3.4 Weathering, Mass Movement and Runoff Flashcards
What is weathering?
The breakdown / disintegration of rock in situ at the ground surface.
Outline weathering as a positive feedback loop.
If the rate of debris removal exceeds the rate of weathering and mass movement, a positive feedback may operate - as the rate of weathering and mass movement could increase
Outline weathering as a negative feedback loop.
If debris removal is slow and ineffective, this will lead to a build up of an apron of debris that reduces the exposure of the cliff face as it extends up the cliff face.
Weathering and mass movement rates will decrease.
What are the 3 different types of weathering?
Mechanical
Biological
Chemical
Outline the 3 types of mechanical (physical) weathering.
- FREEZE THAW. Water enters a crack in the rock when it rains, and then freezes in the cold weather. When water freezes, it expands by 11%, exerting pressure on the rock, forcing the crack to widen. With repeated freezing and thawing, fragments of rock break away and collect at the bottom of the cliff as scree.
- WETTING ABD DRYING. Frequent cycles of wetting and drying are common at the coast. Rocks rich in clay (eg shale) expand when wet and contract when dry - causing the, to crack and break up.
- SALT CRYSTALLISATION. When sand water evaporates, it leaves salt crystals behind. These can grow over time and exert stresses in the rock, causing it to break up. Salt can also corrode rock, esp if it contains traces of iron.
Define mechanical weathering.
The break up of rocks without any chemical changes taking place.
Define biological weathering.
The breakdown of rocks by organic activity.
Outline the 3 different ways biological weathering can break down at the coast.
- thin plant roots grow into small cracks in a cliff face. These crack widen as the roots grow, breaking up the rock.
- birds and animals dig burrows into a cliff.
- water running through decaying vegetation becomes acidic, which leads to increased chemical weathering.
Define chemical weathering.
Chemical weathering involves a chemical reaction where salts may be dissolved, or a clay-like deposit may result which is easily eroded.
Outline the 3 different types of chemical weathering.
- CARBONATION. Rainwater absorbs CO2 from the air to form a weak carbonic acid. This reacts with calcium carbonate in rocks to form calcium bicarbonate, which is easily dissolved.
The cooler the temp of the rainwater, the more CO2 is absorbed. - OXIDATION. The reaction of rock minerals with oxygen, eg iron, to form a rusty red powder, leaving rocks more vulnerable to weathering.
- SOLUTION. The dissolving of rock minerals eg halite.
Define mass movement.
The downhill liege,not of material under the influence of gravity.
Give an example of a slow mass movement.
Soil creep.
Give an example of fast mass movement.
Rockfalls, landslides.
Outline the 7 types of mass movement.
- soil creep
- landslide
- mudflow
- rockfall
- runoff
- slump
- solifluction
Outline the mass movement: soil creep.
Soil creep is the extremely slow form of movement of individual soil partials downhill.
Particles rise towards the ground surface due to wetting of freezing and then return vertically to the surface in response to gravity as the soil dried out.