scheme='http://www.blogger.com/atom/ns#' term='cordless phone hazard'/><category scheme='http://www.blogger.com/atom/ns#' term='dect hazard'/><title type='text'>Cordless phones: the unspoken DECT hazard at home and at work</title><content type='html'>Cordless phones: the unspoken DECT hazard at home and at work&lt;br /&gt;&lt;br /&gt;Why talk about DECT phones on a TETRA website? One main reason is to help determine causes of symptoms that might be attributed falsely to TETRA. We have heard and found many reports of similar adverse symptoms that are more likely to be caused by DECT (Digital Electronic Cordless Telephones), and indeed that have been eliminated by stopping using these phones. You will be unaware of what they do, but if you have one, read the following carefully. Many people will be equally unaware of neighbours using DECT, whose pulses penetrate right through their walls. DECT comes with no guidance and no health warnings. This must be wrong.&lt;br /&gt;About DECT Cordless Telephones&lt;br /&gt;All modern (DECT) digital cordless phones emit the same type of pulsed microwave radiation (about 1.8 GHz) as ordinary (GSM) mobile phones. Emissions can be about 6 V/m within a metre of the base unit, for as long as it is plugged in. These base stations emit their radiation even when the phone is not in use. All DECT base units emit microwaves continuously 24 hours a day as long as they are plugged in. For this reason cordless phones are regarded as bad news. The latest Lennart Hardell paper on mobile phone use and brain tumours (× 3 for 5 years use and × 3 to 4 for 10 years use) also show a dose response increased brain cancer risk for long-term (over 5 years) regular cordless phone use. A DECT phone is a mobile phone, and its base is a mobile phone mast in your house or office. You must use one? Keep the base unit and remote extra handsets away from where you sit or sleep, and remember that you are transmitting into neighbouring property through your walls.&lt;br /&gt;Unlike mobile phones, DECT cordless phones work at a fixed power. Mobiles turn their power down to the lowest level possible, so when you are near a base station this can be much lower than a DECT cordless. DECT pulses are far more aggressive than for mobiles.&lt;br /&gt;Note: DECT phones are now being manufactured and available in Germany, and now in the UK that only transmit from the base when the handset is lifted. Of course, these are not sold as a ‘safer’ variety, but as ‘lower emission’. Lower emissions matter to the more wary manufacturers, who nevertheless claim that there is not much demand. They are safer – to everyone. But don’t be deceived, the handset is still a GSM mobile phone. Read on ...&lt;br /&gt;Orchid have are now producing their 3rd generation ‘low radiation’ DECT cordless phones – their main advantages over the previous models are:&lt;br /&gt;There are no microwave emissions when the phone is not being used. When a call is ended both the phone and the base station go into ‘sleep mode’ (no microwave radiation) until either a call is received or made. There is no need to return the handset back to the base station for ‘sleep mode’ to become operative.&lt;br /&gt;The phone/base station adjust their power output depending on how far away the base station is from the handset. It you make a call up to several meters from the base station power output is reduced by as much as 75%.&lt;br /&gt;&lt;a href="http://www.lowradiation.co.uk/" target="_blank"&gt;Rowtex Limited&lt;/a&gt; has now taken over the sales and distribution of all Orchid Low Radiation phones.&lt;br /&gt;Mobile phone concerns&lt;br /&gt;A team led by Professor Kjell Mild, a Swedish biophysicist, who has produced a number of many leading mobile-phone health effects papers has published an update on his brain-tumour work in the summer of 2001, when he discussed his results to date at an international conference chaired by Alasdair Philips of &lt;a href="htp://www.powerwatch.org.uk/" target="_blank"&gt;Powerwatch&lt;/a&gt;.&lt;br /&gt;Another study by Dr Lennart Hardell, published in the International Journal of Oncology, was based on the analysis of 1,600 tumour victims who had been using mobile phones for up to 10 years before being diagnosed. Prof. Mild now states: ‘The evidence for a connection between phone use and cancer is clear and convincing. The more you use phones and the greater the number of years you have them, the greater the risk of brain tumours. ... Mobile phones are here to stay so my advice is never to use one without a hands-free headset.’&lt;br /&gt;An earlier study by Mild, a cancer specialist, linked brain tumours to the use of analogue mobile phones. The new research repeated this and also looked at digital mobiles and DECT cordless phones. It showed that all three types were linked with increased tumour rates. The extra tumours only start to really show up after about 5 years use, but there is increasing dose-related-response with minutes of use per month and number of years of use.&lt;br /&gt;Since 1980, the number of acoustic neuromas (a rare tumour) diagnosed in Britain has risen from one in every 100,000 of the population to one in 80,000 a year. Some (but not all) other types of tumour also show an increase.&lt;br /&gt;Dr Richard Sullivan, head of clinical programmes at Cancer Research UK and quoted in the &lt;a href="http://www.pamex.ie/reports/sundaytimesarticle.pdf" target="_blank"&gt;Sunday Times on 16th March 2003&lt;/a&gt;, said the study was worrying. ‘It suggests a strong link between mobile phones and brain tumours. We now need a full-scale study.’&lt;br /&gt;On 14 October a study by the &lt;a href="http://www.medicalnewstoday.com/medicalnews.php?newsid=14937" target="_blank"&gt;Karolinska Institute&lt;/a&gt; in Sweden found a pronounced risk of acoustic nuroma (cancer) from use of mobile phones over a ten year period (imagine: aged just from 14 to 24: ages of many big users of mobile phones).&lt;br /&gt;DECT pulse frequency concern&lt;br /&gt;It is important to put out a warning about DECT phones, as they could be up to 100 times worse than an ordinary mobile, particularly if used in built up areas. The reason for this is the frequency of the pulse. DECT pulses at 100Hz whilst a GSM mobile pulses at 217Hz. Remember, the lower the pulsing frequency, the stronger the biological effect. It’s the pulsing within the ELF (extremely low frequency) range we have to be concerned about. That’s why TETRA is so dangerous. It pulses at 17.6Hz, right within the human beta brainwave rhythm range. Dr von Klitzing, who was one of the Medical Physicists signing the &lt;a href="http://www.emrnetwork.org/news/IGUMED_english.pdf" target="_blank"&gt;Freiburger Appeal&lt;/a&gt;, reported his research regarding DECT phones. His research on blood samples taken from children in the vicinity of DECT phones showed that the red blood corpuscles did not ‘ripen out properly’ (a direct translation of his words). The physical signs were: listlessness and/or aggression, pallor, sleeplessness etc. This could be reversed with the removal of the phone.&lt;br /&gt;Choice&lt;br /&gt;In your own home you have a choice, and it is yours. If you have reservations as a result of reading up on DECT, at least revert to an older style analogue cordless phone – or put up with wires!&lt;br /&gt;Neighbours’ phones are another matter. If you know where such a phone base is, you may decide to try foil on the wall in a large patch, to screen the DECT out. If it works, you might prefer to install it more permanently under wallpaper. But do note that microwaves tend to run around such barriers like water around a stone in a stream, so a small phone-sized patch will not work. (Findings from using an Acousticom detector.)&lt;br /&gt;If you find your foil disrupts the neighbouring phone, you don’t want to get into a dispute, with one of you moving the phone and the other moving the screen. Try and explain the problem in an open way, using the research listed here.