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1582498
KQ1: Causes of Landforms
Description
see http://geographyfieldwork.com/GeographyVocabularyGCSECoasts.htm for geog definitions
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physical geography
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sophie.c.cook
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sophie.c.cook
over 10 years ago
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Resource summary
KQ1: Causes of Landforms
Effectiveness of coastal processes
Geology (rock type and structure)
Aspect
Direction of coast in relation to waves
Sea level change
250m higher than 10,000 years ago
Time
Human Activity
Weathering Processes
Salt crystallisation
When sea water enters cracks in the rock and then dries, leaving behind salt growths which prise the cracks apart
Wetting and drying
When rocks are periodically wetted and dried, clay minerals expand causing rocks to break up
Frost shattering
When water enters cracks and freezes, it expands, shattering rocks or expanding cracks
Heating and Cooling (insulation weathering)
Thermal expansion and contraction of rocks (usually the face) can cause onion skin weathering, as a layer of rock will be eroded and another exposed
Oxidation
CO2 gas in the atmosphere reacts with rain water making it acidic, and the solution removes Al and Fe from the rocks, leading to disaggregation
Chelation
The decay of organic matter causes acid to enter rocks, wearing it away
Mass Movements
Slides
Saturated weathered material moving down a slope under the influence of gravity
Falls
Dislodged material falls to the base of cliff, usually caused by undercutting
Slumps
Involves a whole segment of the cliff moving down-slope along a saturated shear-plane
Flows
When extremely saturated mud flows down a cliff
Creeps
The gradual downhill movement, under the force of gravity, of soil and loose rock material on a slope
Marine Processes
Erosion Processes
Hydraulic Action
Abraision
Corrosion
Attrition
Transport Processes
Swash
Body of water pushing up a beach after a wave has broken
Backwash
The movement of water back down a beach after it has reached its highest point
Geology
Lithology
Limestone
Cemented and strong
Sandstone
Resistant but weak if poorly cemented
Clay/Mudstone
Weak, easily saturated and eroded
Granite
Resistant due to interlocking crystals
Boulder Clay
Mixture of grain sizes, weak
Structure
Bedding planes, joins and faults
Allow water to enter rock and expose more cliff face to sub-aerial processes
Poorly cemented (porous)
More succeptable to weathering due to permeability
Plan-form
Discordant coasts expose more rock to weathering than concordant coasts
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