Stability of Slopes Flashcards
1
Q
How can slope stability dec?
A
- human activities: lead to mass movement events
2
Q
How can slope stability inc?
A
- humans can reinforce slope stability by dec. hazard to envi. + human life
3
Q
What is slope stability generally caused by?
A
- an inc. in external stress on slope
- a dec. in internal strength of a slope
4
Q
What are examples of human activities that cause a dec. in slope stability?
A
- mining + quarrying
- construction
- tourism
- agriculture
- forestry
5
Q
How does mining + quarrying dec. slope stability?
A
- removes lateral support from slope (undercutting)
- causes instability in slope: leads to mass movements - land/mud/rock slides or rockfalls
- brings large amounts of waste (often left on slope)
- inc. stress on slopes from weight: leads to mass movement
6
Q
How does construction dec. slope stability?
A
- stress is added (e.g. weight of housing or dams)
- may be undercut so can build: causes instability
- groundwater affected due to sewage + drainage systems + water demand: creates instability
- water erosion affects slopes internal strength. Hydraulic engineering (e.g. dams) causes saturation of surrounding slope if not properly managed: triggers mass movement, esp. mudslides
7
Q
How does tourism dec. slope stability?
A
- common on alpine slopes: skiing
- creates stress on slopes
- erosion of slopes inc. due to trampling of veg., skis, heavy machinery, walking: damages + compacts soil
- alpine areas: seasonal melting is common, dramatically inc. water + triggers mass movement when slope is degraded
8
Q
How does agri. dec. slope stability?
A
- soil compacted by heavy machinery + animals
- leaves slopes vulnerable to soil erosion, changing water flows + dec. veg. cover
- dec. veg. cover from overgrazing + trampling causes soil degradation
- veg. vital to soil’s structure, w/o veg. rates of soil erosion + weathering inc.: inc. risk of large scale mass movements (landslides)
9
Q
How does forestry dec. slope stability?
A
- deforestation:
- dec. soil strength which is enhanced by tree roots: majorly instable if not managed
- dec. interception of pptn: more overland flow + infiltration + less water uptake by roots - inc. soil saturation: erosion + triggers mass movements
- clearcutting leaves slopes vulnerable, esp. to winds
- forest roads constructed to transport timber: interrupts natural flow of water + creates channels for run-off: can be highly erosive