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The Ocean Floor
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Description of Bottom Topography
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Atlantic Ocean Continental Shelf
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Typical Oceanic Profile
continental margin ocean basin coastal region oceanic ridge continental shelf Slope Abyssal plain Depth > 4000 m
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The Continental Margin
ocean basin shelf break coastal region oceanic ridge continental shelf Slope Abyssal plain continental rise > 4000 m
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Continental Margin Fig. 2-3a
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Continental Shelf
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Coastal Region • Includes: •beaches •estuaries • lagoons • marshes
• deltas coastal region Most important region to humans And marine birds and mammals
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Beaches
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Typical Salt Marsh
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Mangrove Swamp
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Continental Shelf less than 0.1° angle
• Definition: shallow part of ocean bottom next to coastline continental margin • SLOPE is less than 0.1° angle continental shelf Slope continental rise
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Most exposed in Pleistocene
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Continental Slope and Rise
• Slope is 1° to 6° • Rise: less than 1° Rise is about 20 km in Atlantic along passive margins Can be absent altogether in active margins with trenches. • Slope & rise can be cut by submarine canyons Slope Continental rise
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Overlapping fans=cones See Fig. 2-3a
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San Lucas Submarine Canyon
2 meters
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Typical Oceanic Profile
continental margin ocean basin shelf break oceanic ridge continental shelf Slope Abyssal plain continental rise
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Are the deep flat areas of the ocean
Ocean Basins Are the deep flat areas of the ocean
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Deep Ocean Basins Fig. 2-3b
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May rise above the surface
Seamounts and Guyots- undersea mountains that rise more than 1 km from the seafloor SEAMOUNT Top is rounded May rise above the surface and form an island GUYOT Top flattened by waves
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3 Major Oceanic Ridges Mid-Atlantic Ridge Carlsberg Ridge E. Pacific
Rise
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The largest is the Mid Atlantic Ridge half that separatat
Characteristics of Oceanic Mountain Ridges • Total length: 60,000 km • Present in all oceans • Between 1,000 and 4,000 km wide • mountains are km high The largest is the Mid Atlantic Ridge half that separatat
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Mid-Ocean Ridges Fig. 2-3c
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Mid-Atlantic Ridge Shallow valleys km wide with high volcanic activity
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Oceanic Trenches • 31 in the world; • Deep; U or V shaped
•These form the deepest places on Earth • Max 130 km wide, 1500 km long
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Distribution of Trenches
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Kurile 10,500 m Mariana 11,000 m Tonga 10,880 m 3 _________ trenches
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Island Arcs are associated with volcanoes
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Atlantic Ocean Pacific Ocean shelf slope hills Ridge plains island arc
seamounts ridge plain trench Pacific Ocean
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HYDROTHERMAL VENTS or BLACK SMOKERS
At a hydrothermal vent, sea water that has sunken into cracks in the ocean crust and been heated (sometimes to over 180 degrees!) by the interior of the earth escapes through crust cracks back into the ocean.
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The superheated water beneath the oceanic crust often dissolves minerals from nearby rocks.
The precipitating minerals often give vent fluids different colored “smoky” appearances.
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As hot vent fluids meet cold ocean water, minerals precipitate (fall) out of vent fluids.
The precipitating minerals form “chimneys” and other formations on the sea floor.
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Hydrothermal Vent Sites
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