&lt;br /&gt;DECT in the office? Again an emotive subject. All your employer will do is refer to the Health and Safety Executive, who refer to the NRPB, who cite the ICNIRP (if it doesn’t heat you it can’t harm you) guidelines. These are wholly inappropriate, so employees have (a) no guidance and (b) no way to assess exposure in the office. The manufacturers give no advice on density of DECT per square metre. If you are sensitive to DECT, try to explain what you experience and ask for a wired phone. But I know it may not be easy.&lt;br /&gt;Signs of change&lt;br /&gt;One might ask why, if there is absolutely nothing to worry about from such a small radiation source as DECT, there has been such medical concern, and now, industry response. Here is a press notice ‘&lt;a href="http://www.bfs.de/bfs/presse/pr06/pr0602" target="_blank"&gt;DECT – radiation source in the dwelling&lt;/a&gt;’ from the German Bundesamot für Strahlenschutz (Federal Office for Radiation Protection) [&lt;a href="http://www.tetrawatch.net/media/bfs_dect.pdf" target="_blank"&gt;translation&lt;/a&gt;]. The issue is that DECT does not need to transmit continuously. And so a new DECT is being manufactured in Germany that does not transmit continuously, and only as required. In fact it is so popular, they cannot make them fast enough.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/1010569638007681966-710608941057293615?l=priyameena.blogspot.com'/&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://priyameena.blogspot.com/feeds/710608941057293615/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='https://www.blogger.com/comment.g?blogID=1010569638007681966&amp;postID=710608941057293615' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/1010569638007681966/posts/default/710608941057293615'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/1010569638007681966/posts/default/710608941057293615'/><link rel='alternate' type='text/html' href='http://priyameena.blogspot.com/2008/02/cordless-phones-unspoken-dect-hazard-at.html' title='Cordless phones: the unspoken DECT hazard at home and at work'/><author><name>priyanka gupta</name><uri>http://www.blogger.com/profile/03282159976818127425</uri><email>noreply@blogger.com</email><gd:extendedProperty xmlns:gd='http://schemas.google.com/g/2005' name='OpenSocialUserId' value='11703516926278611720'/></author><thr:total xmlns:thr='http://purl.org/syndication/thread/1.0'>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-1010569638007681966.post-6895867963606049316</id><published>2008-02-08T22:02:00.000-08:00</published><updated>2008-02-08T22:07:49.607-08:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='mobile hazard'/><category scheme='http://www.blogger.com/atom/ns#' term='cordless phone hazard'/><category scheme='http://www.blogger.com/atom/ns#' term='dect hazard'/><title type='text'>MOBILE PHONES HAZARD.</title><content type='html'>CORDLESS PHONES: THE (DECT) HAZARD.&lt;br /&gt;&lt;br /&gt;Extremely low frequency pulsed electromagnetic radiation does affect living organisms. That means you and me - We are the experiment!!&lt;br /&gt;There have been many reports of adverse symptoms possibly caused by DECT (Digital Electronic Cordless Telephones), and reportedly eliminated by stopping the use of these phones. Many people will be equally unaware of neighbours using DECT, whose pulses penetrate right through their walls. DECT comes with no guidance and no health warnings.&lt;br /&gt;About DECT Cordless TelephonesAll modern (DECT) digital cordless phones emit pulsed microwave radiation (about 1.8 GHz), same as ordinary (GSM) mobile phones. Emissions can be around 6 V/m within a metre of the base unit, while powered. All DECT base units emit microwaves continuously as long as they are plugged in. The latest Lennart Hardell paper on mobile phone use and brain tumours (× 3 for 5 years use and × 3 to 4 for 10 years use) shows a dose response increased brain cancer risk for long-term regular cordless phone use. A DECT phone is a mobile phone, but its base station is a mobile phone mast in your house or office. If you must use one, keep the base unit and remote extra handsets away from where you sit or sleep.&lt;br /&gt;Unlike mobile phones, DECT cordless phones opeate at fixed power levels. Mobiles turn their power down to the lowest level possible. DECT pulses are far more aggressive than mobiles.&lt;br /&gt;Mobile phone concernsA team led by Swedish biophysicist Professor Kjell Mild, author of a number of papers on mobile-phone health effects, has published an update on his brain-tumour work in the summer of 2001. Professor Mild discussed his results to date at an international conference chaired by Alasdair Philips of Powerwatch.&lt;br /&gt;Another study by Dr Lennart Hardell, published in the International Journal of Oncology, based on the analysis of 1,600 tumour victims who had been using mobile phones for up to 10 years. Prof. Mild now states: ‘The evidence for a connection between phone use and cancer is clear and convincing. The more you use phones and the greater the number of years you have them, the greater the risk of brain tumours. ... Mobile phones are here to stay so my advice is never to use one without a hands-free headset.’&lt;br /&gt;An earlier study by Mild linked brain tumours to the use of analogue mobile phones. The new research repeated this and also looked at digital mobiles and DECT cordless phones. demonstrating that all three types were linked with increased tumour rates. Tumours only seem to appear after about 5 years use, but there is increasing dose-related-response with minutes of use per month and number of years of use.&lt;br /&gt;Since 1980, the number of acoustic neuromas (a rare tumour) diagnosed in Britain has risen from one in every 100,000 of the population to one in 80,000 a year. Some (but not all) other types of tumour also show an increase.&lt;br /&gt;Dr Richard Sullivan, head of clinical programmes at Cancer Research UK and quoted in the Sunday Times on 16th March 2003, said the study was worrying. ‘It suggests a strong link between mobile phones and brain tumours. ’&lt;br /&gt;A study by the Karolinska Institute in Sweden found a pronounced risk of acoustic neuroma from use of mobile phones over a ten year period.&lt;br /&gt;DECT pulse frequency concernDECT phones could be up to 100 times worse than an ordinary mobile, particularly if used in built up areas, due to the pulse frequency. DECT pulses at 100Hz whilst a GSM mobile pulses at 217Hz. The lower the pulsing frequency, the stronger the biological effect. Pulsing in the extremely low frequency (ELF) is of great concernt. This is why TETRA is so dangerous. TETRA pulses at 17.6Hz, in the same range as human beta brainwave rhythm. The research of Dr von Klitzing, one of the Medical Physicists signing the Freiburger Appeal, on blood samples taken from children in the vicinity of DECT phones showed that the red blood corpuscles did not ‘ripen out properly’ . The physical signs were: listlessness and/or aggression, pallor, sleeplessness etc. This was often reversed when the phone was removed.&lt;br /&gt;ChoiceIf you are worried, as a result of reading up on DECT, then put up with the wires! However, the neighbours’ phones are another matter. If you know where their DECT phone base is, you can try a patch of foil on the wall, to screen the DECT out. Microwaves tend to run around such barriers like water around a stone in a stream, so a small phone-sized patch will not work. If your foil disrupts the neighbouring phone, to avoid arguments, try to explain the problem, using the research listed here.&lt;br /&gt;DECT in the office? All your employer will do is refer to the Health and Safety Executive, who refer to the NRPB, who cite the ICNIRP (if it doesn’t heat you it can’t harm you) guidelines. These are wholly inappropriate, so employees have (a) no guidance and (b) no way to assess exposure in the office. The manufacturers give no advice on density of DECT per square metre. If you are sensitive to DECT, try to explain what you experience and ask for a wired phone.