Ch. 2.3 Flashcards
(47 cards)
continental margins
boundaries between continental and oceanic crust. Shallow and close to shore
continental shelf
portion of a continent that is submerged under an area of relatively shallow water, known as a shelf sea
Submarine Canyons
narrow steep sided valleys that cut into continental slopes and continental rises of the ocean.
Formed by turbidity currents
shelf break
steepening of the bottom that marks the seaward limit of the continental shelf which begins the continental slope.
continental slope
closest to the exact edge of the continent. Begins at shelf break and descends to deep sea-floor
continental rise
closest to the exact edge of the continent. Begins at shelf break and descends to deep sea floor.
continental rise
sediment moving down a submarine canyon accumilates at the canyon’s base in a deposit called a deep sea fan.
deep ocean basin
deep water area, further from land
turbidity currents
a rapid downhill flow of water caused by increased density due to high amounts of sediment
underwater avalanche of sediment
mid ocean ridges
shallow waters close to the middle of deep ocean basins
Why is the Southern Hemisphere referred to as the water hemisphere?
80% of the Southern Hemisphere is ocean as compared to only 61% of the Northern Hemisphere is earth.
Active Margin
zone where tectonic plates either converge with or shear past one another
-subduction and volcanic activity occurs
-think of the cliffs on the coast
Passive Margin
transition between oceanic and continental lithosphere that is not an active plate margin
-adjacent to where seafloor spreading occurs
-flat long coasts
trenches
formed by subduction of a tectonic plate
- parallel to margin
-located on deep ocean floor
Abyssal plains
flat region of ocean floor usually at base of continental rise; slope of less that 1 degree toward mid ocean ridge
abyssal hills
small submarine hills
seamounts
a submarine mountain
guyots
seamount with flat top used to be islands that sunk below the sea cause of island weight
central rift valley
center of ridge system divergent boundary with magma rising up through the oceanic crust
hydrothermal vents
result of seawater percolating down through fissures in the ocean crust in the vicinity of spreading centers or subduction zones the cold sea water is heated by magma and reemerges to form the vents
black smokers
solidified minerals in the water that build up around the vents forming chimney-like structures.
mantle plume
stationary channel of magma usually far from any plate boundary that rises towards the surface from deep within the mantle
hotspot
area of volcanic activity due to the mantle plume
Why are hotspots and mantel plumes considered an intraplate feature
they tend to be far from plate boundaries