<?xml version="1.0"?>
<rss version="2.0">
   <channel>
      <title>New Zealand by </title>
      <link>https://padlet.com/09055_casp/7tfoltcpb7cd</link>
      <description>Nuria Alomar, Clara Gonzalvo and Andrea Casserres</description>
      <language>en-us</language>
      <pubDate>2017-06-12 13:34:48 UTC</pubDate>
      <lastBuildDate>2017-06-13 08:17:54 UTC</lastBuildDate>
      <webMaster>hello@padlet.com</webMaster>
      <image>
         <url></url>
      </image>
      <item>
         <title>INTRODUCTION</title>
         <author>09055_casp</author>
         <link>https://padlet.com/09055_casp/7tfoltcpb7cd/wish/176099179</link>
         <description><![CDATA[<div><br></div><blockquote>New Zealand is a country that is located in the convergence between three tectonic plates with results of volcanic activity and small earthquakes in the North Island and the South. The islands and their surroundings have hundreds and hundreds of volcanoes, most of them extinct. The most active are those we can find in White Island, near Tuaranga, in the Bay of Plenty.</blockquote>]]></description>
         <enclosure url="" />
         <pubDate>2017-06-12 13:37:15 UTC</pubDate>
         <guid>https://padlet.com/09055_casp/7tfoltcpb7cd/wish/176099179</guid>
      </item>
      <item>
         <title>OMANAWA RIVER</title>
         <author>09055_casp</author>
         <link>https://padlet.com/09055_casp/7tfoltcpb7cd/wish/176105045</link>
         <description><![CDATA[<div><strong>External agents: </strong>fluvial model.<br> It flows north from the northern edge of the Mamaku Plateau, reaching the Wairoa River 10 kilometres southwest of Tauranga. </div>]]></description>
         <enclosure url="https://s-media-cache-ak0.pinimg.com/564x/10/52/44/105244e8e63bec77d88bfd19678b71ca.jpg" />
         <pubDate>2017-06-12 14:10:37 UTC</pubDate>
         <guid>https://padlet.com/09055_casp/7tfoltcpb7cd/wish/176105045</guid>
      </item>
      <item>
         <title>MEANDER AT HAMILTON GARDENS</title>
         <author>09055_casp</author>
         <link>https://padlet.com/09055_casp/7tfoltcpb7cd/wish/176109784</link>
         <description><![CDATA[<div><strong>External agents: </strong>Erotion and depositon<br><strong>Process:</strong> The meander are formed when the moving water in a stream erodes the outer banks. In the inner part has deposites less energy of wàter and the outer part deposites more energy of water.<br><br></div>]]></description>
         <enclosure url="https://cdn.eventfinda.co.nz/uploads/locations/transformed/170356-1139-14.jpg" />
         <pubDate>2017-06-12 14:36:40 UTC</pubDate>
         <guid>https://padlet.com/09055_casp/7tfoltcpb7cd/wish/176109784</guid>
      </item>
      <item>
         <title>OPUIAKI RIVER</title>
         <author>09055_casp</author>
         <link>https://padlet.com/09055_casp/7tfoltcpb7cd/wish/176111137</link>
         <description><![CDATA[<div><strong>External agents: </strong>fluvial model.<br><strong>Process: </strong>The Opuiaki River is a river of the Bay of Plenty Region of New Zealand's North Island</div>]]></description>
         <enclosure url="http://static.panoramio.com/photos/large/19782965.jpg" />
         <pubDate>2017-06-12 14:44:16 UTC</pubDate>
         <guid>https://padlet.com/09055_casp/7tfoltcpb7cd/wish/176111137</guid>
      </item>
      <item>
         <title>MILFORD SOUND</title>
         <author></author>
         <link>https://padlet.com/09055_casp/7tfoltcpb7cd/wish/176205550</link>
         <description><![CDATA[<div><strong>External agents: </strong>fluvial model.<br><strong>Process: </strong>Is a fjord located in the southwest of the South Island of New Zealand.<br><br><br></div>]]></description>
         <enclosure url="https://www.realjourneys.co.nz/media/697678/7945-milford-sound-cruise.jpg?crop=0,0.11927050288758743,0,0.2810223228810802&amp;cropmode=percentage&amp;width=1920&amp;height=768&amp;rnd=131174855000000000" />
         <pubDate>2017-06-13 07:41:13 UTC</pubDate>
         <guid>https://padlet.com/09055_casp/7tfoltcpb7cd/wish/176205550</guid>
      </item>
      <item>
         <title>MOUNT RUAPEHU</title>
         <author></author>
         <link>https://padlet.com/09055_casp/7tfoltcpb7cd/wish/176207260</link>
         <description><![CDATA[<div><strong>External agents: </strong>Erotion and depositon<br><strong>process: </strong>Ruapehu, the largest active volcano in New Zealand, is the highest point on the North Island and has three major peaks<br><br></div>]]></description>
         <enclosure url="https://upload.wikimedia.org/wikipedia/commons/thumb/0/07/Tongariro_Northern_Circuit%2C_New_Zealand_%285%29.JPG/280px-Tongariro_Northern_Circuit%2C_New_Zealand_%285%29.JPG" />
         <pubDate>2017-06-13 07:58:00 UTC</pubDate>
         <guid>https://padlet.com/09055_casp/7tfoltcpb7cd/wish/176207260</guid>
      </item>
   </channel>
</rss>
