Origin of the Oceans Flashcards
tectonic plate (24 cards)
the earth surface can move in three ways?
1) Divergent Motion: When two tectonic plates
move apart from one another.
2) Convergent Motion: When two tectonic plates
move toward one another.
3) Transform or ‘strike slip’ Motion: When two
tectonic plates slide past one another at an angle.
mid Atlantic ridge
east pacific rise
convergent ocean to continental
Subducting Nazca plate
The process of tectonic subduction occurs
when two tectonic plates convergent together.
Continental Crust
Continental crust is made of lower density
minerals.
Continental crust is thick (60-100 km)
Continental crust is very old
New continental crust is very rare
Oceanic Crust
Oceanic crust is made of higher density
minerals
Oceanic crust is rather young in age
Oceanic crust is thin (7-10 km)
Types of Continental Margins
PassivePassive
Not on plate boundaries
Lack active volcanoes & earthquakes
Active Type
On plate boundaries
Active volcanoes & earthquakesActive volcanoes
Features of Passive,Continental Margins
Continental Shelf
Continental Slope
Continental Rise
Features of the Continental Shelf
Average Depth = 133 Meters (440 ft)
Maximum Depth= 200 meters (660 ft)
Average width == 78 km (50 mi)
Range of Width == 0 to 1500 km (950mi)
Sea ward slope == 0.1 degree
Amount above sea level can vary greatly
Continental Margins are good
sediment traps sediments
collect there?
Lithogenous , Gravel, sand, silt, clay
Biogenous, Shells, bone, teeth, droppings
Hydrogenous,Chemical precipitates - lime, salt, sulfides
Active ContinentalMargins,Associated with Divergent Plate Boundaries
Young narrow seas with continental slopes
and shelves (example = Red Sea)
Become passive continental margins as sea
floor spreading continues.
Active ContinentalMargins,Associated with Transform Boundaries
1,Continental Borderlands
2,Alternating up-thrown and down-dropped fault blocks.
3, Often expressed as islands and basin.
Active Continental Margins.
Associated with Convergent Boundaries.
Deep Ocean Trenches.
Island Arcs
Subduction Zones
Active continental mountain ranges
Island Arcs
Arcuate chains of islands, separated from continents by a marginal sea
Ocean Sediment Types
Lithogenous, Gravel, sand, silt, clay
Biogenous, Shells, bone, teeth, droppings
Ooze = sediment with over 30% biogenic material
Hydrogenous, Chemical precipitates - lime, salt, sulfides
Active Continental Margins
Associated with Divergent Plate Boundaries.
Young narrow seas with continental slopes and shelves (example = Red Sea)
-Become passive continental margins as sea floor spreading continues.
Active Continental Margins
Associated with Transform Boundaries
Continental Borderlands
Alternating up-thrown and down-dropped fault blocks.
Often expressed as islands and and basins.
Active Continental Margins
Associated with Convergent Boundaries
Deep Ocean Trenches
Island Arcs
Subduction Zones
Active continental mountain ranges
Examples,Trenches
Kurile Trench
Marianas Trench -Deepest - 11,035 meters
Aleutian Trench
Peru-Chile Trench - Longest - 5900km
Tonga- Kermadec Trench
Puerto RicoTrench
Deep Sea Sediments
Accumulate very slowly
Ø 1 to 15 millimeters per year
Ø (1/2 inch per year)
Abyssal Plains
Relatively flat floors of ocean basins
Ø Thin veneer of deep sea sediment
l Generally about 500 meters (1500 ft) thick
Basaltic oceanic crust underlies sediment
l Often pillow basalt lava
1 to 2 km thick
Lower crustal layer is gabbro plutons
3 to 6 km thick
Why Study Deep Sea Sediments
Climate change
Benthic habitats
Off-shore pollution
Sources of dredged material
Sources of off-shore minerals
Understand ocean floor topography
Understand Earth’s different
environments