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      <title>Oceanic Basin by Joshell Ballano</title>
      <link>https://padlet.com/ballanojoshell09/pf6zhmkldlcnip1b</link>
      <description>An oceanic basin is the land surface under an ocean that includes the various topography below the water.</description>
      <language>en-us</language>
      <pubDate>2023-01-30 23:46:40 UTC</pubDate>
      <lastBuildDate>2023-02-01 12:20:54 UTC</lastBuildDate>
      <webMaster>hello@padlet.com</webMaster>
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      <item>
         <title>The Structure of Ocean Basins</title>
         <author>ballanojoshell09</author>
         <link>https://padlet.com/ballanojoshell09/pf6zhmkldlcnip1b/wish/2464363019</link>
         <description><![CDATA[<div>The continental margins of major features of the ocean floor are<br><br></div>]]></description>
         <enclosure url="https://padlet-uploads.storage.googleapis.com/1949741433/ac6fa17fe408ef5520a1fae0b12a36ce/ocean_floor_sea_underwater_relief_260nw_1089473621.webp" />
         <pubDate>2023-02-01 10:33:12 UTC</pubDate>
         <guid>https://padlet.com/ballanojoshell09/pf6zhmkldlcnip1b/wish/2464363019</guid>
      </item>
      <item>
         <title>Continental Shelf </title>
         <author>ballanojoshell09</author>
         <link>https://padlet.com/ballanojoshell09/pf6zhmkldlcnip1b/wish/2464365314</link>
         <description><![CDATA[<ul><li>&nbsp;is a portion of a continent that is submerged under an area of relatively shallow water, known as a shelf sea.</li><li>less than 150 meters of water depth</li></ul>]]></description>
         <enclosure url="https://padlet-uploads.storage.googleapis.com/1949741433/dd0d3d43f1f60f762fc567b7805553c7/continental_shelf.png" />
         <pubDate>2023-02-01 10:35:27 UTC</pubDate>
         <guid>https://padlet.com/ballanojoshell09/pf6zhmkldlcnip1b/wish/2464365314</guid>
      </item>
      <item>
         <title>Continental Slope </title>
         <author>ballanojoshell09</author>
         <link>https://padlet.com/ballanojoshell09/pf6zhmkldlcnip1b/wish/2464368027</link>
         <description><![CDATA[<ul><li>depth up to 1200 meters</li><li>is a geological feature marking the divide between two ocean zones.</li></ul>]]></description>
         <enclosure url="https://padlet-uploads.storage.googleapis.com/1949741433/4044242c57afa9b56eb5a9f7ec93ea2f/1280_continental_slope.png" />
         <pubDate>2023-02-01 10:38:04 UTC</pubDate>
         <guid>https://padlet.com/ballanojoshell09/pf6zhmkldlcnip1b/wish/2464368027</guid>
      </item>
      <item>
         <title>Continental Rise</title>
         <author>ballanojoshell09</author>
         <link>https://padlet.com/ballanojoshell09/pf6zhmkldlcnip1b/wish/2464374303</link>
         <description><![CDATA[<ul><li>at the base of the continental slope&nbsp;</li><li>is a wide, gentle incline from a deep ocean plain (abyssal plain) to a continental slope.</li></ul>]]></description>
         <enclosure url="" />
         <pubDate>2023-02-01 10:43:11 UTC</pubDate>
         <guid>https://padlet.com/ballanojoshell09/pf6zhmkldlcnip1b/wish/2464374303</guid>
      </item>
      <item>
         <title>Type of margins</title>
         <author>ballanojoshell09</author>
         <link>https://padlet.com/ballanojoshell09/pf6zhmkldlcnip1b/wish/2464382053</link>
         <description><![CDATA[<ol><li>Active (less than 1 kilometer wide) Active new ocean basins have a lot of new structures being created and shaped.</li><li>Passive (hundreds of kilometer wide)<br>&nbsp;Inactive surface is slow to change and does little more than collect sediment.</li></ol><div><br></div>]]></description>