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/1010569638007681966-6895867963606049316?l=priyameena.blogspot.com'/&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://priyameena.blogspot.com/feeds/6895867963606049316/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='https://www.blogger.com/comment.g?blogID=1010569638007681966&amp;postID=6895867963606049316' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/1010569638007681966/posts/default/6895867963606049316'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/1010569638007681966/posts/default/6895867963606049316'/><link rel='alternate' type='text/html' href='http://priyameena.blogspot.com/2008/02/mobile-phones-hazard.html' title='MOBILE PHONES HAZARD.'/><author><name>priyanka gupta</name><uri>http://www.blogger.com/profile/03282159976818127425</uri><email>noreply@blogger.com</email><gd:extendedProperty xmlns:gd='http://schemas.google.com/g/2005' name='OpenSocialUserId' value='11703516926278611720'/></author><thr:total xmlns:thr='http://purl.org/syndication/thread/1.0'>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-1010569638007681966.post-6224616999941159158</id><published>2008-02-08T21:44:00.000-08:00</published><updated>2008-02-08T21:52:32.201-08:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='barriers'/><category scheme='http://www.blogger.com/atom/ns#' term='communication barriers'/><category scheme='http://www.blogger.com/atom/ns#' term='obstacles'/><title type='text'>OBSTACLES AND BARRIERS BEHAVIORS IN GROUP DYNAMICS</title><content type='html'>OBSTACLES AND BARRIERS BEHAVIORS IN GROUP DYNAMICS&lt;br /&gt;&lt;br /&gt;The following questions can used to self-debrief your behavior in settings where personal communications are used to build relationships -- at work, at home, in a church, with a spouse and about any place where two or more gather. These are the common barriers and you may think of others or variations. It is often helpful to do this evaluation in a group and exchange your views to enhance learning about yourself. The value of this is to discover what you may be doing to shut off communications and find ways to improve your behavior.A second way to use these barriers is to just copy the heading and discuss each within a group. The number one barrier to communications is not listening. Different forms of this are at the end of the list.&lt;br /&gt; &lt;a href="http://www.community4me.com/barriers.html#Anchor-PROJECTS-59379"&gt;(jump to listening barriers)&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;EXPECTATIONS:&lt;br /&gt; Are your expectations of others or organizations a barrier? Do others know your expectations or do you just think they know them? Can you change your expectations or let go of them to be part of a group or a relationship? How would that feel? Did this in any way feel like giving up your "self" to be what the group wants you to be? This is probably the number one barrier to communications. Expectations are often not expressed to others and it is as if the other is expected to have a crystal ball and know what you expect.RISKING: What is a risk for you? How much do you risk in a communications setting? What keeps you from risking? Is it fear? If so, fear of what? Is it control? Control of what? Yourself or others or the group? Do you wish to risk more? What will it take to risk more?This is probably the top barriers in communicating authentically. Risk in communication often has this silent question: " If I risk myself and this is all I've got, what will happen if I am rejected?" Building communications with others authentically takes a degree of risk.AVOIDANCE: What did you do to avoid looking at yourself? Think about this. What was behind the avoidance? Fear of rejection? Fear of loss of control? Were you part of an avoidance "project"? What did the group do to avoid doing what it needed to do? Did group norms facilitate avoidance?Avoidance frequently is present when a person feels unsafe or is unsure if its safe. Many business meetings start with considerable avoidance and only in the last minutes does the group get to the real subject, and then often try a quick fix. Avoidance can become a habit.FIXING: Did anyone try to fix you? The group? How did that feel? Did you try to fix, heal or convert anyone or the group? Can you fix anyone other than yourself? How aware are you that this is often done, with good intentions and well-meaning but usually not wanted and unaccepted 90+% of the time? What is your level of acceptance of people just as they are?&lt;br /&gt;Fixing is often trying to get the other to believe as you do or to do as you have done in a similar situation or to be more like you so you will feel more comfortable.&lt;br /&gt;&lt;br /&gt;PROJECTS:&lt;br /&gt; Most groups are creative in making projects that have something to do with avoidance. Can you name a project in your group? What do pseudo-projects represent in a group?Sometimes projects are things, sometimes people and often it's something completely outside the group and the room. Projects can be a way of fooling ourselves and have many of the characteristics of "organizing a group" and represent avoidance. They can be barriers to communications. Projects are sometimes necessary to help build safety and trust in groups. They can take the form of challenging the norms of a group or the written rules.SCAPEGOATING: Did you feel scapegoated? What did it feel like? Were you part of a scapegoating effort on another person?Scapegoating is often another form of avoidance or blaming or excluding. It may be an attempt to keep focus off of the person doing the scapegoating! It is seen in most family situations and in the workplace and is usually destructive to the personality.PROBING: Did anyone probe you for information? How did that feel? Did it create a barrier for you? If you were probed and did not like it, what kept you from confronting the prober? If you were the prober, why did you probe? Did it have anything to do with keeping the focus off of you?Probing can be avoidance of task or scapegoating if carried too far.SPEAKING IN CODE: If you were part of a subgroup of two or more people, did/do you speak with language that only those in the subgroup can understand? Can you understand how this is a form of exclusivity?This is often done without realizing it in all kinds of groups. It is not polite and keeps understanding low.CONTROL: Did anyone try to control you or what you said? How did it feel? Were you aware at any time that you were trying to control an outcome? If you tried to control, what was the reason? Was it to control what might happen to you? Did you notice others trying control?Most of us believe we have far more control than we actually do. Letting go of control and risking more may result in more love coming into your life.&lt;br /&gt;&lt;br /&gt;BLAMING:&lt;br /&gt; Did anyone blame you for what was or was not happening? How did that feel? Did you blame anyone? What was your motive for the blaming? Did it have to do with trying to make some other person responsible for your behavior? Did you experience blaming in your family of origin?Blaming can become an almost unconscious habit.&lt;br /&gt;&lt;br /&gt;PLACATING:&lt;br /&gt; Did you feel placated by anyone? Did you placate anyone? How does it feel to be placated?CHAOS AVOIDANCE: Do you run from conflict or avoid it in some way instead of trying to go through it? Do you leave a conversation when it gets too hot for you? (either actual or emotionally) How do you react to change?Another word for Chaos is change. People find many ways to avoid talking about change as it usually feels uncomfortable because of the unknown. Chaos can also mean conflict and many will do anything to avoid it. Chaos is one of the most certain things in life and it is well to learn how to embrace it.&lt;br /&gt;&lt;br /&gt;SILENCE:&lt;br /&gt; How comfortable are you with silence? Can you listen to yourself? To your source of spirit? Do you recognize respectful silence? Do you experience a silent time at home? What would it be like if you asked for some silence in your workplace during a meeting?Silence is an unused tool that is very effective in all kinds of ways. Scott Peck says in the Different Drum, "Silence is the primary key to emptiness." Also, "More than half of Beethoven's music is silence. Without the silence there is no music; there is only noise." Most people have little true silence in their lives, yet it provides considerable peacefulness.