MASS MOVEMENT Flashcards

1
Q

what is mass movement?

A

processes whereby masses of rock and soil move downhill under influence of gravity

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2
Q

types of mass movement

A

landslide, mudslide, rock avalanche

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3
Q

what causes it

A

arises from rock fragmentation through weathering and is a major geomorphological process on slopes (esp steep slopes) resulting in decline in slope angle over time

frequently a geohazard

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4
Q

ultimate controlling factor of mass movement

A

gravity

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5
Q

controlling factors of mass movement

A

nature of material
moisture content of material
slope angle

influenced by human characteristics

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6
Q

rock sitting stationary on top of slope

what would cause rock to move down slope? – trigger factors

A

increase weight
lubrication
increase slope angle

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7
Q

controlling factors:

explain nature of slope materials

A
  • materials vary according to geology - main division is between consolidated and unconsolidated material
  • unconsol material = has angle of repose
  • size and shape of particles are main determinants

cons material
-slope steepness can be maintained but instability is still possible -
- slope if undercut (over
steepened)
- vegetation cover is removed (clearing or fire)

deep weathering alters the rock by reducing binding forces and make slopes susceptible to movement/failure

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8
Q

angle of repose

A

maximum angle at which a slope of loose material lies without movement

slopes steeper than angle of repose are unstable

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9
Q

angle of repose - fine vs course particles

A

fine - shallower angle of rep

course - larger angle of rep

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10
Q

controlling factors: explain moisture content

A

saturation of material reduces internal friction and promotes movement

water between all particles keeps them together and allows them to flow

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11
Q

controlling factors: explain slope characteristics (angle)

A

uncon materials have angle of rep - when this angle is exceeded - failure

combination of other factors

slopes developed on softer/weathered rock may lie at or close to the angle of repose (shale is often relatively soft and weathers into small fragments)
.
Harder and more resistant rocks (sandstone, limestone) may fragment into large blocks which can form steep cliffs e.g. Table Mountain.

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12
Q

bedding planes

  • define
  • attitude of bedding planes
A

-

  • the attitude of a plane is
  • the attitude in relation to actual slope angle may be important in determining the type of movement
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13
Q

trigger factors

A

vibration - earthquakes and tremors
heavy rainfall - lubrication
human mod of slopes = over-steeping, increase lubrication and vibration

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14
Q

how are mass movements classified?

A

nature of materials
velocity of movement
nature of movement

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15
Q

mass movements = creep

A
  • very slow movement of soil under the influence of gravity
  • promoted by cycles of wet/dry, hot/cold, freeze/thaw – produce heaving
  • 1.0 - 10 mm per year
  • Deformation is evident in appearance of fences, trees, telephone poles etc.
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16
Q

special case of creep in cold climates

A

solifluction

17
Q

explain solifluction

A

accelerated creep that is restricted to high latitude - tundra

surface layers thaw in summer and saturated soil flows across frozen subsoil (permafrost)

faster rate - 1 -10m per year

18
Q

mass movements = flow

A

further classified as earthflow or mudflow – depending material involved

faster than creep 100km/h

19
Q

flow : mudflow

A

fine grained material

associated with heavy rainfall

20
Q

special case of flow under volcanic conditions

A
  • pryroclastic flow/lahar
  • mixture of hot volcanic gasses and ash
  • mount vesuvius
21
Q

flow : debris flow

A

-mixture of finer and coarser grained matieral

22
Q

mass movements = slide/slump

A

landslide is the most commonly used term - includes slumps, debris slides and rock slides

23
Q

mass movement - slump (slides)

A

involve rotational movement as a single unit along a well defines slippage plane

slumped block usually tilts backwards and is separated from the original face by a curved incision scar – often spoon shaped

rate of move - slower than slide = 50km/h

24
Q

mass movements = fall

A

feature of cliffs - associated with consolidated parent materials

25
Q

fall : rockfall

A

detachment of individual blocks which free fall instantaneously from a cliff

result = accumulation of
blocks of fallen rock at the
base of the slope

26
Q

talus/scree

A

accumulation of blocks of fallen rock at the base of the slope

27
Q

Human activity ===== Mass movement

A

humans affect mass movement
-excavation, dam construction

mass movements affect humans
-particularly the high magnitude-low frequency events such as catastrophic landslides.

28
Q

case of Vaiont, Italy

A
  • concrete dam built – massive which caused instability
  • massive debris slide filled the dam and caused spill over into river = flood wave of 70m moved down valley
  • almost 3000 dead, whole village consumed
29
Q

could the Vaiont disaster have been avoided?

A
  • geo investigation would have revealed weakness in surrounding limestones and shales
  • scar of ancient slide on valley side above reservoir
  • small rockslide in 1960 - a few years prior
30
Q

landslide hazard assessments

A
  • careful observation and monitoring of risk factors
  • assessment of history of mass movement act in area
  • avoid construction on vulnerable areas - no oversteepening, manage drainage
  • geo engineering solutions
  • early warning systems
31
Q

define mitigation

A

the action of reducing the severity, seriousness, or painfulness of something.