Features of the Ocean Floor Flashcards
bathymetry def
measurement of ocean depths and charting of the shape of the ocean floor
abyssal plains
deep flat features that are occasionally interuppted by seamounts, that have thick accumulations of sediment that bury rugged floor
what are 3 things that abyssal plains consist of
1) fine sediments from currents
2) precipitated mineral matter
3) shells and skeletons
what ocean has the most abyssal plains and why
atlantic bc it has so few trenches
Seamounts
submarine volcaanoes that can become oceanic islands but most don’t have enough eruptive history
where ocean has the most seamounts
pacific
where can seamounts form over
hot spots
volcanic island
volcano that grows large enough before it’s carried from its magma source by plate motion
examples of volcanic islands
easter island, tahiti
guyots
submereged, flat topped seamounts
how do guyots form
inactive volcanic islands are lowered to sea level by weathering and erosion and are moved away from ridge or hot spot where they formed and sink
oceanic plateaus
composed of thick accumulations of pillow basalts and other mafic rocks
how do oceanic plateaus form
bulbous heat of a ring mantle plume melts and produces outpourung of basaltic lavaaa
mid ocean ridges
ridges that run throught the middle of an ocean basin
rise
spreading rate
distance from center of ocean
ridges far from the center of fthe ocean (flatter and faster spreaading rate)
slab pull
subduuction of cold dense slabs of coeanic lithosphere which are more dense than thee underluying warm asthenosphere due to gravity
ridge push
gravity driven force that results from the elevated position of ridge, causing slabs of lithosphere dto slide ddown ridge
what contributes more to plate motion? ridge push or slab pull
slab pull
What are features of convection
flow-upwelling of hot rock and mantle plummes (up flow) and cool lithopheric plates sink (drive downward moving flow)
transports heat away from interior to surface to space
whole-mantle convection aka
plume model
whole mantle convection
cold oceanic lithosphere sinks and stirs eentire mantle and ultimate burial ground for lithosphere is core. Balancedd by mantle plumes of hot mantle rock to ssurface.
whole mantle convection plumes
mantle plume is narrow and tube like from coree-mantle noundary
large mega plumes
layer cake model
two zones of convection: thin dynamic layer in upper mantle and thick, large sluggishh one in lower mantle and drives heat up
leyer cake model oceanic lithosphere
drives downward convective flow but doesn’t reach depths of no more than 1000 km