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The Ocean Floor. The Ocean Floor. The World Ocean Imaging the Ocean Floor Continental Margins The Deep-Ocean Floor Oceanic Ridges Seafloor Sediments. Terms. Oceanography: An Interdisciplinary Science. PSCI 131: The Ocean Floor. Geology Ocean floor, oceanic crust Biology Marine life
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The Ocean Floor • The World Ocean • Imaging the Ocean Floor • Continental Margins • The Deep-Ocean Floor • Oceanic Ridges • Seafloor Sediments
Oceanography: An Interdisciplinary Science PSCI 131: The Ocean Floor • Geology • Ocean floor, oceanic crust • Biology • Marine life • Chemistry • Composition of ocean water • Physics • Waves, heat transfer, ocean circulation
The World Ocean PSCI 131: The Ocean Floor
The World Ocean PSCI 131: The Ocean Floor Earth’s surface is 71% ocean Majority is in Southern Hemisphere Northern Hemisphere Southern Hemisphere
Oceans vs. Continents PSCI 131: The Ocean Floor: The World Ocean • Continents • Average elev.: about 2800 feet above sea level • Highest point: about 30,000 feet a.s.l. • Oceans • Average depth: about 12,200 feet • Deepest point: about 36,000 feet
Imaging the Ocean Floor PSCI 131: The Ocean Floor
Ocean Floor Mapping PSCI 131: The Ocean Floor: Imaging the Ocean Floor • HMS Challenger • British • 1872-1876 • All oceans except Arctic • Used weighted ropes to find ocean depths
Ocean Floor Mapping PSCI 131: The Ocean Floor: Imaging the Ocean Floor • HMS Challenger’s route • British • 1872-1876 • All oceans except Arctic • Used weighted ropes to find ocean depths
Ocean Floor Mapping PSCI 131: The Ocean Floor: Imaging the Ocean Floor • Sonar • Single beam • Multibeam
Ocean Floor Mapping PSCI 131: The Ocean Floor: Imaging the Ocean Floor • Sonar • Travel time of ping / 2 = depth
Seismic Reflection Profiles PSCI 131: The Ocean Floor: Imaging the Ocean Floor • Seismic waves penetrate mud, bounce off rock
Seismic Reflection Profiles PSCI 131: The Ocean Floor: Imaging the Ocean Floor
Ocean Floor Provinces PSCI 131: The Ocean Floor: Imaging the Ocean Floor • Revealed by ocean floor imaging techniques • Continental margins • Passive and active • Deep-ocean floor • Oceanic ridges
Ocean Floor Provinces PSCI 131: The Ocean Floor: Imaging the Ocean Floor
Continental Margins PSCI 131: The Ocean Floor
Continental Margin Types PSCI 131: The Ocean Floor: Continental Margins • Passive • Little geologic activity • Gentle slope • Flatter coastlines • Active • Frequent geologic activity • Steeper slope • More rugged coastlines
Passive Margins PSCI 131: The Ocean Floor: Continental Margins
Passive Margins PSCI 131: The Ocean Floor: Continental Margins
Passive Margin Formation PSCI 131: The Ocean Floor: Continental Margins Crustal stretching & thinning Initial, narrow ocean basin forms Mature basin with passive margins
Passive Margins: Submarine Canyons PSCI 131: The Ocean Floor: Continental Margins Undersea “landslides” move down continental slopes and cut into shelves to form submarine canyons.
Passive Margins: The Hudson submarine canyon PSCI 131: The Ocean Floor: Continental Margins Modern Hudson River mouth Hudson River mouth during last ice age
PSCI 131: The Ocean Floor: Continental Margins Active Margins (aka subduction zones)
PSCI 131: The Ocean Floor: Continental Margins Active Margins (aka subduction zones)
The Deep-Ocean Basin PSCI 131: The Ocean Floor
Key Deep-Ocean Basin Features PSCI 131: The Ocean Floor: The Deep-Ocean Basin • Abyssal plains • Trenches • Seamounts
Abyssal Plains PSCI 131: The Ocean Floor: The Deep-Ocean Basin • Very flat • Deep sediment
Abyssal Plains PSCI 131: The Ocean Floor: The Deep-Ocean Basin Abyssal plains are dark blue
Trenches PSCI 131: The Ocean Floor: The Deep-Ocean Basin • Deepest places in the oceans • Subduction-related • Sediment traps Florida Puerto Rico Trench
Seamounts PSCI 131: The Ocean Floor: The Deep-Ocean Basin • Undersea volcanoes • Form islands if peaks are above sea level • Most are not
Oceanic Ridges PSCI 131: The Ocean Floor
Oceanic Ridges PSCI 131: The Ocean Floor: Oceanic Ridges • Elevated, linear features
Oceanic Ridges PSCI 131: The Ocean Floor: Oceanic Ridges • Also called “spreading centers” or “divergent plate boundaries” • Two crustal plates are spreading apart • New crust formed at center of ridge
Diagram of an oceanic ridge PSCI 131: The Ocean Floor: Oceanic Ridges Central rift valley w/ volcanoes Plate motion Plate motion Fault blocks Rising molten rock from mantle
Oceanic ridge formation PSCI 131: The Ocean Floor: Oceanic Ridges
Earth’s Largest Topographic Feature PSCI 131: The Ocean Floor: Oceanic Ridges • Over 70,000 miles long
Seafloor Sediments PSCI 131: The Ocean Floor
Ocean Sediment Types PSCI 131: The Ocean Floor: Seafloor Sediments • Terrigenous (~45% of ocean floor) • “Terra” = earth • Derived from continents • Biogenous (~55%) • Created by organisms • Hydrogenous (<1 %) • Crystallize out of seawater
Terrigenous Sediments PSCI 131: The Ocean Floor: Seafloor Sediments • Concentrated along continental margins • Mineral and rock material • From rivers, wind, glaciers
Biogenous Sediments PSCI 131: The Ocean Floor: Seafloor Sediments • Concentrated away from continents • Mainly dead plankton shells White Cliffs of Dover, England – ancient biogenous seafloor sediment Plankton shells at high magnification
Hydrogenous Sediments PSCI 131: The Ocean Floor: Seafloor Sediments • Dispersed throughout ocean and along shorelines • Chemical precipitation of minerals from seawater • Common examples • Manganese nodules • Calcium carbonate Manganese nodules in south Pacific, depth 15,000 feet
End of Chapter PSCI 131: The Ocean Floor