&lt;br /&gt;&lt;br /&gt;EXCLUSION:&lt;br /&gt; Did you feel excluded at any time? Did you exclude yourself? Did some person say anything that made you feel excluded? Was your feeling of exclusion accurate? Is this something that often happens to you? Did you exclude any person either by avoiding them, or emotionally tuning them out, or by making a judgmental statement? Did you later change the exclusion to inclusion?Think of how people are often excluded and why. It is often done as an unconscious act that may have been learned in the family or work place.&lt;br /&gt;&lt;br /&gt;BOUNDARY OR BARRIER:&lt;br /&gt; A boundary is often created for protection and should only be changed with considerable thought. A boundary "rule" is one you have originated that defines what is good or bad for you. A boundry may be a barrier to communication depending on what it is. Are you aware of any boundary you have that is a barrier to meaningful communications? Are you aware of any boundary that you want to change? How will you do that and how will you know if it is safe to change?Boundaries are accumulated during life for protection and become a learned method of existing. Boundaries need to be changed slowly and may be replaced with another boundary that offers more freedom until it becomes safe to "take the next step". Some people have few or almost no boundries and this often gets them into trouble. An example of this is a person that regulary offers far more information that is asked for by people they talk to. This becomes a turnoff to others and may result in other avoiding you.&lt;br /&gt;&lt;br /&gt; &lt;a name="Anchor-PROJECTS-59379"&gt;&lt;/a&gt;LISTENING:&lt;br /&gt; How well do you listen to what people say? Do you hear what is not said with words, but with emotions or body language? How about listening to what is not said? How can you listen with your whole being, body, mind, spirit and heart? There are many sub-barriers that come under Listening. Below are some.&lt;br /&gt;Automatic Talking: Listening just long enough to find a word that you know something about. Then shut off the rest of what is being said, particularly the emotional content. Then start talking about the word you know something about. This blocks real communications by not hearing the total content. This is the most used form of blocking true communication. For more on this, see &lt;a href="http://www.community4me.com/autotalking.html"&gt;Automatic Talking Exercise.&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;SELECTIVE LISTENING:&lt;br /&gt;This is when a person hears another but selects to not hear what is being said by choice or desire to hear some other message. This can take several forms and result in acting out in destructive ways. An example is to become passive agressive by prentending to hear and agree to what was said when actually your intent is to NOT act on the message, but make the other person think you will. Another form is to act on what you wanted to hear instead of what was said. Continued selective listening is one of the best ways to destroy a relationship.&lt;br /&gt;&lt;br /&gt;BEING A "FIXER":&lt;br /&gt; A fixer is a person that tries to fix another person's faults, problems or personality by offering what worked for them or a friend in a similar situatuon. Fixers often cut off others in the middle of a conversation without hearing the whole story to offer their fix. People overall do not like to be fixed and most suggestions for a fix will be disregarded and may result in anger toward the fixer.Using "You" or "We" statements instead of "I" statements. "I statements show ownership of what is being said. "You" statements are often a form of criticism. "We" statements often implies everyone within listening distance agrees with the statement which is not true. Its like you speaking for another person without their permission.Absolute Statements. These use such words as Never, always, forever, etc. and are often make a statement untrue. Use a less absolute word.Daydreaming. Letting your attention drift away. There are many causes of this and you can stop it by getting into the conversation and saying you are having a hard time staying with what is being said, without blaming. You may find out others are having the same difficulty and will do the same.Being right. This can take several forms. The most common is polite criticism of how a person speak or what they say or to insinuate that the person said it wrong. This can stop communication particularly with sensitive people. Many people have to learn how to communicate and can only do it by trying the way they know how.Derailing. (a form of avoidance) Changing the subject, or tell a joke, or point a finger at another person or try and turn a question around and back to the speaker.Name calling or belittling. This is hurtful and may make another feel foolish or stupid and they may exclude themselves from further conversation.Being the Reactor. On occasion, a person will attempt to get you to speak by trying to "hook" you to react. Swearing is a way of hooking some people. A good listener will continue to just listen and not react. This will often cause the person to stop trying to hook you if you keep it up long enough.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/1010569638007681966-6224616999941159158?l=priyameena.blogspot.com'/&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://priyameena.blogspot.com/feeds/6224616999941159158/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='https://www.blogger.com/comment.g?blogID=1010569638007681966&amp;postID=6224616999941159158' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/1010569638007681966/posts/default/6224616999941159158'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/1010569638007681966/posts/default/6224616999941159158'/><link rel='alternate' type='text/html' href='http://priyameena.blogspot.com/2008/02/obstacles-and-barriers-behaviors-in.html' title='OBSTACLES AND BARRIERS BEHAVIORS IN GROUP DYNAMICS'/><author><name>priyanka gupta</name><uri>http://www.blogger.com/profile/03282159976818127425</uri><email>noreply@blogger.com</email><gd:extendedProperty xmlns:gd='http://schemas.google.com/g/2005' name='OpenSocialUserId' value='11703516926278611720'/></author><thr:total xmlns:thr='http://purl.org/syndication/thread/1.0'>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-1010569638007681966.post-4110513531245512008</id><published>2008-02-08T21:31:00.000-08:00</published><updated>2008-02-08T21:43:39.378-08:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='barriers'/><category scheme='http://www.blogger.com/atom/ns#' term='communication barriers'/><category scheme='http://www.blogger.com/atom/ns#' term='communication'/><title type='text'>BARRIERS TO  COMMUNICATION (community)  EXERCISE</title><content type='html'>BARRIERS TO  COMMUNICATION (community)  EXERCISE&lt;br /&gt;&lt;br /&gt;&lt;a href="http://www.community4me.com/barriers.html#Anchor-HANDOUT-50558"&gt;(jump to barriers and skip exercise)&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;INTRODUCTION:This group dynamics exercise allows people to find their communications barriers. It can be used in any kind of group an can be adapted for use in a number of ways. You may just want to use the handout of barriers and discuss them or just part of them. The main barriers people have are listed first in the handout except for the barriers on listening which are listed last. The exercise below is how this is done in conjunction with a Community Building Workshop. I've used this exercise more than 100 times and always with great success.&lt;br /&gt;&lt;br /&gt;HOW TO DO THE EXERCISE:&lt;br /&gt;&lt;br /&gt;This exercise is done toward the end of the second day of a community building event. The introduction is usually done at about 4 -4:30 p.m. and the small groups work is in the evening with presentations given the following day.