Features of the Ocean Floor Flashcards

1
Q

bathymetry def

A

measurement of ocean depths and charting of the shape of the ocean floor

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2
Q

abyssal plains

A

deep flat features that are occasionally interuppted by seamounts, that have thick accumulations of sediment that bury rugged floor

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3
Q

what are 3 things that abyssal plains consist of

A

1) fine sediments from currents
2) precipitated mineral matter
3) shells and skeletons

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4
Q

what ocean has the most abyssal plains and why

A

atlantic bc it has so few trenches

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5
Q

Seamounts

A

submarine volcaanoes that can become oceanic islands but most don’t have enough eruptive history

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6
Q

where ocean has the most seamounts

A

pacific

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7
Q

where can seamounts form over

A

hot spots

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8
Q

volcanic island

A

volcano that grows large enough before it’s carried from its magma source by plate motion

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9
Q

examples of volcanic islands

A

easter island, tahiti

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10
Q

guyots

A

submereged, flat topped seamounts

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11
Q

how do guyots form

A

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

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12
Q

oceanic plateaus

A

composed of thick accumulations of pillow basalts and other mafic rocks

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13
Q

how do oceanic plateaus form

A

bulbous heat of a ring mantle plume melts and produces outpourung of basaltic lavaaa

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14
Q

mid ocean ridges

A

ridges that run throught the middle of an ocean basin

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15
Q

rise

spreading rate
distance from center of ocean

A

ridges far from the center of fthe ocean (flatter and faster spreaading rate)

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16
Q

slab pull

A

subduuction of cold dense slabs of coeanic lithosphere which are more dense than thee underluying warm asthenosphere due to gravity

17
Q

ridge push

A

gravity driven force that results from the elevated position of ridge, causing slabs of lithosphere dto slide ddown ridge

18
Q

what contributes more to plate motion? ridge push or slab pull

A

slab pull

19
Q

What are features of convection

A

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

20
Q

whole-mantle convection aka

A

plume model

21
Q

whole mantle convection

A

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.

22
Q

whole mantle convection plumes

A

mantle plume is narrow and tube like from coree-mantle noundary
large mega plumes

23
Q

layer cake model

A

two zones of convection: thin dynamic layer in upper mantle and thick, large sluggishh one in lower mantle and drives heat up

24
Q

leyer cake model oceanic lithosphere

A

drives downward convective flow but doesn’t reach depths of no more than 1000 km

25
Q

SOURCE OF Magma for volcanism away from plate boundaries cak model

A

melting of lithosphereic frangments