2.4. Mass movement Flashcards
1
Q
What is mass movement?
A
The downhill movement of material under the influence of gravity
2
Q
Where is mass movement common and why?
A
Common at the coast due to the weight of rainwater and weak geology
3
Q
What does the type of movement depend on?
A
- angle
- rock type
- vegetation
- how wet the ground is
4
Q
What are the 4 types of mass movement?
A
- creep
- flow
- slide
- fall
5
Q
What is soil creep?
A
- An extremely slow form of movement of individual soil particles downhill
- cannot be seen in operation but can be seen by the build up of soil on the upslope side of walls and the bending of tree trunks
6
Q
What are mudflows?
A
- involves earth and mud flowing downhill, usually over unconsolidated or weak bedrock, often after heavy rainfall
- mudflows are often sudden and fast flowing
- water gets trapped within rock which increased pore water pressure, forcing rock particles apart and leads to slope failure
7
Q
What are landslides?
A
- A landslide involves a block of rock moving very rapidly downhill along a planar surface
- landslides tend to be very rapid
- moving block in a landslide remains largely intact
- frequently triggered by earthquakes or heavy rainfall
8
Q
What is a rockfall?
A
- the sudden collapse or breaking away of individual rock fragment at a cliff face
- most commonly associated with steep or vertical cliffs in heavily jointed and quite resistant rock
- often triggered by mechanical weathering or earthquakes
- once broken away from source, rock falls or bounces down slope to from scree at foot
9
Q
What is a landslip or slump?
A
- differs from a landslide in that its slide surface is curved, rather than flat
- landslips or slumps are characterised by a sharp break of slope and formation of a scare
- often occur in weak, unconsolidated clays and sands
10
Q
What is run-off?
A
- occurs down a slope or cliff- face and small particles are moved down slope, forming input into sediment cell
- type of flow that transfers water and sediment from one store to another
11
Q
What is solifluction?
A
- similar to soil creep but specific to cold environments where temps fluctuate around freezing
- in summer, surface layer of soil thaws and becomes extremely saturated and it sits on top of impermeable permafrost
- known as active layer, sodden soil with blanket of vegetation slowly moved downhill by combination of heave and flow
12
Q
A