&lt;br /&gt;PURPOSE: The facilitator introduces the exercise by telling that barriers to communication most often keep people from experiencing community in a workshop and in relationships they have in life. The purpose of the exercise is for each individual to find one primary personal barrier they would like to change. Discuss various barriers and how you see them in your communications with others. Then talk about what you would like to do to minimize one barrier in your life.&lt;br /&gt;FACILITATIVE NOTES:&lt;br /&gt;Tell the group that you know they are probably tired and that this is a time they may go into chaos, but you are asking them to be patient for the next 10 minutes. Listen to the instructions and be prepared to ask some questions. Tell them they will work in small groups and you will start by dividing them into the groups.&lt;br /&gt;You can do this in two ways:&lt;br /&gt; (1) Put people in the groups you want them in. Use this only when you have a number of subgroups and what a person from each subgroup in a small group.&lt;br /&gt; (2) Count off by the number of people you want in each small group. This can be 3, 4, 5, 6, or 7. Any larger groups may not provide enough individual time. I prefer an odd number of 3 or 5 people per group.Each group will need a private place (room) to meet. Some may decide to have dinner together and work after in a persons room. You need to limit where they meet to the facility where the workshop is being held.&lt;br /&gt;&lt;br /&gt;PROCEDURE:&lt;br /&gt;Read the following to the group and give each person a copy with the handout.The object of this project is to have you discuss barriers and obstacles to community, both individual and group, and then determine how to transcend these in your everyday life. Be sure to look at how "coming from emptiness" plays a part in overcoming obstacles. Also, try to use actual examples in your life or from the workshop to learn how the barrier works in your life.&lt;br /&gt;&lt;br /&gt;Priorities in this exercise:&lt;br /&gt;&lt;br /&gt;1. Have fun!&lt;br /&gt;2. Build Community in your group3. Do the assigned task.&lt;br /&gt;&lt;br /&gt;Instructions:&lt;br /&gt;1. In your small group, take some silence and start to build community in this group. (have fun)&lt;br /&gt;&lt;br /&gt;2. Examine the Barriers Handout. Discuss your barriers in your group in an attempt to find the barrier you would like to transform (let go of or improve) in your life. (have fun)&lt;br /&gt;&lt;br /&gt;3. Share your personal insights with each other. (have fun)&lt;br /&gt;&lt;br /&gt;4. Select a barrier (or barriers) to present to the large group. This can be a common barrier or each person may feel a need to present their individual barrier. (have fun)&lt;br /&gt;&lt;br /&gt;5. Together as a group, decide how you wish to present the barrier(s) and their transformation to the large group. This can be done in about any way you desire. Be creative. Make it fun. It can be just a report, a song or group of songs, or a poster, but a skit is preferred. Try to keep the your presentation to 10 minutes. You can use props. The transformation should embody emptiness in some way. (have fun)&lt;br /&gt;&lt;br /&gt;6. There are a few rules about the presentation:&lt;br /&gt;· Do not use any presentation that uses fire or smoke (fire detectors may go off and stop the workshop.)· Do not require participation by individuals in the large group.· Be mindful of our differences and respect all differences .&lt;br /&gt;Ask if there are any question and for only one person at a time to speak.&lt;br /&gt;Have some materials available that they can make props from, like cardboard boxes, marking pens, colors, poster board, old "dress up" clothes, hats and anything else you can think of.&lt;br /&gt;Have each group write on a paper where they will be doing their project and the times they will be there. Your task in the evening is to move between the groups and help if they truly get stuck. Some groups will get stuck but can usually get themselves out of it. So don't do a rescue until you know they are truly stuck. On very rare occasion, some group may find it very difficult to work together. In this case you will have to work with them and perhaps tell them what to do. This is very rare. Many groups will struggle and that is good. Some will be working out chaos that happened in the workshop or even work out differences between people. Usually three hours is enough for most groups. Some have gone six hours because they were having such fun. You may need to limit them to a certain time to quit. I usually say 9:30 pm. Some will labor to have a skit. You can encourage them to just have a theme and let it happen. I've seen groups put their skits together as they did them and it looked like they had practiced it for hours. Tell them to let the spirit guide them.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/1010569638007681966-4110513531245512008?l=priyameena.blogspot.com'/&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://priyameena.blogspot.com/feeds/4110513531245512008/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='https://www.blogger.com/comment.g?blogID=1010569638007681966&amp;postID=4110513531245512008' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/1010569638007681966/posts/default/4110513531245512008'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/1010569638007681966/posts/default/4110513531245512008'/><link rel='alternate' type='text/html' href='http://priyameena.blogspot.com/2008/02/barriers-to-communication-community.html' title='BARRIERS TO  COMMUNICATION (community)  EXERCISE'/><author><name>priyanka gupta</name><uri>http://www.blogger.com/profile/03282159976818127425</uri><email>noreply@blogger.com</email><gd:extendedProperty xmlns:gd='http://schemas.google.com/g/2005' name='OpenSocialUserId' value='11703516926278611720'/></author><thr:total xmlns:thr='http://purl.org/syndication/thread/1.0'>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-1010569638007681966.post-7504032795186549658</id><published>2008-02-07T02:08:00.000-08:00</published><updated>2008-02-07T02:09:45.257-08:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='technology'/><category scheme='http://www.blogger.com/atom/ns#' term='crashing'/><category scheme='http://www.blogger.com/atom/ns#' term='computer'/><category scheme='http://www.blogger.com/atom/ns#' term='computer crashing'/><title type='text'>Computer Crashings</title><content type='html'>&lt;a title="Permanent Link to Computer Crashings" href="http://generallordisimo.wordpress.com/2008/02/05/computer-crashings/" rel="bookmark"&gt;Computer Crashings&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;br /&gt;People are impatient, which doesn’t come as a surprise to me seeing as I am listed in that category (especially when I am driving).  For the last four/five days the library has been having some significant computer problems with our Pharos system, which is the system that allows patrons to log on to the public computers.  The effect of these problems has been that for long periods of time over the last couple of days nobody has been able to get on any of the computers.  Now I can understand how this could make somebody pretty impatient, especially if they have some piece of important business they need to get done.  Still there were are a few people who just don’t seem to get, “We are really sorry that the system is down, IT is working on it, and hopefully they will be back up as soon as possible.”  There was this one dude this morning who just didn’t get it, and he was getting all pissed off and trying to use the 15 minute express computers even though I had told him they were down too.  Again I can understand the frustration but I have to say that when somebody has politely explained to you that the problem is being worked on and will hopefully be resolved soon, I’d think that you’d probably just try and accept it.  Not this dude though, he was going to keep trying to log on until it worked even if he sat here all day long.  I actually finally had to ask him to leave because he started playing around with the power buttons, turning a couple of the computers on and off (which is a big no-no in the library — only myself or other library employees are allowed to turn the machines off or on).  