GET https://junior.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/en/media/585-lithospheric-plates

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App\Entity\MediaTranslation
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App\Entity\MediaTranslation {#1397
  -id: 4463
  -title: "Lithospheric plates"
  -description: """
    <p>Different types of observations related to lithospheric plates:</p>\r\n
    \r\n
    <ul>\r\n
    \t<li>locations of plates.</li>\r\n
    \t<li>topography.</li>\r\n
    \t<li>age of the ocean floor.</li>\r\n
    \t<li>locations of recent seismic activity and active volcanism.</li>\r\n
    \t<li>geothermic waves emerging from the Earth.</li>\r\n
    </ul>
    """
  -legends: """
    Ridge volcanism\r\n
    Active volcano\r\n
    Rift\r\n
    from 0 to 5\r\n
    Subduction zone\r\n
    Collision zone\r\n
    Velocity in cm per year\r\n
    South-American plate\r\n
    North-American plate\r\n
    Indo-Australian plate\r\n
    Eurasian plate\r\n
    Philippine plate\r\n
    Cocos plate\r\n
    Caroline plate\r\n
    Caribbean plate\r\n
    African plate\r\n
    Pacific plate\r\n
    Nazca plate\r\n
    Antarctic plate\r\n
    Arabic plate\r\n
    Lithospheric plates and their relative movements\r\n
    The Earth's surface topography\r\n
    The distribution of the geothermic flow coming from Earth's interior\r\n
    The age of the ocean floor (million years)\r\n
    The recent seismic activity and the active volcanism\r\n
    Hypothetical boundary\r\n
    Divergent boundary\r\n
    Geothermic flow in mW/m²\r\n
    Recent earthquake epicenter\r\n
    Select a map\r\n
    Altitude above sea level\n(in meters)\r\n
    Age in millions of years\r\n
    1000 and more\r\n
    Plate movement\r\n
    Scotia Plate\r\n
    Plates and relative movements\r\n
    Topography\r\n
    Age of the oceanic floor\r\n
    Seismic activity and volcanism\r\n
    Geothermic flow\r\n
    -7000 to -5000\r\n
    -5000 to -3000\r\n
    -3000 to 0\r\n
    0 to 500\r\n
    500 to 1000\r\n
    > 1000\r\n
    from 0 to 5\r\n
    from 5 to 25\r\n
    from 25 to 60\r\n
    60 and more\r\n
    from 20 to 60\r\n
    from 60 to 100\r\n
    from 100 to 200\r\n
    from 200 to 400\r\n
    Juan de Fuca\nPlate
    """
  -goals: """
    <ul>\r\n
    \t<li>To observe the arrangement of the lithospheric plates and their respective movements.</li>\r\n
    \t<li>To make the connection between the ocean floor&rsquo;s topography, seismic and volcanic activity, the age of ocean floors and geothermic waves.</li>\r\n
    </ul>
    """
  -more: """
    <p>On the surface of the Earth, a rigid layer called the <strong>lithosphere </strong>is composed of 11 mobile plates, on which continents rest. These plates renew themselves and grow at the level of the <strong>ocean ridges</strong>; this phenomenon is called <strong>accretion</strong>. They disappear when they go under other plates in <strong>subduction zones</strong>. Continents are carried along by the movements of the <strong>lithospheric plates</strong>, which are themselves carried along by convective motions in the mantle. When the floor moves, the surface is also modified. The lithosphere, which extends from the surface to 70-150 km deep, includes the crust of the earth and the upper part of the mantle.<br />\r\n
    <br />\r\n
    The oldest parts of the ocean&rsquo;s crust are the farthest from the ridges and are millions of years old.<br />\r\n
    <br />\r\n
    Correlation with the distribution of seismic and volcanic phenomena indicates the edges of the plates. But volcanoes born from <strong>hot spots </strong>can also be found inside the plates.<br />\r\n
    <br />\r\n
    The Earth internal heat constantly dissipates, but in an uneven way on the globe&rsquo;s surface. The internal energy&rsquo;s dissipation is mainly expressed by a wave of heat or <strong>geothermic wave</strong>. These waves are more extensive along the ridges and weaker near the continents.</p>
    """
  -scenario: null
  -features: "<p><strong>Rollover </strong>the map to see the borders of the lithospheric plates.\n<strong>Select</strong> other maps in the menu.</p>"
  -publishedAt: DateTimeImmutable @1431302400 {#1394
    date: 2015-05-11 00:00:00.0 UTC (+00:00)
  }
  -preventIndexForSearch: false
  #locale: "en"
  #translatable: App\Entity\Media {#1308 …}
  #status: "published"
  #createdAt: DateTime @1208988000 {#1395
    date: 2008-04-23 22:00:00.0 UTC (+00:00)
  }
  #updatedAt: DateTime @1704142563 {#1396
    date: 2024-01-01 20:56:03.0 UTC (+00:00)
  }
}
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