Mass Movements Flashcards

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1
Q

Free fall

A
  • Material detaches from a slope and then free falls through the air, or bounces and rolls downslope
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2
Q

Slide

A
  • Material (either rock or regality) that slides along a surface of rupture
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3
Q

Flow

A

Continuous movement of rock, regolith, or both that behaves as a high viscosity liquid

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4
Q

Rock falls are…

A

extremely rapid

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5
Q

Debris/earth falls are..

A

Rapid to extremely rapid

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6
Q

Rock slides are…

A

Very slow to extremely rapid

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7
Q

Debris/earth slides are…

A

Very slow to very rapid

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8
Q

Rock slumps are…

A

Extremely slow to moderate

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9
Q

Debris/earth slumps are…

A

Very slow to very rapid

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10
Q

Distinguishing the speed of motion:

A
  • Slow (cree
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11
Q

What factors make up the criteria for the classification scheme or mass movements?

A
  • Nature of the mixture of solids (rock, debris, or earth materials)
  • Type of motion (fall, slide or flow)
  • Velocity of motion (avalanche, flow, or creep)
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12
Q

Creep

A

Is slow and only detected by dislocation or bending of features at the surface

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13
Q

Debris Avalanches:

A

Are very rapid flows of rock, regolith, vegetation and/or sometimes ice

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14
Q

Flow

A

Are the continuous movements of rock, regolith, or both which behaves like a high viscosity liquid. Flow occurs on different scales

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15
Q

Rock creep:

A

Is extremely slow to slow (slow flows)

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16
Q

Debris/earth creep:

A

Is extremely slow to slow

17
Q

Debris/earth flow:

A

Is very rapid

18
Q

Debris avalanche (rock and regolith):

A

Is very rapid to extremely rapid

19
Q

When are rock falls common?

A

They are common where rock is highly jointed and on a steep slope

20
Q

Talus

A

Is the loose material that piles up at the base of steep slopes. Lack of vegetation/soil on talus indicates that material is actively accumulating

21
Q

Planar slides:

A

Move downslope in contact with a surface of rupture, typically along bedding planes, foliation, or joint planes oriented parallel to the slope

22
Q

Slump:

A

Is the curved rotational slide surfaces that are scoop shaped and usually form in regolith, poorly consolidated, or weak rock where bedding/joints do not influence failure

23
Q

What forces AFFECT slope stability?

A
  • Gravity force
  • Friction
  • Cohesion
24
Q

Gravity force:

A

In order for motion to happen, the gravity force parallel to the surface must be greater than the resisting strength

25
Q

Friction

A
26
Q

What increases friction?

A

More roughness = more friction

27
Q

Cohesion

A

Is the attraction of particles at the atomic level

28
Q

What has little cohesion?

A

Loose sand and gravel

29
Q

What factors DETERMINE slope stability

A

Angle of repose

Vegetation

30
Q

Angle of repose

A

The maximum angle of stability at which no movement occurs as determined by the friction, cohesion, and particle shape

31
Q

Vegetation

A

Is very important as roots penetrate and bind together regolith and absorbs water from precipitation

32
Q

Arid Climates

A

Have low vegetation abundance and slow rates of weathering and surface water removes most regolith particles very quickly as they loosen from bedrock

33
Q

Angle of sliding friction

A

The angle at which the particles start to slide