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  <title><![CDATA[Regional topographic relief map. (Naif et al)]]></title>
      <body><![CDATA[<p><span><span><span><strong><span><span>From&nbsp;the&nbsp;study:&nbsp;</span></span></strong></span></span></span><span><span><span><span><span><span>The&nbsp;Cocos&nbsp;and&nbsp;Nazca&nbsp;plates&nbsp;are&nbsp;formed&nbsp;at&nbsp;the&nbsp;EPR&nbsp;and&nbsp;the&nbsp;GSC.&nbsp;The&nbsp;Galápagos&nbsp;Triple&nbsp;Junction&nbsp;(GTJ)&nbsp;trace&nbsp;marks&nbsp;the&nbsp;boundary&nbsp;between&nbsp;EPR-&nbsp;and&nbsp;GSC-derived&nbsp;oceanic&nbsp;crusts.&nbsp;The&nbsp;Galápagos&nbsp;Plume&nbsp;is&nbsp;currently&nbsp;centered&nbsp;beneath&nbsp;the&nbsp;Galápagos&nbsp;Islands&nbsp;200&nbsp;km&nbsp;south&nbsp;of&nbsp;the&nbsp;GSC&nbsp;and&nbsp;generates&nbsp;two&nbsp;hot&nbsp;spot&nbsp;tracks,&nbsp;the&nbsp;Cocos&nbsp;Ridge&nbsp;and&nbsp;the&nbsp;Carnegie&nbsp;Ridge.&nbsp;</span></span></span></span></span></span></p>
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    <alt><![CDATA[Regional topographic relief map. ]]></alt>
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      <alt><![CDATA[Regional topographic relief map. ]]></alt>
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