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Warm Up 12-5-14

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Warm Up 12-5-14 1. What are the four minerals that compose salt water? 2. What are the three reasons the ocean is salty? 3. What percentage of a drop of water ... – PowerPoint PPT presentation

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Title: Warm Up 12-5-14


1
Warm Up 12-5-14
  • 1. What are the four minerals that compose salt
    water?
  • 2. What are the three reasons the ocean is
    salty?
  • 3. What percentage of a drop of water contains
    sea salt?
  • 4. What are the parts of the continental margin?

2
Ocean Landforms
3
The Ocean Floor
4
Revealing the Ocean Floor
  • If you could travel to the bottom of the ocean,
    you would see the worlds largest mountain chain
    and canyons much deeper than the Grand Canyon.
  • How can the ocean floor be mapped?

5
Revealing the Ocean Floor
  • Sonar (stands for Sound Navigation and Ranging)
  • Invented in the 1920s
  • Primary instrument for measuring depth
  • Reflects sound from ocean floor

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Revealing the Ocean Floor
  • Use of satellites for mapping
  • Employs satellites equipped with radar altimeters
  • Scientists are able to measure the direction and
    speed of ocean currents.
  • Measure the different heights of the ocean water
    surface to make maps of ocean floor.
  • Can cover more territory using satellites rather
    than ship sonar.

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Continents Edge
  • Called the continental margin
  • Three parts
  • Continental shelf
  • Continental slope
  • Continental rise

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Continental Shelf
  • Begins at the shoreline, Depth can reach 200
    meters, meets the continental slope.
  • This is what you walk on at the beach.

18
Continental Slope
  • Begins at the edge of shelf, Depth ranges from
    200 meters to 4000 meters
  • Continent ends at bottom of continental slope

19
Continental Rise
  • Slopes more gently
  • Made of sediments that come off the shelf
  • Like underwater avalanches of sediment and
    water

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Abyssal Plain
  • Broad, flat portion of the deep-ocean floor.
  • Covered with mud and remains of marine organisms.
  • Average depth is 4,000 meters

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Mid-Ocean Ridges
  • Mountain chains formed where tectonic plates pull
    apart.
  • Pulling motion creates cracks in the crust called
    rift zones.
  • Rift Valley forms between mountains in the
    mid-ocean ridge.

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Seamounts
  • Individual mountains of volcanic material.
  • If a seamount builds up above sea level, it
    becomes an island.
  • A guyot is a flat-topped seamount.

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Actual footage of an erupting underwater volcano.
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Ocean Trench
  • bottomless cracks in the ocean basin (floor).
  • Formed where one oceanic plate is forced
    underneath another plate.
  • Most famous Marianas Trench

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