<?xml version="1.0"?>
<rss version="2.0">
   <channel>
      <title>Earthquake History  by Jasmine Evans</title>
      <link>https://padlet.com/jasminese1009/zt0eafb5m5c8</link>
      <description>Earthquakes in many different countries , and how it still effects others today </description>
      <language>en-us</language>
      <pubDate>2015-03-19 15:21:39 UTC</pubDate>
      <lastBuildDate>2024-07-28 12:07:30 UTC</lastBuildDate>
      <webMaster>hello@padlet.com</webMaster>
      <image>
         <url></url>
      </image>
      <item>
         <title>On average, a magnitude 8 quake strikes somewhere every year and some 10,000 people die in earthquakes annually. Collapsing buildings claim by far the majority of lives, but the destruction is often compounded by mud slides, fires, floods, or tsunamis. Smaller temblors that usually occur in the days following a large earthquake can complicate rescue efforts and cause further death and destruction.</title>
         <author>jasminese1009</author>
         <link>https://padlet.com/jasminese1009/zt0eafb5m5c8/wish/54088274</link>
         <description><![CDATA[]]></description>
         <enclosure url="http://environment.nationalgeographic.com/environment/natural-disasters/earthquake-profile/" />
         <pubDate>2015-03-19 15:25:53 UTC</pubDate>
         <guid>https://padlet.com/jasminese1009/zt0eafb5m5c8/wish/54088274</guid>
      </item>
      <item>
         <title>Fault</title>
         <author>jasminese1009</author>
         <link>https://padlet.com/jasminese1009/zt0eafb5m5c8/wish/54638839</link>
         <description><![CDATA[<p>an unattractive or unsatisfactory feature, especially in a piece of work or in a person's character</p>]]></description>
         <enclosure url="https://padlet-uploads.storage.googleapis.com/59447713/a5155b5dda519dc7251fc637d7224c07d884826d/9bfff9cf089a971a2108a63a282b279b.png" />
         <pubDate>2015-03-24 15:14:27 UTC</pubDate>
         <guid>https://padlet.com/jasminese1009/zt0eafb5m5c8/wish/54638839</guid>
      </item>
      <item>
         <title>Epicenter</title>
         <author>jasminese1009</author>
         <link>https://padlet.com/jasminese1009/zt0eafb5m5c8/wish/54639336</link>
         <description><![CDATA[<p> point on the earth's surface vertically above the focus of an earthquake</p>]]></description>
         <enclosure url="https://padlet-uploads.storage.googleapis.com/59447713/70181933b352b7fd0d92d03f8ff5880db5d1be7a/124399e44fb58d038fb240388268cc27.png" />
         <pubDate>2015-03-24 15:16:11 UTC</pubDate>
         <guid>https://padlet.com/jasminese1009/zt0eafb5m5c8/wish/54639336</guid>
      </item>
      <item>
         <title>Focus </title>
         <author>jasminese1009</author>
         <link>https://padlet.com/jasminese1009/zt0eafb5m5c8/wish/54639941</link>
         <description><![CDATA[<p>the center of interest or activity.</p>]]></description>
         <enclosure url="https://padlet-uploads.storage.googleapis.com/59447713/6383acc23a5966607d6ac31a76d48f1c487d5c31/788753ba43cb21cdc3ace2d1c41d792c.png" />
         <pubDate>2015-03-24 15:18:05 UTC</pubDate>
         <guid>https://padlet.com/jasminese1009/zt0eafb5m5c8/wish/54639941</guid>
      </item>
      <item>
         <title>Transform Boundaries</title>
         <author>jasminese1009</author>
         <link>https://padlet.com/jasminese1009/zt0eafb5m5c8/wish/54640902</link>
