Geomorphical Processes 3.1.3.2 Flashcards
Types of mass movement
-soil creep
-mudflows
-landslides
-rockfall
-landslip/slump
-runoff
-solifluction
Soil creep
-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
Evidence of soil creep
Terracettes
Mudflows
-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
Landslide
-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
Rockfall
-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
Land slip / slump
-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
Runoff
-surface runoff/overland flow occur following a rainfall event
-smaller particles flow downslope within the overland flow to the littoral zone
Solifluction
-same as soil creep in colder environments
-frozen soil thaws in summer and becomes saturated
-saturated layer creeps down full over layer of permafrost
What are geomorphical processes?
Processes causing change to the landscape including subaerial and marine processes
Sub aerial processes
Weathering
Mass movement
Erosional processes
-hydraulic action
-wave quarrying
-corrosion
-abrasion
-solution
-attrition
Hydraulic action
-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
Wave quarrying
-destructive waves break against unconsolidated material
-they then scoop loose material away
Corrasion
-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
Abrasion
-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
Solution
-weak acids in sea water dissolve alkaline rocks (chalks/limestone)
-alkaline cement bonds rocks together
-overtime rocks crumble and sediment is washed away
Attrition
-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
Factors affecting the amount of erosion
Geology
Type of coastline
Presence/absence of beach
Wave energy