Week 9 Flashcards
1
Q
What is a landslide
A
- a slide of land
- the movement of a mass of rock, debris, or earth and/or mud down a slope
- rocks can slide or roll downhill: rockfall
- may occur when large volume of material moves downslope quickly: rotational/translational landslides
- may be wet: debris flows
- may occur gradually: creep
2
Q
Rotational slides
A
- move downward and outward above curved slip surface, with movement rotational about an axis parallel to slope
- head moves downward and rotates backward
- toe moves upward on top of landscape
- move short distance
3
Q
Translational slides
A
- move on planar slip surface such as fault, joint, clay rich layer
- move as long as on downward-inclined surface, and driving mass exists
- Underlying material fails so overlying material slides
- different behaviors:
1. remain coherent as block
2. deform and disintegrate to form debris slide
4
Q
Forces on a slope
A
- driving force: gravity pulls down on material
- external forces contribute, e.g earthquakes, eruptions - Resisting force: holds material in place
- strength of material and amount of friction
- Factors contributing to slope failure: slope steepness, material weight, moisture content
5
Q
Slope and load
A
- relationship between slope angle and load is a key factor in slope failure
- steeper slope - greater driving force - greater likelihood of slope failure
- angle of repose: steepest angle at which any loose material is stable
- depends on angularity and size of grains and moisture content
6
Q
Driving vs Resisting force
A
- frictional resistance depends on:
1. slope angle
2. Load - a critical mass
3. cohesion
7
Q
Source of weakness for planar internal surfaces
A
- layers in sedimentary rock
- fractures in any kind of rock
- contact between rocks of different strength
- faults, or slip surfaces of old landslides
8
Q
Cohesion adding to frictional resistance
A
- important force for holding soil grains together
- due to surface tension of water ( or other glue material) between loose grains
- cohesion is overcome when driving force is large enough
9
Q
role of water
A
- small amounts of moisture can stick together, increasing angle of repose
- effective frictional strength of rocks decreased by water
- decrease cohesion
10
Q
Slope changes due to external factors
A
- stream or wave action
- loading upper slope by construction
- removing vegetation
11
Q
Impact of rockfall
A
- very fast: 1 m/s to 100 m/s
- short runout
- patchy impact
12
Q
Impact of debris flow
A
- fast: 1 cm/s to 10 m/s
- long runout
- impact through burial, boulders and dynamic forces
- level of impact related to sediment concentration, debris content, velocity and depth
13
Q
Impact of Rot./ tran landslide
A
- fast: 1 cm/s to 10 m/s
- long runout
- complete impact through burial, boulders, and dynamic forces
- can transform into debris avalanche
14
Q
Impact of Creep
A
- slow: 0.3mm/yr to 3.1cm/yr
- short runout
- damage to brittle structures through ground movement
15
Q
Mitigation
A
- a lot of monitoring comes from the mining industry
- remote sensing
- adding materials to base of slope to reinforce weak layers (heavy boulders)
- removing materials from top of slope to reduce weight
- building suspension roads, instead of on the slope
- planting vegetation