         <description><![CDATA[<p>-&nbsp;A transform fault or transform boundary, also known as conservative plate boundary since these faults neither create nor destroy lithosphere, is a type of fault.</p>]]></description>
         <enclosure url="https://padlet-uploads.storage.googleapis.com/59447713/95bb07b7f556649d96e5cd55d7a06f3f6fc290cd/d3ac5f309efea7b7eb14b5e90cddc428.png" />
         <pubDate>2015-03-24 15:21:03 UTC</pubDate>
         <guid>https://padlet.com/jasminese1009/zt0eafb5m5c8/wish/54640902</guid>
      </item>
      <item>
         <title>S Wave</title>
         <author>jasminese1009</author>
         <link>https://padlet.com/jasminese1009/zt0eafb5m5c8/wish/55514826</link>
         <description><![CDATA[<p>S wave A type of elastic <b>wave</b>, the <b>S</b>-<b>wave</b>, secondary <b>wave</b>, or shear <b>wave</b>  is one of the two main types of elastic body <b>waves</b>, so named because they move through the body of an object, unlike surface </p>]]></description>
         <enclosure url="https://padlet-uploads.storage.googleapis.com/59447713/a1100eae30cd9054bcf74c86c6a06d9379863f42/fa1a28ec35c4d9bcb3c6cefa682fff0c.jpg" />
         <pubDate>2015-03-31 15:12:13 UTC</pubDate>
         <guid>https://padlet.com/jasminese1009/zt0eafb5m5c8/wish/55514826</guid>
      </item>
      <item>
         <title>P Wave </title>
         <author>jasminese1009</author>
         <link>https://padlet.com/jasminese1009/zt0eafb5m5c8/wish/55515482</link>
         <description><![CDATA[<p><b>P</b>-<b>waves</b> are a type of body <b>wave</b> that is the first <b>wave</b> to arrive at the seismograph, called seismic <b>waves</b> in seismology, that can travel through a continuum</p>]]></description>
         <enclosure url="https://padlet-uploads.storage.googleapis.com/59447713/90670a5d5d543dffd45456ecc01ebdbefb0d44dc/747ca4b40f30eb648e94a98b8b056723.gif" />
         <pubDate>2015-03-31 15:15:51 UTC</pubDate>
         <guid>https://padlet.com/jasminese1009/zt0eafb5m5c8/wish/55515482</guid>
      </item>
      <item>
         <title>Aftershock</title>
         <author>jasminese1009</author>
         <link>https://padlet.com/jasminese1009/zt0eafb5m5c8/wish/55515756</link>
         <description><![CDATA[<p></p><ol><li>An <b>aftershock</b> is a smaller <b>earthquake</b> that occurs after a previous large <b>earthquake</b>, in the same area of the main shock. If an <b>aftershock</b> is larger than the main shock, the <b>aftershock</b> is redesignated as the main shock and the original main shock is redesignated as a foreshock.</li></ol><p></p>]]></description>
         <enclosure url="https://padlet-uploads.storage.googleapis.com/59447713/dfcebd880cc3cd38ca60c187d873fc1e0cd3c314/c9a93c471bed139180f2d652d82011f8.gif" />
         <pubDate>2015-03-31 15:17:09 UTC</pubDate>
         <guid>https://padlet.com/jasminese1009/zt0eafb5m5c8/wish/55515756</guid>
      </item>
      <item>
         <title>Rictor Scale</title>
         <author>jasminese1009</author>
         <link>https://padlet.com/jasminese1009/zt0eafb5m5c8/wish/55516164</link>
         <description><![CDATA[<p>Rictor scale - smaller earthquake following the main shock of a large earthquake.is a base-10 logarithmic <b>scale</b>, which defines magnitude as the logarithm of the ratio of the amplitude of the seismic waves to an arbitrary, minor amplitude</p>]]></description>
