marine processes L8 Coasts Flashcards

1
Q

Weathering

A

the breakdown of rock in situ

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2
Q

mass movement

A

the downhill movement of material under the influence of gravity

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3
Q

flows (mass movement)

A

material is mixed together and is wet, acts like a complete fluid

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4
Q

slides (mass movement)

A

material remains intact and is just lubricated (not necessarily wet)

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5
Q

Landslides (mass movement)

A

flat slide area and tend to be in areas of more resistant geology

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6
Q

landslips (mass movement)

A

areas of weak geology with a curved slide area (rotational slip basically)

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7
Q

soil creep vs solifluction (mass movement)

A

Slow downhill movement of soil
Solifluction is specifically in periglacial environments

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8
Q

rockfalls (mass movement)

A

Collapse of rock fragments in regions of resistant rock

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9
Q

slumping

A

weak geology occurs on a curved surface where saturated soil can undergo liquefaction, (causing rotational slip)

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10
Q

Outline the processes of mass movement at the coast.

A

explain what mass movement is then give examples and explanations of how they work

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11
Q

marine process

A

operates on the coastline and are connected to actions of the sea
E.g. tides and waves

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12
Q

sub-aerial processes

A

operate on land but affect the shape of a coastline
E.g. weathering, mass movement and runoff

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13
Q

lithology

A

geological structure of rock

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14
Q

geology

A

the study of rocks
(Focus on the type of rock)

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15
Q

hydraulic action

A

waves force water into cracks, compressing the air and building up pressure, weakening rock over time

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16
Q

cavitation

A

when bubbles form and collapse violently due to pressure changes, weakening rock (linked to hydraulic action)

17
Q

wave quarrying

A

energy of waves coupled with hydraulic action breaks away fragments of rock from the coast

18
Q

corrasion

A

Waves throw sand and pebbles and larger rocks against cliffs, wearing them down like sandpaper

19
Q

abrasion

A

similar to corrasion, grinding and scraping effect of sediment carried by waves, resulting in smooth cliff faces

20
Q

difference between corrasion and abrasion

A

corrasion has the erosive impact
Abrasion is the smoothing process

21
Q

solution/corrosion (erosion)

A

seawater which is acidic due to dissolved CO2, reacts with certain rocks like limestone and chalk, dissolving them over time
Works with carbonation

22
Q

attrition

A

Rocks and pebbles smash against one another, becoming smaller and rounder, not eroding the coastline but still a process

23
Q

suspension

A

Finde sediment like sand and silt is carried within the water but not dissolved, making it cloudy

24
Q

traction

A

Large, heavy rocks and boulders are rolled and dragged along the seabed by strong currents and waves

25
saltation
smaller pebbles and sediment are bounced along the seabed when waves momentarily lift them above the seabed
26
solution (transportation)
dissolved minerals such as calcium carbonate from limestone is carried invisibly due to being subjected to acidic water
27
what is the solution in water of limestone
calcium carbonate
28
Longshore/Littoral Drift
transfer/flow mechanism responsible for moving sediment along the coastline and eventually out to sea Key component of the sediment cell
29
how does LSD work
swash acts on an angle similar to prevailing wind Backwash occur directly perpendicular to the beach under gravity
30
When does deposition occur
when the velocity of water falls below a critical value so that a particular size of particle can no longer be transported
31
why is sediment deposition important
Creates depositional landforms which are sinks Considered both inputs and outputs in coastal systems
32
what is a sediment sink
a store of sediment
33
example of a high energy coastal environment in the UK
the S coast of England Sand and clay are easily transported to leave behind heavier coarser pebble beaches
34
example of a low energy coastal environment
tiver estuaries where even the smallest clay particles drop to the seabed and form mudflats. Some sediment may be carried offshore as well to forom sandbanks