Midterm Study Guide 6 Flashcards

Mass Wasting

1
Q

List three effects of water (e.g. via heavy rain) on mass wasting processes.

A

1) Water in permeable materials adds weight (mass)
2) Abundant water added to unconsolidated materials reduces their cohesiveness
3) Fluid pressures in earth materials reduces all normal stresses in those materials by the amount of the fluid pressure (the effective stress concept). Shear stresses are not affected.

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2
Q

What range of velocities are spanned by mass wasting processes in nature?

A

Creep (mm to cm/yr) to catastrophic (several hundred km/hr).

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3
Q

What is a toe and a head in the context of mass wasting?

A

toe = material pushed out at the base of the landslide; supports the landslide. Head = top of landslide that used to be part of the original ground surface.

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4
Q

List three effects determining the likelihood of a landslide.

A

water content, friction, pressure

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5
Q

What is anisotropy of strength?

A

When a certain material is stronger in a way rather than a different way

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6
Q

What role does friction play in the stability of a hill side?

A

Friction holds everything in place. It helps keep all the grains or sediment more intact. The less friction the more it is deemed to fail.

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7
Q

What is effective normal stress?

A

a force that keeps a collection of particles rigid. It normally applies to sand, soil or gravel. Example: If you pinch a stack of coins between your fingers, the stack stays together. If you then loosen the pressure between your fingers, the coin stack falls apart. Similarly, a pile of sand keeps from spreading out like a liquid because the weight of the sand keeps the grains stuck together in their current arrangement, mostly out of static friction. This weight and pressure is the effective stress

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8
Q

What is the relationship between force and stress?

A

Stress = Force/Area

Depending on what you are holding constant stress is the outcome of greater force or greater area

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9
Q

What role does erosion play in mass wasting?

A

shaping the landscape

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10
Q

What is the angle of repose?

A
  • The angle of repose is the steepest angle at
    which a pile of unconsolidated grains remains
    stable, and is controlled by the frictional
    contact between the grains. In general, for dry
    materials the angle of repose increases with
    increasing grain size.
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11
Q

What man-made or natural processes can affect the stability of an existing hill side negatively?

A

Cutting into the hillside to form a flat surface for houses or roads - creates a very steep vertical cliff that is highly unstable.

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12
Q

landslide

A

Landslide is any perceptible downslope movement of bedrock, regolith.

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13
Q

friction coefficient

A

Friction coefficient is the ratio of the frictional force to the force acting perpendicular to the two surfaces in contact

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14
Q

potential energy

A

the energy of an object or a system due to the position of the body or the arrangement of the particles of the system.

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15
Q

erosion

A

Erosion is the process by which soil and rock are removed from the Earth’s surface by exogenetic processes such as wind or water flow, and then transported and deposited in other locations.

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16
Q

effective normal stress

A

the force that keeps a collection of particles together.

17
Q

critical angle

A

Critical angle refers to the highest angle the light can possibly refract into or between objects without disappearing

18
Q

normal stress

A

Normal stress is the component perpendicular to each plane. Wants to hold rock together.

19
Q

rock fall

A

ice wedging often breaks rocks along joints, preparing them to loosen and fall away

20
Q

talus

A

Talus is a sloping mass of rock fragments at the foot of a cliff.

21
Q

fluid pressure

A

Fluid pressure is the pressure at some point within a fluid, such as water or air. reduces the normal stresses but doesn’t affect shear stresses. Once normal stress is gone, it’s more likely that things will slide.

22
Q

angle of repose

A

Angle of repose is the steepest angle at which a sloping surface formed of a particular loose material is stable.

23
Q

shear stress

A

Shear stress is defined as a stress which is applied parallel or tangential to a face of a material, as opposed to a normal stress which is applied perpendicularly. Wants to break rock apart.

24
Q

creep

A

a. Creep is the gradual downward movement of
disintegrated rock or soil due to gravitational
forces.

b. Two types of creep
i. Seasonal creep: movement of soil by heave
caused by expansion and contraction of soil,
wetting and drying , freeze thaw from
weather change (operates in upper few feet
of soil
ii. Continuous creep: strain reponse to stress
generated by weight of overburden driven
by gravity alone, not heave which may
affect consolidated rock ( function at levels
well below the surface)

*(hopefully this helps clarify the difference between all the slides, flows, etc.)

25
Q

Avalanche (flow)

A

flows downhill after eq loosens large masses – flows down on air (which acts as the fluid).

26
Q

Fall

A

rocks broken along joints and they free fall as individual blocks (rock fall). A vertical drop.

27
Q

Slide

A
  • jointed bedrock layers broken along joints and
    move downhill as a unit (rock slide).
    • Slump – a mass slides down as a unit for a
      short distance fastly then stops,
      leads to a scar.
      - Debris soil – rock/soil/surface features like
      trees move as units downward. Key
      to slide – moving as unit.
28
Q

Flow

A
  • Rain soaked stuff flows. Soil (earth flow) or a
    mixture of rock/mud/debris (debris flow).
         - Lahar – water and lava.