         <enclosure url="" />
         <pubDate>2023-02-01 10:50:22 UTC</pubDate>
         <guid>https://padlet.com/ballanojoshell09/pf6zhmkldlcnip1b/wish/2464382053</guid>
      </item>
      <item>
         <title>Abyssal fan</title>
         <author>ballanojoshell09</author>
         <link>https://padlet.com/ballanojoshell09/pf6zhmkldlcnip1b/wish/2464398970</link>
         <description><![CDATA[<ul><li>also known as deep-sea fans, underwater deltas, and submarine fans, are underwater geological structures associated with large-scale sediment deposition and formed by turbidity currents.&nbsp;</li></ul><div><br></div>]]></description>
         <enclosure url="https://youtu.be/9Ghm5iHaB34" />
         <pubDate>2023-02-01 11:07:30 UTC</pubDate>
         <guid>https://padlet.com/ballanojoshell09/pf6zhmkldlcnip1b/wish/2464398970</guid>
      </item>
      <item>
         <title>Mid ocean ridges </title>
         <author>ballanojoshell09</author>
         <link>https://padlet.com/ballanojoshell09/pf6zhmkldlcnip1b/wish/2464416800</link>
         <description><![CDATA[<ul><li>Above the oceanic floor</li><li>At the center of oceans basins</li><li>23% of the earth’s surface water</li><li>Long linear mountain chain in all oceans and bound basins</li><li>Fracture zones are perpendicular to ridges&nbsp;</li></ul>]]></description>
         <enclosure url="https://padlet-uploads.storage.googleapis.com/1949741433/8ad42a4050bfa7132096fa242c2d1d15/Illustrations_of_Mid_Ocean_Ridge__1_.png" />
         <pubDate>2023-02-01 11:24:36 UTC</pubDate>
         <guid>https://padlet.com/ballanojoshell09/pf6zhmkldlcnip1b/wish/2464416800</guid>
      </item>
      <item>
         <title>Oceanic Trenches </title>
         <author>ballanojoshell09</author>
         <link>https://padlet.com/ballanojoshell09/pf6zhmkldlcnip1b/wish/2464438332</link>
         <description><![CDATA[<ul><li>is a deep indent in the surface floor of the ocean and is the deepest part of the ocean</li><li>They are typically 50 to 100 kilometers wide and 3 to 4 km below the level of the surrounding oceanic floor, but can be thousands of kilometers in length</li></ul>]]></description>
         <enclosure url="https://padlet-uploads.storage.googleapis.com/1949741433/57f575bc4ab15b6b2e35e0d2c1c754e5/pt9_ocean_trenches_noaa.jpg" />
         <pubDate>2023-02-01 11:46:33 UTC</pubDate>
         <guid>https://padlet.com/ballanojoshell09/pf6zhmkldlcnip1b/wish/2464438332</guid>
      </item>
      <item>
         <title>Guyot </title>
         <author>ballanojoshell09</author>
         <link>https://padlet.com/ballanojoshell09/pf6zhmkldlcnip1b/wish/2464448090</link>
         <description><![CDATA[<ul><li>or seamount, is an undersea mountain&nbsp;</li><li>Seamounts are formed by volcanic activity and can be taller than 10,000 feet.</li><li>They can be isolated or part of large mountain chains</li></ul>]]></description>
         <enclosure url="" />
         <pubDate>2023-02-01 11:55:49 UTC</pubDate>
         <guid>https://padlet.com/ballanojoshell09/pf6zhmkldlcnip1b/wish/2464448090</guid>
      </item>
      <item>
         <title>Stages of Ocean Basins Evolution (Wilson Cycle)</title>
         <author>ballanojoshell09</author>
         <link>https://padlet.com/ballanojoshell09/pf6zhmkldlcnip1b/wish/2464460482</link>
         <description><![CDATA[<ol><li>Embryonic&nbsp;</li><li>Juvenile&nbsp;</li><li>Mature&nbsp;</li><li>Declining&nbsp;</li><li>Terminal</li><li>Relict scar</li></ol>]]></description>
         <enclosure url="https://padlet-uploads.storage.googleapis.com/1949741433/e4253d4c82661d0024229590bebbac0d/Rock_cycle_in_Wilson_Cycle.png" />
         <pubDate>2023-02-01 12:07:33 UTC</pubDate>
