Geology 101 Quiz 10 Flashcards

1
Q

mass wasting

A

large-scale movement of rock or sediment down slope

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2
Q

the terminology for mass wasting events is based on three criteria

A

nature of motion, material, speed

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3
Q

natures of motion as they apply to mass wasting events

A

fall (freefall)
slide (mass stays intact and moves down-slope as a unit)
flow (mass moves a fluid)

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4
Q

materials as they apply to mass wasting events

A

rock, unconsolidated material (non-lithified sediment)

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5
Q

speed as it applies to mass wasting events

A

slow (creep and solifluction)
moderate (slides, slumps, and flows)
fast (falls and avalanches)

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6
Q

creep

A

slow, uniform movement of soil

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7
Q

solifluction

A

creep of saturated soil over permafrost

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8
Q

permafrost

A

ground that remains frozen all year

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9
Q

how does solifluction occur

A

melting ice and snow during the summer saturates the soil on top of the permafrost; the saturated soil slowly flows down the slope forming rounded lobes

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10
Q

slump

A

slow or fast displacement of block

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11
Q

slide

A

movement of block parallel to surface (most common where thin rock layers are sloped and eroded)

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12
Q

flow

A

fast; debris becomes fluidized by water or air

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13
Q

fall/avalanche

A

free falling from cliff (fall) or bounding down steep slope (avalanche)

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14
Q

influences on slope stability

A

steepness of slope, composition, vegetation, water content,

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15
Q

steeper slopes are (less/more) stable

A

less

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16
Q

consolidated material is (less/more) stable

A

more

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17
Q

physical and chemical weathering weaken rock making is (less/more) stable

18
Q

(smaller/larger) particles make LESS stable slopes

19
Q

(rounded/angular) particles make LESS stable slopes

20
Q

angle of repose

A

the maximum slope angle unconsolidated material can maintain

21
Q

a stack of marbles will have a ? angle of repose

22
Q

a stack of angular fragments will have a ? angle of repose

23
Q

fine sand has a (lower/higher) angle of repose than coarse sand

24
Q

vegetation generally (decreases/increases) slope stability and why?

A

increases; a network of roots through the soil

25
exceptions to vegetation increasing slope stability
root action that increases weathering, and heavy trees adding weight to an already weak overhang
26
increasing the water content generally (decreases/increases) slope stability, but not always
decreases
27
a small amount of water causes particles to adhere to each other due to surface tension, resulting in
a higher angle of repose
28
excess water eliminates air spaces resulting in loss of surface tension and reduces friction between particles; thus, the angle of respose is
much lower
29
heavy rains or raising the water level in a reservoir can ?; caves are an exception
destabilize weakened rock slopes
30
caves are (less/more) stable when completely filled with water and why?
more; the water helps support the roof
31
a cave with a thin or weak roof may collapse when
the water level drops below the top of the cave
32
flooding
mass wasting causing flooding, and flooding causing mass wasting
33
examples of mass wasting causing flooding
Gros Ventre River, Wyoming, 1925; Vaiont Dam, Italy, 1963
34
liquefaction
liquefying saturated sediments by vibration (vibration is typically achieved by earthquakes)
35
? and ? are the most commonly susceptible to liquefaction during earthquakes
sands and silts
36
examples of liquefaction
1964 large earthquake in Alaska caused it in Alaska and Japan; 2004 earthquake in Japan
37
quick clay
unstable clay that can suddenly liquefy and flow
38
quick clay is formed when
marine clay with a high salt content is uplifted and leached by freshwater
39
example of quick clay
Rissa, Norway: a farmer dug a pit to extend a barn and placed the removed sediment near the edge of a lake, causing underlying clay to suddenly give way and flow like water into the lake; Canada over 250 known slides have been attributed to quick clays (one in 1908 in Quebec killed 33)
40
most quick clays are found in
northern countries once covered with continental glaciers