         <enclosure url="https://padlet-uploads.storage.googleapis.com/59447713/0c6678abab25aa64b93278feb62b775b8c5d2db2/3bd7c808cd02cecd99d9c9c5721af51d.jpg" />
         <pubDate>2015-03-31 15:18:42 UTC</pubDate>
         <guid>https://padlet.com/jasminese1009/zt0eafb5m5c8/wish/55516164</guid>
      </item>
      <item>
         <title>Tectonic Volcanoes </title>
         <author>jasminese1009</author>
         <link>https://padlet.com/jasminese1009/zt0eafb5m5c8/wish/56047255</link>
         <description><![CDATA[<p></p><ol><li>A <b>volcano tectonic</b> earthquake is an earthquake induced by the movement (injection or withdrawal) of magma. The movement results in pressure changes in the rock around where the magma has experienced stress. At some point, the rock may break or move.</li></ol><p></p>]]></description>
         <enclosure url="https://padlet-uploads.storage.googleapis.com/59447713/3cee783139b7a6c1453dc39cd712e830a125db26/31829257352258a3b79af189e0366ffa.jpg" />
         <pubDate>2015-04-07 14:58:12 UTC</pubDate>
         <guid>https://padlet.com/jasminese1009/zt0eafb5m5c8/wish/56047255</guid>
      </item>
      <item>
         <title>Volcanic Volcanoes </title>
         <author>jasminese1009</author>
         <link>https://padlet.com/jasminese1009/zt0eafb5m5c8/wish/56047546</link>
         <description><![CDATA[<p></p><ol><li>A <b>volcano</b> is a rupture on the crust of a planetary-mass object, such as Earth, that allows hot lava, <b>volcanic</b> ash, and gases to escape from a magma chamber below the surface. Earth's <b>volcanoes</b> occur because its crust is broken into 17 major, rigid tectonic plates that float on a hotter, softer layer in its mantle.</li></ol><p></p>]]></description>
         <enclosure url="https://padlet-uploads.storage.googleapis.com/59447713/30d7d6f1c1f240e829cf8d65002af220bd1749d0/4d7bf40d9b6bf36cb4a837fbae47c7ba.jpg" />
         <pubDate>2015-04-07 14:59:56 UTC</pubDate>
         <guid>https://padlet.com/jasminese1009/zt0eafb5m5c8/wish/56047546</guid>
      </item>
      <item>
         <title>Collapse Volcanoes</title>
         <author>jasminese1009</author>
         <link>https://padlet.com/jasminese1009/zt0eafb5m5c8/wish/56048087</link>
         <description><![CDATA[<ol><li>A caldera is a cauldron-like&nbsp;<b>volcanic</b>&nbsp;feature usually formed by the <b>collapse</b>&nbsp;of land following a&nbsp;<b>volcanic eruption</b>. They are sometimes confused with&nbsp;<b>volcanic</b>&nbsp;craters. </li></ol>]]></description>
         <enclosure url="https://padlet-uploads.storage.googleapis.com/59447713/6e1740ef9cec38b78b0906d9a06a8113734a4454/7d6d5601543c992985fedb46e2733278.jpg" />
         <pubDate>2015-04-07 15:03:12 UTC</pubDate>
         <guid>https://padlet.com/jasminese1009/zt0eafb5m5c8/wish/56048087</guid>
      </item>
      <item>
         <title>Explosion </title>
         <author>jasminese1009</author>
         <link>https://padlet.com/jasminese1009/zt0eafb5m5c8/wish/56048240</link>
         <description><![CDATA[<p>An <b>explosive</b> eruption is a <b>volcanic</b> term to describe a violent, <b>explosive</b> type of eruption. </p>]]></description>
         <enclosure url="https://padlet-uploads.storage.googleapis.com/59447713/9288ab470dcea36cb4a79675580b25c21ce56059/089417dd4265602712503bee3ccbdc54.jpg" />
         <pubDate>2015-04-07 15:04:06 UTC</pubDate>
         <guid>https://padlet.com/jasminese1009/zt0eafb5m5c8/wish/56048240</guid>
      </item>
   </channel>
</rss>