He wasn’t too happy to be asked to leave either but I just gave him a slight smile and said, “I’m really sorry for the inconvenience this is causing you sir but there is very little that can be done about it right now.  I cannot have you turning computers on and off in here.  Doing so isn’t going to fix anything anyway.  There are six gentlemen downstairs who are working as fast as they can to get the system back up.  I recommend that if you have any other business in the library or downtown you might want to go ahead in do that and check back a little later to see if the computers are back up.  I don’t know how long it will be before they are working again but I think it is safe to assume that it will be a little while.”  That probably wasn’t verbatim what I said, but it was probably pretty close seeing as I’ve had to say very similar things to about a hundred plus people in the last two days.  My angry dude did take his leave, albeit with a lot of grumbling and cursing under his breath (he also showed up almost immediately as soon as the computer started working again about an hour later which leads me to believe he was just sulking around the library for some time.  Further, his very important need to get on a computer was just to play computer games, which he has been doing non-stop since the system started working again).  So far the computers have not crashed again today which is a good thing because the computers malfunctioning cause inconvenience for patrons.  It also gets annoying to me to have to repeat again and again that the computers are down especially considering that when they crash I always promptly put up signage explaining that there are system problems in the library (this has led me to believe very firmly that people really just don’t pay attention to signs.  The same goes for all the “No Cellular Phone Use in the Library” signs that are literally unavoidable in this place, yet every day people have to be asked to please silence there phones or go outside to have conversations).  Well the computers have been back up and running okay for several hour now and hopefully they won’t crash again (knock on wood here).  I’d just say to all the people who use library public computers everywhere, remember that they are computers and computers have problems sometimes, so try to be patient when things don’t work, because being impatient or rude isn’t going to do anything to make things work any better, it is just going to piss other people off.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/1010569638007681966-7504032795186549658?l=priyameena.blogspot.com'/&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://priyameena.blogspot.com/feeds/7504032795186549658/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='https://www.blogger.com/comment.g?blogID=1010569638007681966&amp;postID=7504032795186549658' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/1010569638007681966/posts/default/7504032795186549658'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/1010569638007681966/posts/default/7504032795186549658'/><link rel='alternate' type='text/html' href='http://priyameena.blogspot.com/2008/02/computer-crashings.html' title='Computer Crashings'/><author><name>priyanka gupta</name><uri>http://www.blogger.com/profile/03282159976818127425</uri><email>noreply@blogger.com</email><gd:extendedProperty xmlns:gd='http://schemas.google.com/g/2005' name='OpenSocialUserId' value='11703516926278611720'/></author><thr:total xmlns:thr='http://purl.org/syndication/thread/1.0'>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-1010569638007681966.post-6586958076846730887</id><published>2008-02-07T02:00:00.000-08:00</published><updated>2008-02-07T02:05:36.011-08:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='blocks'/><category scheme='http://www.blogger.com/atom/ns#' term='swarm algorithm'/><category scheme='http://www.blogger.com/atom/ns#' term='pictures'/><category scheme='http://www.blogger.com/atom/ns#' term='multicorecomputers'/><category scheme='http://www.blogger.com/atom/ns#' term='computer'/><title type='text'>Swarm Algorithms, Better Pictures, and Multicore Computers</title><content type='html'>&lt;a title="Permanent Link: Swarm Algorithms, Better Pictures, and Multicore Computers" href="http://softwareblogs.intel.com/2008/02/04/swarm-algorithms-better-pictures-and-multicore-computers/" rel="bookmark"&gt;Swarm Algorithms, Better Pictures, and Multicore Computers&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;br /&gt;I received an interesting email this morning, the Dr. Dobb's Report, a newsletter I subscribe to. The lead article is titled "Swarm Algorithms and (Better) Digital Photos." Whenever I see something like this, I am immediately reminded of the potential benefits of multicore processors on home computers. Surely, if there's a way to improve the quality of digital pictures, that's something everyone's going to want to be able to do.&lt;br /&gt;But if improving the pictures involves complex algorithms, then those algorithms will have to be multithreaded, using &lt;a href="http://www.threadingbuildingblocks.org/"&gt;Threading Building Blocks&lt;/a&gt; or some other technique, and the enhancement program will have to run on a multicore system; otherwise, users will be idly watching their screens, getting ever more impatient as they wait forever for the enhancement analysis to complete.&lt;br /&gt;The Method: Particle Swarm Optimization Enhancement&lt;br /&gt;Here's a snippet from the Dr. Dobb's Report message:&lt;br /&gt;... researchers are turning to "swarm intelligence" as a means of enhancing digital photos. Swarm intelligence is an AI technique that's based on the collective behavior of decentralized, self-organized systems.&lt;br /&gt;The technique ... uses a &lt;a href="http://www.swarmintelligence.org/"&gt;Particle Swarm Optimization&lt;/a&gt; (PSO) algorithm to enhance contrast and details without distortion.&lt;br /&gt;Somewhat like Genetic Algorithms, PSO treats each version of an image as an individual member of a swarm and makes a single, small adjustment to contrast levels, edge sharpness, and other image parameters. The algorithm then determines whether the new members of the swarm are better or worse than the original, according to an objective fitness criterion.&lt;br /&gt;The authors' paper, &lt;a href="http://www.inderscience.com/search/index.php?mainAction=search&amp;amp;action=record&amp;amp;rec_id=16795"&gt;"Particle swarm optimization enhancement approach for improving image quality"&lt;/a&gt;, was published in the &lt;a href="http://www.inderscience.com/browse/index.php?journalID=215&amp;amp;year=2007&amp;amp;vol=1&amp;amp;issue=2"&gt;International Journal of Innovative Computing and Applications&lt;/a&gt; in 2007, and is available for purchase.&lt;br /&gt;Conclusion&lt;br /&gt;Algorithmic techniques that are applicable to everyday activities are being actively researched. The advent of multicore computers and multithreading techniques like TBB present opportunities to bring these innovations to home and office desktop computers. I expect that, once people realize such software is possible, they'll want to have it. The beneficiaries will be the developers and software vendors who recognize the full potential of multicore processors, and bring these new products to market early on.