Geomorphical Processes 3.1.3.2 Flashcards

1
Q

Types of mass movement

A

-soil creep
-mudflows
-landslides
-rockfall
-landslip/slump
-runoff
-solifluction

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2
Q

Soil creep

A

-soil particles on a hillside get wet after rainfall
-rainfall lubricates the particles making them heavier and making them have less friction
-they slowly move downslope causing trees to bend
-slowest form of mass movement

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3
Q

Evidence of soil creep

A

Terracettes

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4
Q

Mudflows

A

-earth and mud are on a hill slope
-rainfall fills pores in the soil which increases pressure- lubricant
-mud particles are heavier due to them being wet
-sediment flows downhill and mixes together in a rapid and dangerous mudflow
-forms a lobe of mud

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5
Q

Landslide

A

-rock moves along a plane
-rainfall occurs and lubricates the land surface reducing friction
-solid blocks of material slide rapidly down the hill
-triggered by earthquakes

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6
Q

Rockfall

A

-Rocks (often resistant ones) are on a steep and vertical cliff face
-mechanical weathering such as freeze thaw repeatedly occur overtime
-large blocks of rock break away and collect as scree
-scree is a temporary store of sediment becoming an input into sediment cells

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7
Q

Land slip / slump

A

-material is in a curved surface often permeable rock overlies impermeable rock
-rainfall occurs and can percolate through permeable rock but not the impermeable so a layer of water forms causing pressure
-saturated layer of material moves/slumps downhill

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8
Q

Runoff

A

-surface runoff/overland flow occur following a rainfall event
-smaller particles flow downslope within the overland flow to the littoral zone

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9
Q

Solifluction

A

-same as soil creep in colder environments
-frozen soil thaws in summer and becomes saturated
-saturated layer creeps down full over layer of permafrost

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10
Q

What are geomorphical processes?

A

Processes causing change to the landscape including subaerial and marine processes

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11
Q

Sub aerial processes

A

Weathering
Mass movement

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12
Q

Erosional processes

A

-hydraulic action
-wave quarrying
-corrosion
-abrasion
-solution
-attrition

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13
Q

Hydraulic action

A

-caused by the sheer force of water crashing against the coastline
-the water traps and compresses air in joints and cracks in the cliff
-waves retreat, air expands
-overtime this weakens the cliff and pieces break off
-any bubbles in the water may implode due to high pressure further eroding rock

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14
Q

Wave quarrying

A

-destructive waves break against unconsolidated material
-they then scoop loose material away

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15
Q

Corrasion

A

-sand and pebbles are picked up from seabed by waves advancing towards the coast
-transported material is thrown at the cliffs chipping away rock
-energy of the waves and size/shape of sediment determines how much erosion occurs

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16
Q

Abrasion

A

-abrasion involves picking up sediment from the seabed as it advances towards the coast
-transported material is dragged across the shoreline smoothing rocky surfaces in a ‘sandpapering’ effect
-contributes towards formation of wave-cut platform

17
Q

Solution

A

-weak acids in sea water dissolve alkaline rocks (chalks/limestone)
-alkaline cement bonds rocks together
-overtime rocks crumble and sediment is washed away

18
Q

Attrition

A

-gradual wearing down of rocks due to impact of abrasion and the impact of them bashing together when moved by waves/currents/tides
-overtime the rocks become smaller, smoother and more rounded

19
Q

Factors affecting the amount of erosion

A

Geology
Type of coastline
Presence/absence of beach
Wave energy