Mass Wasting Flashcards

1
Q

what is mass wasting?

A

downslope movement of rock or regolith (loose weathered materials + soil driven by force of gravity)

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2
Q

What should we care about mass wasting?

A

The cost of recovery from mass wasting (all forms combined) is more each year than earthquakes + volcanoes, tornadoes combined

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3
Q

What are the controls of mass wasting?

A

Properties of material involved (rigid, cohesive or loose)

Slope angle

Water content of material

Removal of vegetation

Mass movement triggers

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4
Q

what are the properties of material involved in mass wasting?

A

Rigid, brittle material (e.g. rock)

Soft, cohesive material (e.g. clay-rich soil or rock in which particles stick tgt + form a coherent mass)

Loose particles (e.g. gravel, sand, etc.)

Phys + chem weathering can further weaken geologic materials + make them prone to failure (esp in case of rock)

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5
Q

What is the angle of repose?

A

maximum angle that a given material will sustain

Diff in angle of repose according to grain size, grain shape (round vs angular) + water content

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6
Q

What is the slope angle?

A

Gravity has greater effect on potential downslope movement of material on steeper slopes

Increase the sloped, increase the driving force (mass wasting events tend to be most spectacular on steep mountain slopes)

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7
Q

What are the natural slopes prone to mass wasting?

A

River banks

Mountain slopes

Fault surfaces

Wave-cut shorelines

Glacial valleys

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8
Q

What are the Man-made slopes prone to mass wasting?

A

Road-cuts

Excavation projects

Gravel pits

Quarries

Drainage ditches

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9
Q

what can water do to particles

A

Presence of some water can increase cohesion of loose particles (due to surface tension)

But addition of lots of water can destabilize material

Many cases:

Water along fractures + btwn particles can act as a lubricant (Promoting blocks to slide)

Water can cause particles to remain separated + to move freely (Material behaves like fluid)

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10
Q

What can plants do for material?

A

Roots of plants anchor loose material such as soil in place on a slope

Removal of vegetation removes this stabilizing factor + can promote downslope movement

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11
Q

What can trigger mass movement?

A

vibrations , from shaking + liquefaction (lubrication of particles by invading water)

Weather events

Slightest added stress on a material can trigger mass movement

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12
Q

Types of mass wasting classified according to what 3 criteria?

A

type of movement
type of material moved
rate of movement (velocity)

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13
Q

what are the types of movement?

A

Falling (freefall)

Sliding (along planar or curved surface)

Flowing (material internally deforms like a fluid)

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14
Q

what are the types of material moved?

A

Brittle solid material (most rock)

Cohesive solid material (e.g. clay-rich soil or rock)

Loose particles (e.g. particles of soil, mud, debris of assorted sizes)

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15
Q

what are the rates of movement

A

rapid or slow

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16
Q

What is a rockslide?

A

Blocks of solid, brittle rock slide down a planar surface

Generally very fast + destructive

17
Q

what is a rock avalanche

A

After a mass of rock is dislodged (often in a rockslide), it can break into many smaller pieces + move downslope as a rock avalanche

Fragments of rock travel downslope on a cushion of air within + beneath the moving mass of rock fragments

18
Q

what is a slump

A

Material moves as coherent blocks along curved surfaces (little or no internal deformation within blocks)

Commonly occurs in cohesive clay-rich sedimentary rocks (e.g. shales) + soils (clay helps particles stick together)

At surface, slump scarps mark these curved surfaces of sliding

Rate of movement depends on material involved (but usually slow)

19
Q

what is an earthflow

A

When clay-rich soil becomes saturated w/ water, it behaves like a viscous fluid (deforming internally)

Commonly produced at the foot of a slump (where water is leaking from curved slump surface)

Typically move slowly, but can move quickly if lots of water has soaked into the material and/or the slope above is steep

20
Q

what is a debris flow

A

if assortment of surface materials, both fine- and coarse-grained

21
Q

what is a mudflow

A

if predominantly fine grained materials

22
Q

both debris flow + mudflow consist of what?

A

loose material mixed w/ large amt of water
- less viscous than earthflows + can move extremely quickly (extremely destructive)
- movement of this liquefied material is often confined to channels

23
Q

what are lahars

A

debris flows + mudflows specifically associated w/ volcanoes

24
Q

how are lahars formed

A

Formed when large amts of water (e.g. from heavy rainfall, or from melting snow at the summit of an active volcano) mixes w/ loose pyroclastic materials (e.g. ash) + flows downslope

25
Q

what is a creep

A

Expansion + contraction of surface material leads to very slow + gradual downhill movement of soil

Its effects can be observed in the tilting fences + headstones + curvature of tree trunks + damage to building foundations

Unspectacular but very costly

26
Q

what are the human influences on mass wasting

A

Natural Processes + increased population density + increased human activity = increased hazard potential

27
Q

list the human influence on mass wasting hazards

A

Weakening of slope material by saturation by water
-Enhanced due to land use changes such clear cutting + agriculture

Steepening of the slope by artificial or natural undercutting of toe of slope
-For buildings and roads

Addition of weight at top of slope
-Dams, buildings, urbanization, roads

Humans are sculpting the surface of Earth faster than natural processes – no slope is too rugged for development

28
Q

what are some strategies to reduce damage from slope movements

A

Grading (add material to reduce slope angle)

Surface + subsurface drainage control (devices to permit drainage of excess water from soil + underlying weathered rock)

Retaining walls, and slope supports (stabilize slope + support surfaces of potential weakness such as fault planes + rupture surfaces under potential slump blocks

Anchoring into bedrock (to reduce load + prevent slippage of man-made structures due to deformation of loose materials)