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/1010569638007681966-6586958076846730887?l=priyameena.blogspot.com'/&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://priyameena.blogspot.com/feeds/6586958076846730887/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='https://www.blogger.com/comment.g?blogID=1010569638007681966&amp;postID=6586958076846730887' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/1010569638007681966/posts/default/6586958076846730887'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/1010569638007681966/posts/default/6586958076846730887'/><link rel='alternate' type='text/html' href='http://priyameena.blogspot.com/2008/02/swarm-algorithms-better-pictures-and.html' title='Swarm Algorithms, Better Pictures, and Multicore Computers'/><author><name>priyanka gupta</name><uri>http://www.blogger.com/profile/03282159976818127425</uri><email>noreply@blogger.com</email><gd:extendedProperty xmlns:gd='http://schemas.google.com/g/2005' name='OpenSocialUserId' value='11703516926278611720'/></author><thr:total xmlns:thr='http://purl.org/syndication/thread/1.0'>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-1010569638007681966.post-1942410237725270054</id><published>2008-02-07T01:56:00.000-08:00</published><updated>2008-02-07T02:00:28.753-08:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='technology'/><category scheme='http://www.blogger.com/atom/ns#' term='liquid interface'/><category scheme='http://www.blogger.com/atom/ns#' term='semantic'/><category scheme='http://www.blogger.com/atom/ns#' term='interface'/><category scheme='http://www.blogger.com/atom/ns#' term='web'/><category scheme='http://www.blogger.com/atom/ns#' term='computer'/><title type='text'>Can Computers Create Usable Interfaces by themselves?</title><content type='html'>&lt;a title="'Permanent" href="http://useroriented.wordpress.com/2008/02/04/can-computers-create-usable-interfaces-by-themselves/" rel="bookmark"&gt;Can Computers Create Usable Interfaces by themselves?&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;br /&gt;Composing &lt;a href="http://useroriented.wordpress.com/2007/07/29/semantic-web-services-a-short-introduction/"&gt;semantic Web services&lt;/a&gt; is a fascinating technology: creating new applications on-the-fly from existing services. However, it raises a new problem for user interfaces. Usability cannot be evaluated or optimized in traditional ways when the application is constructed dynamically, and can change during runtime.&lt;br /&gt;In order to answer this problem, we tried to construct an automatic method for evaluating and optimizing the usability of simple composition of Web services. The method is encapsulated in the &lt;a href="http://useroriented.wordpress.com/2006/11/11/liquid-interfaces/"&gt;LiquidInterface &lt;/a&gt;system, which automatically creates Web-based mockup application for semantic Web services.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/1010569638007681966-1942410237725270054?l=priyameena.blogspot.com'/&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://priyameena.blogspot.com/feeds/1942410237725270054/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='https://www.blogger.com/comment.g?blogID=1010569638007681966&amp;postID=1942410237725270054' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/1010569638007681966/posts/default/1942410237725270054'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/1010569638007681966/posts/default/1942410237725270054'/><link rel='alternate' type='text/html' href='http://priyameena.blogspot.com/2008/02/can-computers-create-usable-interfaces.html' title='Can Computers Create Usable Interfaces by themselves?'/><author><name>priyanka gupta</name><uri>http://www.blogger.com/profile/03282159976818127425</uri><email>noreply@blogger.com</email><gd:extendedProperty xmlns:gd='http://schemas.google.com/g/2005' name='OpenSocialUserId' value='11703516926278611720'/></author><thr:total xmlns:thr='http://purl.org/syndication/thread/1.0'>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-1010569638007681966.post-6370038168678684049</id><published>2008-02-07T01:55:00.000-08:00</published><updated>2008-02-07T01:56:42.399-08:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='birdflu'/><category scheme='http://www.blogger.com/atom/ns#' term='disease'/><category scheme='http://www.blogger.com/atom/ns#' term='flu'/><category scheme='http://www.blogger.com/atom/ns#' term='bird'/><title type='text'>Bird Flu</title><content type='html'>Bird Flu&lt;br /&gt;&lt;br /&gt;&lt;br /&gt;It’s not like this has taken off. Just note that everytime you read about human contact with this disease the fatality rate is around 85-percent. That’s why they get so freaked.&lt;br /&gt;HANOI, Jan. 26 (Xinhuanet) — Bird flu has, since January, spread to 26 cities and provinces across Vietnam, killing and leading to the forced culling of over 613,000 fowls, local newspaper Youth reported Wednesday.&lt;br /&gt;A total of 454 areas in 263 communes of 26 out of 64 localities nationwide have been hit by bird flu. The latest locality being hit by the disease is northern Thai Nguyen province.&lt;br /&gt;Since Dec. 28, 2004, a total of 11 human cases of bird flu infection have been reported in Vietnam, eight in the south and three in the north. Among the 11 victims, nine have died.&lt;br /&gt;Among the two alive patients, one has already recovered fully, and the other will be discharged from the Tropical Disease Institute in Hanoi capital city in a couple of days, local doctorssaid, noting that early hospitalization is largely attributed to their recovery.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/1010569638007681966-6370038168678684049?l=priyameena.blogspot.com'/&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://priyameena.blogspot.com/feeds/6370038168678684049/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='https://www.blogger.com/comment.g?blogID=1010569638007681966&amp;postID=6370038168678684049' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/1010569638007681966/posts/default/6370038168678684049'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/1010569638007681966/posts/default/6370038168678684049'/><link rel='alternate' type='text/html' href='http://priyameena.blogspot.com/2008/02/bird-flu.html' title='Bird Flu'/><author><name>priyanka gupta</name><uri>http://www.blogger.com/profile/03282159976818127425</uri><email>noreply@blogger.com</email><gd:extendedProperty xmlns:gd='http://schemas.google.com/g/2005' name='OpenSocialUserId' value='11703516926278611720'/></author><thr:total xmlns:thr='http://purl.org/syndication/thread/1.0'>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-1010569638007681966.post-162651700059708992</id><published>2008-02-07T01:48:00.000-08:00</published><updated>2008-02-07T01:52:37.753-08:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='technology'/><category scheme='http://www.blogger.com/atom/ns#' term='theives'/><category scheme='http://www.blogger.com/atom/ns#' term='computer'/><category scheme='http://www.blogger.com/atom/ns#' term='Diocese'/><category scheme='http://www.blogger.com/atom/ns#' term='steal'/><title type='text'>Thieves steal four Diocese of Providence computers</title><content type='html'>Thieves steal four Diocese of Providence computers&lt;br /&gt;&lt;br /&gt;Victims:Current and former Catholic school employeesNumber Affected:about 5,000Types of Data:Names, addresses and Social Security numbersBreach Description:Sometime during the weekend of January 27th, 2008 thieves broke into the Chancery of the Roman Catholic Diocese of Providence and stolen four desktop computers, one of which contained sensitive personal information belonging to current and former Catholic school employees.Reference URL:&lt;a href="http://www.dioceseofprovidence.org/?id=212" target="_blank"&gt;The Diocese of Providence online announcement&lt;/a&gt; &lt;a href="http://www.projo.com/news/content/catholic_identity_theft_02-02-08_BK8S2PA_v13.363690c.html" target="_blank"&gt;The Providence Journal online story&lt;/a&gt;Report Credit:The Diocese of ProvidenceResponse:From the online sources cited above:An individual or individuals broke into the Diocesan Office Building (also known as the Chancery) located at One Cathedral Square in Providence.  The perpetrator(s) gained access by breaking through an office window in the Catholic School Office suite.Once in the building, the perpetrators forcibly entered through two locked office doors where they stole desktop computers and other equipment.The office suite that was burglarized did not have an alarm system[Evan] It was reported that the Diocese does employ a security guard, but it is not known where he/she was at the time of the break-in.  The fact that the timeframe in question is 8 hours (10 PM Friday - 6 AM Saturday) is interesting.  