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Habitat Where an organism lives
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Depressions filed with sea water that we call oceans
Ocean Basin Depressions filed with sea water that we call oceans
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Pacific Largest and deepest
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Atlantic & Indian About half the size as the Pacific & almost as deep
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Smallest and shallowest
Arctic Smallest and shallowest
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Density Mass per unit volume D = m/V
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Earth's Structure Inner core: 0-1200 km Outer core: 1200-2500 km
Mantle: km Crust: Outer most 100 km
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Oceanic Crust Crust directly under oceans thin & dense
made of mostly basalt
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Continental Crust Crust containing the continents thick & less dense
Made of mostly granite
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The Earth’s crust is made up of many plate that are in constant motion
Plate Tectonics The Earth’s crust is made up of many plate that are in constant motion
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Original supercontinent containing all of the present day continents
Pangaea Original supercontinent containing all of the present day continents
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Plate Boundary Crack between plates Where two plate meet Fault line
Rift
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Types of Boundaries Mid-ocean Ridges Subduction Boundary
Shear Boundary Mountain Range
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Mid-Ocean Ridge Spreading center
Continuous chain of volcanic submarine mountains that encircle the globe Like seams on a baseball
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Subduction When an oceanic plate slides under another plate
Both volcanic and earthquake activity occur Forms very deep trenches
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Shear Boundary When two plates slide parallel to each other
Only earthquake activity San Andreas Fault
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Mountain Range Forms when two continental plates collide
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Hot Spot Forms when there is enough heat upwelling to form a volcano, but not enough to form a mid-ocean ridge
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Continental Margin Where the continent meets the sea
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Active Margin A continental margin that is geologically active
A continental margin near a plate boundary USA’s west coast
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Passive Margin A continental margin with no geological activity
A continental margin not near a plate boundary USA’s east coast
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Sediment Loose material like sand or mud that settles to the bottom of any body of water Sediment thickness increases as you move from m-o-r
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Types of Sediment Lithogenous: from a non-living source
Biogenous: from a living source
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Calcareous Ooze Carbon based sediment
Sediment containing calcium carbonate CaCO3
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Siliceous Ooze Silicon based sediment
Sediment containing silicon dioxide or silicates SiO2 or SiO4-4
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Oceanic volcanoes that do not penetrate the surface of the ocean
Seamounts Oceanic volcanoes that do not penetrate the surface of the ocean
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Guyots Flat-topped seamounts Seamounts that are no longer active
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Oceanic hot spot where hot gases escape through the ocean floor
Hydrothermal Vent Oceanic hot spot where hot gases escape through the ocean floor
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Black Smoker Another name for hydrothermal vents
As hydrogen sulfide gas precipitates in cold water, you get a black precipitate
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Passive Margins Parts Continental shelf Shelf break Continental slope
Continental rise The Abyss
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Continental Shelf Nearly flat, slightly sloping, not too deep area just off the shoreline
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Where the continental shelf abruptly breaks off into a steep slope
Shelf Break Where the continental shelf abruptly breaks off into a steep slope
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Continental Slope The steeply sloping part of the margin that goes from the shelf break to the ocean floor
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Where sediment builds up between the slope and the abyss
Continental Rise Where sediment builds up between the slope and the abyss
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The Abyss The Ocean Floor The Abyssal plain
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Active Margin Parts Continental Shelf Shelf Break Continental Slope
Trench The Abyss
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In the water column or at any depth in the sea
Pelagic In the water column or at any depth in the sea
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Pelagic Zones Epipelagic Mesopelagic Bathopelagic Abyssopelagic
Hadopelagic
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Epipelagic Zone Surface water where light can penetrate & photosynthesis can take place Photic zone
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Mesopelagic Zone Middle zone, just below the epipelagic where no light penetrates, but is shadowy Twilight zone
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Bathopelagic Zone Deep ocean water where no light penetrates and it is pitch black Complete darkness
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Abyssopelagic Zone The water near the sea floor Bottom water
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Hadopelagic Zone Sea water in the deep trenches Trench water
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The Deep Sea Because the bathopelagic, abyssopelagic, & hadopelagic zones are so similar, they are lumped together as the deep sea
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