9.2: mass movement Flashcards
mass movement
mass movements are large scale movement of Earth’s surface not accompanied by a moving agent such as a river, glacier or ocean wave
weathering
the decomposition and disintegration of rocks in situ
aggradation
to build up a surface or soil through the addition of material such as mass wasting deposits
geology
the study of rocks
degradation
the wearing down of the land by the erosive action of water wind or ice
geological structure
the arrangements of rocks in the Earth’s crust: strata, bedding planes, joints etc
regolith
the layer of unconsolidated material covering the bedrock of a planet (soil)
aspect
the direction in which a slope faces
name three factors which can reduce shear strength
- water –> loss of grain to grain contact, reducing the cohesion of soil
- earthquakes and the movement of trees cause vibrational shock
- burrowing of animals and other biological weathering of roots
name three factors which can increase shear stress
- weathering processes such as freeze thaw, dilatation and hydration can increase stress through lateral pressure
- water –> increase in pore water pressure as well as adding to the weight of the slope
- increasing weight by adding vegetation or accumulation of debris eg slag heaps when mining
what are slumps
weaker rocks such as clays ‘slump’ with a rotational movement along a curved slip plane
explain the key characteristics of a slump
clay saturated with water and minerals expand. the lubrication of slip plane causes a series of material slumps, along curved slip plane. Commonly occurs if the base has been undercut. This can be gradual or sudden separate, jerky events. This can leave a crescent shape scar on the slope.
what is a flow
more continuous, smoother form of slump. Occurs in deeply weathered clay, and if particle size is the same or smaller than a grain of sand
define a mudflow
fine grains mixed with water, slowing down a channel. Accumulates material down the slope. Faster than earthflows (which are deeper and thicker)
define debris flow
loose mud, sand and soil saturated with water. Larger than mudflows, accumulating material as it travels. Its higher water content allows flows to occur on shallow slopes and can occur on saturated toes of a landslide or as a separate event. This can create a scar, flowtrack and toe lobe