Typically security guards are expected to make regular rounds (~ once every hour or two) throughout the area being guarded.  Eight hours is a long time for a break-in to go undetected, so an alarm system would have been very beneficial as an alert if not a deterrent.One of the stolen computers (a desktop computer, not a laptop) contained a substantial amount of data that included personnel information on present and former Catholic school employees throughout the Diocese of Providence. The Rhode Island State Police have been notified of this incident.  Additionally, the Providence Police Department has assumed responsibility for the investigation.Thus far, the stolen equipment has not been recovered however, the Catholic Schools Office is fully cooperating with law enforcement who are investigating the situation.Present and former employees of Rhode Island Catholic schools may be affected.A number of safeguards are in place such as: locked offices, password protected computers, local administrator account password protected, guest accounts disabled.[Evan] These are all good security practices.Employees have unique passwords that they are required to change every few weeks[Evan] Another good security practice, but every few weeks might be a little too often.  If we make people change their passwords too often we increase the chances that they will write them down.Additionally, personal information of students, teachers, parents and others associated with the Catholic Schools Office are prohibited from storage on lap top computers.[Evan] Yet another good security practice.Personal information of students and their parents and or guardians was not stored on the stolen equipment.In addition to notifying current and former employees by letters sent to last known addresses, the Catholic Schools Office has created this page on  the web site and established a special phone number, 401/278-4678 to answer inquiries from those who feel they may have been affectedAnother diocese office was broken into about a year ago and a computer stolen“The Catholic schools office sincerely apologizes for any inconvenience this incident may cause its current and former employees,”Commentary:Judging from what the Diocese has told us about their security practices it is easy to see that they have made a conscious effort to secure confidential information.  They put some sound information security practices to use, but now we understand that it wasn't enough.  At least two vital information security controls were missed; data at rest encryption and adequate physical security (alarm system missing).  There is no mention as to whether or not the Diocese or Chancery are surveilled.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/1010569638007681966-162651700059708992?l=priyameena.blogspot.com'/&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://priyameena.blogspot.com/feeds/162651700059708992/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='https://www.blogger.com/comment.g?blogID=1010569638007681966&amp;postID=162651700059708992' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/1010569638007681966/posts/default/162651700059708992'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/1010569638007681966/posts/default/162651700059708992'/><link rel='alternate' type='text/html' href='http://priyameena.blogspot.com/2008/02/thieves-steal-four-diocese-of.html' title='Thieves steal four Diocese of Providence computers'/><author><name>priyanka gupta</name><uri>http://www.blogger.com/profile/03282159976818127425</uri><email>noreply@blogger.com</email><gd:extendedProperty xmlns:gd='http://schemas.google.com/g/2005' name='OpenSocialUserId' value='11703516926278611720'/></author><thr:total xmlns:thr='http://purl.org/syndication/thread/1.0'>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-1010569638007681966.post-7125557945521440521</id><published>2008-02-07T01:46:00.000-08:00</published><updated>2008-02-07T01:48:18.338-08:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='IBM'/><category scheme='http://www.blogger.com/atom/ns#' term='online'/><category scheme='http://www.blogger.com/atom/ns#' term='XML'/><category scheme='http://www.blogger.com/atom/ns#' term='web'/><category scheme='http://www.blogger.com/atom/ns#' term='computer'/><title type='text'>HOWTO save daily WebSphere 6.1 configuration with an "online" way?</title><content type='html'>HOWTO save daily WebSphere 6.1 configuration with an "online" way?&lt;br /&gt;&lt;br /&gt;Hi all, in my previuos experience I'm used to export the whole configuration daily using XMLConfig tool. Guessed! In the previous experience I had a cluster of 6 WS4.0.7. Now I want to replicate this kind of managing, but talking with our IBM specialists I was warned about ws_ant ExportImport procedure. ws_ant stops all the applications but I have the goal of maintaining 24/7 usability SLA. Unfortunately I can't use only the wsadmin generation scripts to rebuild a disaster situation because of many performance tunning were performed all day long from many working units. So, I ask the community: what is your best suggestion on this issue?&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/1010569638007681966-7125557945521440521?l=priyameena.blogspot.com'/&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://priyameena.blogspot.com/feeds/7125557945521440521/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='https://www.blogger.com/comment.g?blogID=1010569638007681966&amp;postID=7125557945521440521' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/1010569638007681966/posts/default/7125557945521440521'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/1010569638007681966/posts/default/7125557945521440521'/><link rel='alternate' type='text/html' href='http://priyameena.blogspot.com/2008/02/howto-save-daily-websphere-61.html' title='HOWTO save daily WebSphere 6.1 configuration with an &quot;online&quot; way?'/><author><name>priyanka gupta</name><uri>http://www.blogger.com/profile/03282159976818127425</uri><email>noreply@blogger.com</email><gd:extendedProperty xmlns:gd='http://schemas.google.com/g/2005' name='OpenSocialUserId' value='11703516926278611720'/></author><thr:total xmlns:thr='http://purl.org/syndication/thread/1.0'>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-1010569638007681966.post-9177108463812179764</id><published>2008-02-01T22:53:00.000-08:00</published><updated>2008-02-01T23:02:31.166-08:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='pharmaceutical'/><category scheme='http://www.blogger.com/atom/ns#' term='nano'/><category scheme='http://www.blogger.com/atom/ns#' term='nanotechnology'/><title type='text'>Pharmaceutical Nanotechnology Formulation</title><content type='html'>Pharmaceutical Nanotechnology Formulation&lt;br /&gt;&lt;br /&gt;.&lt;br /&gt;Scientists at Cirrus Pharmaceuticals, Inc. use nanotechnology to approach classical and novel drug delivery applications. They provide services for producing, formulating, and characterizing nanoparticles for a wide array of applications including, but not limited to, oral, pulmonary, and parenteral delivery.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/1010569638007681966-9177108463812179764?l=priyameena.blogspot.com'/&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://priyameena.blogspot.com/feeds/9177108463812179764/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='https://www.blogger.com/comment.g?blogID=1010569638007681966&amp;postID=9177108463812179764' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/1010569638007681966/posts/default/9177108463812179764'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/1010569638007681966/posts/default/9177108463812179764'/><link rel='alternate' type='text/html' href='http://priyameena.blogspot.com/2008/02/pharmaceutical-nanotechnology.html' title='Pharmaceutical Nanotechnology Formulation'/><author><name>priyanka gupta</name><uri>http://www.blogger.com/profile/03282159976818127425</uri><email>noreply@blogger.com</email><gd:extendedProperty xmlns:gd='http://schemas.google.com/g/2005' name='OpenSocialUserId' value='11703516926278611720'/></author><thr:total xmlns:thr='http://purl.org/syndication/thread/1.0'>0</thr:total></entry></feed>