Mass Movements Flashcards
Free fall
- Material detaches from a slope and then free falls through the air, or bounces and rolls downslope
Slide
- Material (either rock or regality) that slides along a surface of rupture
Flow
Continuous movement of rock, regolith, or both that behaves as a high viscosity liquid
Rock falls are…
extremely rapid
Debris/earth falls are..
Rapid to extremely rapid
Rock slides are…
Very slow to extremely rapid
Debris/earth slides are…
Very slow to very rapid
Rock slumps are…
Extremely slow to moderate
Debris/earth slumps are…
Very slow to very rapid
Distinguishing the speed of motion:
- Slow (cree
What factors make up the criteria for the classification scheme or mass movements?
- 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)
Creep
Is slow and only detected by dislocation or bending of features at the surface
Debris Avalanches:
Are very rapid flows of rock, regolith, vegetation and/or sometimes ice
Flow
Are the continuous movements of rock, regolith, or both which behaves like a high viscosity liquid. Flow occurs on different scales
Rock creep:
Is extremely slow to slow (slow flows)
Debris/earth creep:
Is extremely slow to slow
Debris/earth flow:
Is very rapid
Debris avalanche (rock and regolith):
Is very rapid to extremely rapid
When are rock falls common?
They are common where rock is highly jointed and on a steep slope
Talus
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
Planar slides:
Move downslope in contact with a surface of rupture, typically along bedding planes, foliation, or joint planes oriented parallel to the slope
Slump:
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
What forces AFFECT slope stability?
- Gravity force
- Friction
- Cohesion
Gravity force:
In order for motion to happen, the gravity force parallel to the surface must be greater than the resisting strength
Friction
What increases friction?
More roughness = more friction
Cohesion
Is the attraction of particles at the atomic level
What has little cohesion?
Loose sand and gravel
What factors DETERMINE slope stability
Angle of repose
Vegetation
Angle of repose
The maximum angle of stability at which no movement occurs as determined by the friction, cohesion, and particle shape
Vegetation
Is very important as roots penetrate and bind together regolith and absorbs water from precipitation
Arid Climates
Have low vegetation abundance and slow rates of weathering and surface water removes most regolith particles very quickly as they loosen from bedrock
Angle of sliding friction
The angle at which the particles start to slide