         <guid>https://padlet.com/ballanojoshell09/pf6zhmkldlcnip1b/wish/2464460482</guid>
      </item>
      <item>
         <title>Embryonic </title>
         <author>ballanojoshell09</author>
         <link>https://padlet.com/ballanojoshell09/pf6zhmkldlcnip1b/wish/2464465469</link>
         <description><![CDATA[<ul><li>Continental rifting plays a key role in the formation of an ocean.</li><li>A new basin will become part of the eventual continental shelf-slope-rise zone</li></ul>]]></description>
         <enclosure url="" />
         <pubDate>2023-02-01 12:11:23 UTC</pubDate>
         <guid>https://padlet.com/ballanojoshell09/pf6zhmkldlcnip1b/wish/2464465469</guid>
      </item>
      <item>
         <title>Juvenile </title>
         <author>ballanojoshell09</author>
         <link>https://padlet.com/ballanojoshell09/pf6zhmkldlcnip1b/wish/2464467963</link>
         <description><![CDATA[<ul><li>Seafloor basalts begin forming&nbsp;</li><li>Fairly shallow&nbsp;</li><li>Normal marine sedimentation of muds, sand and limestone depending on local conditions.</li></ul>]]></description>
         <enclosure url="" />
         <pubDate>2023-02-01 12:12:51 UTC</pubDate>
         <guid>https://padlet.com/ballanojoshell09/pf6zhmkldlcnip1b/wish/2464467963</guid>
      </item>
      <item>
         <title>Mature</title>
         <author>ballanojoshell09</author>
         <link>https://padlet.com/ballanojoshell09/pf6zhmkldlcnip1b/wish/2464469214</link>
         <description><![CDATA[<ul><li>Broad as it widen&nbsp;</li><li>Fairly shallow</li><li>Trenches develop and subduction begin</li><li>Abyssal plains form</li><li>Fully-developed shelf-slope-rise zone&nbsp;</li></ul><div><br></div>]]></description>
         <enclosure url="" />
         <pubDate>2023-02-01 12:13:45 UTC</pubDate>
         <guid>https://padlet.com/ballanojoshell09/pf6zhmkldlcnip1b/wish/2464469214</guid>
      </item>
      <item>
         <title>Declining </title>
         <author>ballanojoshell09</author>
         <link>https://padlet.com/ballanojoshell09/pf6zhmkldlcnip1b/wish/2464470355</link>
         <description><![CDATA[<ul><li>Subduction eliminates much of seafloor and oceanic ridges</li><li>Dominant are spreading and shrinking&nbsp;</li></ul>]]></description>
         <enclosure url="" />
         <pubDate>2023-02-01 12:14:51 UTC</pubDate>
         <guid>https://padlet.com/ballanojoshell09/pf6zhmkldlcnip1b/wish/2464470355</guid>
      </item>
      <item>
         <title>Terminal</title>
         <author>ballanojoshell09</author>
         <link>https://padlet.com/ballanojoshell09/pf6zhmkldlcnip1b/wish/2464471169</link>
         <description><![CDATA[<ul><li>African plate is being consumed under of European plate</li><li>the continents are not yet touching but subduction of the intervening oceanic crust causes a narrowing of the sea separating the continents</li></ul>]]></description>
         <enclosure url="" />
         <pubDate>2023-02-01 12:15:40 UTC</pubDate>
         <guid>https://padlet.com/ballanojoshell09/pf6zhmkldlcnip1b/wish/2464471169</guid>
      </item>
      <item>
         <title>Suturing</title>
         <author>ballanojoshell09</author>
         <link>https://padlet.com/ballanojoshell09/pf6zhmkldlcnip1b/wish/2464477060</link>
         <description><![CDATA[<ul><li>Continental collision&nbsp;</li><li>Shrinking and uplifting of young mountains</li><li>Example can be given are the himalaya mountains</li></ul>]]></description>
         <enclosure url="" />
         <pubDate>2023-02-01 12:20:47 UTC</pubDate>
         <guid>https://padlet.com/ballanojoshell09/pf6zhmkldlcnip1b/wish/2464477060</guid>
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