Sediments Flashcards

(55 cards)

1
Q

what are marine sediments formed from

A

from weathered rock which gets transported to ocean by air/water

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2
Q

is erosion/deposition equal

A

no because of plate tectonics, sediments squeezed at subduction zones mountains eroded into sea

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3
Q

how to classify sediments

A

grain size

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4
Q

what is mud

A

silt and clay, fine

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5
Q

what are most common sediments in sea

A

mud/sand

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6
Q

what does grain size/sorting show

A

how it was transported/deposited

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7
Q

textural maturity

A

particles round overtime, sorting increases

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8
Q

factors controlling deposition

A

energy of transport, material, size

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9
Q

slow eroded rock

A

small/fine grain, well sorted, mature, mud/clay separated

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10
Q

fast eroded rock

A

high energy, large grains, not well sorted, gravel/sand mixed

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11
Q

high energy conditions

A

fine grains suspended, large grains roll, large grains deposited

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12
Q

low energy conditions

A

large grains too heavy to suspend, fine grain deposited

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13
Q

the larger the particle…

A

the larger the velocity needed to move it

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14
Q

why does clay need more energy then sand

A

clay sticks together so needs more energy to break apart

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15
Q

terrigenous/lithogenic

A

produced from weathered rocks, reflects composition of rocks where it was eroded, then gets transported by air/wind/ice

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16
Q

biogenous

A

produced from hard shells of organisms, macroscopic (bones), microscopic (shells, small)

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17
Q

hydrogenous

A

precipitated from water near seafloor, manganese nodules

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18
Q

volcanogenic

A

ejected from volcanoes

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19
Q

cosmogenic

A

from space

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20
Q

where is most terrigenous/lithogenic sediment found

A

continental margins

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21
Q

what does biogenic sediments do

A

settle on ocean and rains down ocean

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22
Q

biogenic ooze

A

when biogenic sediment clumps together and forms ooze (organisms dissolve), 30% is ooze, rest is mud

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23
Q

what happens after an organism dies

A

it sinks to floor and forms fecal pellat

24
Q

calcareous ooze

A

CaCO3, foraminifer, coccolithophores

25
silicious ooze
high productivity areas, diatoms, accumulates past CCD
26
deep ocean and CaCO3
its undersaturated with CaCO3, not enough calcium to combine with carbonate
27
calcite compensation depth
depth where CaCO3 dissolves so there's none on seafloor
28
carbonate dissolution depends on...
temperature/pressure, rate of carbonate supply, acidity
29
lysocline
depth where CaCO3 declines rapidly
30
factors controlling distribution
productivity, dissolution, dilution
31
ferromanganese nodules
lumps of metal oxides that have precipitated around a nuclei, metals come from weathering of rock
32
phosphorites
needed for growth of organisms, high productive areas
33
evaporites
formed when water evaporates, minerals
34
metal sulfides
iron/nickel, hydrothermal vents
35
as you approach a continent there's more...
terrigenous sediment
36
sources of deep sea sediment
terrigenous/biogenous
37
bulk emplacement
large amount of sediment transported (not grains), moved due to gravity, sediment build up causes instability/slope failure
38
slump
sediment piles slides downslope
39
mud flows (slurries)
mud/sediment mixed with water
40
turbidity currents
transport sediments to deep sea
41
pelagic sediment
fine terrigenous/biogenic sediment settled at bottom of ocean
42
inorganic
red clay
43
organic
oozes
44
continental shelf
flat plane of land underwater, where land meets sea
45
what is shelf sedimentation controlled by
tides/waves/currents
46
what happens to energy as depth increases
it decreases
47
what does shoreline turbulence do
prevents small particles from settling
48
where is calcareous ooze
tropics
49
where is sand/mud
temperate
50
subduction zones
squeeze sediment, creates prism
51
ice rafting
bulk emplacement of terrigenous sediment, large ice fragments broken off glaciers
52
as seafloor spreads...
ooze accumulates at top of ridge and gets buried/lithified and turns into limestone, as plate spreads it goes past CCD and ooze dissolves, pelagic mud forms and buries limestone protecting older limestone
53
as continents move apart...
sediments fill gaps as plates move, terrigenous sediment eroded by continent accumulates on shelf causing it to widen, sediment weighs continent down/sinks so sediment can be deposited
54
Atlantic margins
build up of sediment balances out subsidence, as plate sinks it has enough room for sediment build up
55
pacific margins
same as subduction zones