Surface Processes Flashcards
1
Q
mass wasting
A
downslope movement of rock and debris under the influence of gravity
2
Q
landslide
A
general term for all types of mass movement
3
Q
causes of slope failure
A
- contributing factors that make slope vulnerable to failure
- Main cause: gravity
- Others: slope angle, local relief, thickness of soil over bedrock, orientation of planes of weakness in bedrock, climatic factors (ie. Ice, water in soil, precipitation), vegetation
4
Q
triggers of slope failure
A
- single event that initiates movement
- Earthquakes
- Weight added to upper part of slope
- Undercutting bottom of slope
- Heavy rainfall
- Volcanic activity
- Human modification
5
Q
relationship between gravity and slope stability
A
- Understanding the materials involved and forces involved is key to predicting slope stability
- Shear stress < shear resistance = stable (frictional force on block is sufficient that it won’t fall -> Even with a high slope angle, with enough friction the slope may still be stable)
- Shear stress > shear resistance = unstable, will fall
- Shear stress < shear strength of solid -> stable (In unconsolidated materials like soil, we consider the strength of the material (shear strength))
6
Q
angle of repose
A
- Loose materials rest at a natural angle of repose, which is different depending on the material
- If angle > greater than their angle of repose -> unstable
7
Q
effect of rock structure on slope stability
A
- Parallel cracks/bedding/fractures on granite rocks are planes of weakness
- Low porosity rocks in a sequence can prevent groundwater from seeping away – another plane of weakness
8
Q
effect of water on slope stability
A
- Unsaturated soil or debris vs. Saturated soil or debris
- Surface tension is an important force – a little bit of water is okay, but if material is saturated, the grains are forced apart and the material flows
9
Q
how are slope features classified?
A
- Combines type of movement, rate of movement, type of material
- Slides, flows, falls
10
Q
slides
A
- Failure plane along a definite slip surface – mass stays intact
- Transactional (glide block)
- Rotational (slump)
11
Q
flows
A
- Material moves as viscous fluid
- Debris flows: earth or mud
- Debris avalanche
- Slump earth flow complex: In thick soils and soft sedimentary rocks; common for slump to break up into smaller blocks as it travels down slope and begin to flow
- Lahar: volcanic mud/debris flow
- Creep: a imperceptibly slow type of flow
12
Q
falls
A
- Mass falls through the air
- ex. Rock fall
13
Q
how do we decrease slope hazards?
A
- Identify unstable and potentially unstable slopes by geological mapping
- Legislate appropriate zoning laws and enforce them
- Control or stop existing landslides
- Design slopes or engineer structures to prevent new landslides
14
Q
techniques used to stabilize landslides
A
- Build retaining walls, sink piers into stable ground (need to remember to increase surface or subsurface drainage -> give water a way to drain freely out of walls otherwise pressure will build and it’ll collapse)
- Revegetate slopes (Hyrdoseeding, applying jute netting)
- Regrade slopes (cut problematic parts off)
- Cover slopes (Chicken wire “shotcrete”; rock bolts -> steel bolts anchored in cement to connect outer rock to a more stable layer in the middle)
- Contain/redirect the hazard (Ex. Avalanche sheds)