Surface Processes Flashcards

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1
Q

mass wasting

A

downslope movement of rock and debris under the influence of gravity

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2
Q

landslide

A

general term for all types of mass movement

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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
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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
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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))
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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
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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
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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
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9
Q

how are slope features classified?

A
  • Combines type of movement, rate of movement, type of material
  • Slides, flows, falls
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10
Q

slides

A
  • Failure plane along a definite slip surface – mass stays intact
  • Transactional (glide block)
  • Rotational (slump)
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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
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12
Q

falls

A
  • Mass falls through the air

- ex. Rock fall

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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
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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)
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