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      <title>GEOGRAPHY tectonic activity case studies by Luke Dobbe</title>
      <link>https://padlet.com/ldobbe1/Tectonic_casestudies</link>
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      <language>en-us</language>
      <pubDate>2016-05-12 12:16:00 UTC</pubDate>
      <lastBuildDate>2016-05-24 11:47:48 UTC</lastBuildDate>
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         <title>Volcanoes - Montserrat 1997</title>
         <author>ldobbe1</author>
         <link>https://padlet.com/ldobbe1/Tectonic_casestudies/wish/110628593</link>
         <description><![CDATA[<div>Causes:<br>- Caribbean island that lies on destructive plate boundary.<br>The oceanic Atlantic plate moving towards the contental Caribbean plate. <br>- this area of the plate is known as the volcanic arc due to high number of valconaes present<br><br>Social: <br>- population decline from 12000 to 3000 due to the risk (long term)<br>- over 20 villages and 2/3 of building destroyed, leading to displacement of people (long term)<br>- 19 people died and 7 were injured (short term)<br>-aging population created as younger people left as they saw no economic future (long term)<br>- health suffers as volcanic ash leads to respiratory illness (long term)<br><br>Economic p:<br>- over 20 villages destroyed (short term)<br>- airport and pry destroyed (short term)<br>- tourist stayed away for following years as resorts were damaged - income lost and jobs affected (long term)<br>-tourism has now increased as people visiting the volcanoes and jobs created (long term)<br>- Plymouth the capital destroyed and covered with 12m of ash </div>]]></description>
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         <pubDate>2016-05-12 18:12:33 UTC</pubDate>
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         <title>Volcanoes - Montserrat continued </title>
         <author>ldobbe1</author>
         <link>https://padlet.com/ldobbe1/Tectonic_casestudies/wish/110630999</link>
         <description><![CDATA[<div>Environmental:<br>- vegetation damaged by ash and crops destroyed (short term)<br>-volcanic ash has now improved should fertility and yield increased (long term)<br><br>Short term responses:<br>- evacuee camps set up in north of island<br>-British government gave £200 million in emagancy aid<br>-small scale substance framing in south damaged so country relied on food aid<br>-aid,food and water sent to refuel gee camps by aid agave has such as the Red Cross<br>-charities set up temporary schools and sent emergency food for farm animals<br>-roads diverted to abide damage from pyroclastic flows.<br><br>Long term responses:<br>- little ray redeveloped as new capital<br>50%od population evacuated afterwaords<br>-British aid spent on developing new airport, docks and hiuses<br>- volcanoes observatory opened to monitor&nbsp; volcanoe<br>- exclusion zone set up in south of island till present, it evacuated of 5000 people.</div>]]></description>
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         <pubDate>2016-05-12 18:20:52 UTC</pubDate>
         <guid>https://padlet.com/ldobbe1/Tectonic_casestudies/wish/110630999</guid>
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         <title>Super volcanoes - Yellowstone</title>
         <author>ldobbe1</author>
         <link>https://padlet.com/ldobbe1/Tectonic_casestudies/wish/110633183</link>
         <description><![CDATA[<div>super volcanoes not near a plate boundary, they are caused by a hot spot under the contental crust.<br><br>-6.5km below Yellowstone is a 64km wide magma chamber.<br>-has hot springs and gyizers<br><br>-lot bigger than normally volcanoes and not on plate boundaries. Crater emits 11,000 times more emmjsons. They also don't have a leak as they are flat<br><br>-magma is blocked from reaching the Earths surface.<br>-the pressure builds and more rock melts creating a magma chamber.<br>-when pressure is too much the entire surface is blown away by a huge explosions forming a caldera.<br><br>-magma flung 50km into atmosphere.<br>- all life 1000km away will be killed by ash, lava flows and the force of the explosion&nbsp;<br>- 1000'km cubed of larva&nbsp; pour out.<br>- the USA would be covered with 12.5cm of ash<br>- ash would kill crops and block out the sun leading to a nuclear winter<br>-economy's would collapse&nbsp;<br>-it would destroy and flatten every single tree in blast zone which is 25km north.<br><br></div>]]></description>
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         <pubDate>2016-05-12 18:28:26 UTC</pubDate>
         <guid>https://padlet.com/ldobbe1/Tectonic_casestudies/wish/110633183</guid>
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         <title>Earthquake - chile 2010</title>
         <author>ldobbe1</author>
         <link>https://padlet.com/ldobbe1/Tectonic_casestudies/wish/110704513</link>
         <description><![CDATA[<div>-27 of February 2010<br>-8.8 on richter scale<br>-epicentre 115km from concepcion<br>-focus 34km be,ow ground<br>-destructive plate boundary (Nazca and South American plate)<br>-focus just if the coast caused a tsunami.<br>-building codes meant there was less destruction.<br><br>-500 people killed (primary)<br>-12,000 people injured (primary)<br>Buildings destroyed (primary)<br>-500000 homes damaged (primary)<br>-Bridges and roads destroyed (primary)<br>- talca hospital badly damaged(primary)<br><br>-wide loss of power and other services (secondary)<br>-other countries hit by tsunamis (secondary)<br>-fire at chemical plants meant that Santiago was evacuated&nbsp;<br>-little danage to copper mines<br><br>- rapid analysis of situation (immediate)<br>- needed aid was requested (immediate)<br>-Route 5 repaired to deliver aid<br>-10 days later 90%of homes had power and water (immediate)<br>- $60 million raised for emergency shelter<br><br>- housing reconstruction plan to help 196,000 households a month after earth quake (long term)<br>-stronger economy so recovered quickly with foreign aid to help reconstruction efforts and rebuilding (long term)</div>]]></description>
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         <pubDate>2016-05-13 06:53:57 UTC</pubDate>
         <guid>https://padlet.com/ldobbe1/Tectonic_casestudies/wish/110704513</guid>
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