2.6 - Mass Movement And Weathering Flashcards
What is weathering
weathering is the breakdown of rock in its place of origin
Types of mechanical weathering
When rocks break down with no chemical changes
- Freeze thaw: water expands by 9% in volume when freezing which exerts a force within cracks and fissures, repeated expansion and contraction causes further crack until rock breaks apart
- Wetting and drying: happens in warmer climates where rocks rich in clay expand when they get wet and contract when they dry, this repeated process causes them to crack and break over time
- Salt crystallisation: happens when sea spray gets through cracks in rocks, when the water evaporates it leaves behind salt crystals, the growth of these crystals in cracks and pore spaces can exert a breaking force, the salt can also corrode rocks
- Exfoliation/onion skin: when rocks warm up during the day the rock expands, at night the rock cools and contracts, overtime this causes very thin layers of rock to flake off
Types of biological weathering
rocks break down due to organic activity
- Rock boring: many marine molluscs live on coastal rocks, scraping away at the rock surface to get food or boring a hole in the rock to make a home
- Plant roots: trees and plants roots grow into cracks and fissures forcing rocks apart
- Animals: dig burrows into the cliff breaking rocks
Types of chemical weathering
rocks break down due to a chemical reaction
- Carbonation: as rain is slightly acidic, it reacts with carbonate rocks such as limestone causing them to dissolve
- Oxidation: when iron minerals in the rock react with oxygen in the air causing t=rust and the breaking down the rock
- Solution: when other salt minerals in the rock are dissolved
- Hydrolysis: the break down of minerals to form new clay minerals due to the effects of water and dissolved carbon dioxide
What is mass movement
Mass movement is the downslope movement of material (rock and soil) under the force of gravity
Mass movement is classified based on: speed, water content and nature of material
What are the 4 types of mass movement
- Rock fall: a rapid from of mass movement, blocks can be dislodged by mechanical weathering or hydraulic action, undercutting leads to large falls
- Slide: blocks of rockslide down a dip slope towards the sea, a very low angle dip will prevent rockfalls
- Flow: saturated soil and rock debris lose their cohesion and flow downslope, heavy rainfall and high tides can contribute to this
- Slump: huge masses of material can slowly rotate downslope over periods from days to years, can occur along a curved surface
What is a rotational scar
- Curved, Un-weathered, Un-vegetated
- Forms as a result of rotational slumping
- The section that has detached is at the base of the cliff often with vegetation attached
What is a talus scree slope
- A talus scree slope is a fan-shaped mound of material, often having a concave profile
- Made of block-fall debris which has accumulated at the foot of a cliff
What is a terraced cliff profile
- The profile of the cliff is stepped
- This is the result of the lithology or fractures in the rock