Lecture 20 - Mass Wasting Part 2 Flashcards

1
Q

fall

A

a material dropping through air, vertically or almost vertically

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2
Q

slide

A

a material movie as a mass along a sloping surface (there is no internal motion within the mass itself)

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3
Q

flow

A

downslope movement of a material that also has internal motion, like a fluid (eg. water, lava)

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4
Q

regardless of name, most mass wasting examples include two or more of the following: ____

A

fall, slide, or flow

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5
Q

falls are an extremely __ or very ___ form of mass wasting seen with ___ and ____

A

rapid
rapid

rocks (rockfall)
unconsolidated materials (soil fall)

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6
Q

rockfalls

A
  • rapid downslope movement of dislodges rocks that originates above a steep enough slope
  • rocks may experience falling, rolling, bouncing, and/or sliding
  • falling rocks include broken chunks from bedrock outcrops or boulders coming down mountain slides/cliffs
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7
Q

bedrock

A
  • hard, solid sock (ie. consolidated rock) under unconsolidated surface materials such as soil, sand or gravel
  • can extend hundreds of meters below earths surface
  • exposed (ie. above earths surface) bedrock seen on mountain tops, along coastlines, in quarries and on plateaus
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8
Q

plateau

A

region of relatively level/flat ground with a higher elevation than surrounding area

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9
Q

outcrops

A

visible exposures of bedrock occurring due to erosion or tectonic plate activity

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10
Q

hydrostatic pressure

A

pressure exerted by any fluid (eg. water) in a confined space

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11
Q

rockfalls and soil falls can also be driven by:
(other than factors discussed in previous lecture — shear force, shear strength, rock strength)

A
  • hydrostatic pressure and the presence of water in bedrock cracks
  • freeze (ie. expansion) and thaw (ie. contraction) cycles
  • heavy snowfall and subsequent melt
  • plant roots in bedrock cracks
  • erosion by rivers/streams and/or wave action below (aka. undercutting)
  • quarrying (ie. mining) activities
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12
Q

slides can range from extremely ___ to extremely __. this form of mass wasting is seen with __ and __

A

slow
rapid

rocks
unconsolidated materials such

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13
Q

types of slides

A
  • rock slide
  • rock avalanche
  • slump
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14
Q

rock slide

A
  • sliding motion of rocks along a sloped surface
  • can range from very slow to moderately fast
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15
Q

rock avalanche

A
  • sliding motion of rocks along a sloped surface
  • larger rocks moving downhill quickly (at speeds on the order of meters/second) fragment (ie. breaks down) to form smaller rocks/pieces that keep moving downhill /slope
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16
Q

slump

A
  • sliding encountered when have thick (>10 meters) layer/slice of unconsolidated material on a curved slope
  • (may also observe same for rock layer on curved slope)
  • can occur extremely slowly to moderately fast
  • mass of unconsolidated material gradually moves downward and spread outward
  • often caused by presence of excess water between unconsolidated layer and served slope
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17
Q

types of flows

A
  • creep
  • mudflows
  • debris flows
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18
Q

what’s a creep

A
  • very slow (mm/year to cm/year) movement of soil/unconsolidated materials down a slope
  • prevalent on sloped surfaces
  • an example of very slow flow but difficult to rule out some sliding in many cases
  • results in cracked roads
  • results in trees, fenceposts, grave markers, etc… that lean downhill
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19
Q

trees exposed to creep end up with ___

A

curved lower trunk

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20
Q

curved trunk is also known as ___

A

pistol butt

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21
Q

flows can range from extremely ___ to extremely ___. this form of mass wasting is generally associated with unconsolidated materials

22
Q

creep down a sloped surface can be enhanced by (3)

A
  • frozen subsoil preventing water drainage and wet materials down above slowly moves downhill
    -freeze/thaw
  • frequent wetting/drying of soil
23
Q

what is solifluction

A
  • creep triggered by freeze-thaw in colder climates
  • gradual movement of wet soil/wet unconsolidated materials down a slope
24
Q

what are mudflows and debris flows

A
  • often rapid and extremely raid movement of soil/sediment/unconsolidated materials down a slope

sediment/unconsolidated materials saturated with water (eg. due to heavy rain, ice/snow thaw) lose strength and ability to stay/stick together

sediment/unconsolidated material grains are pushed apart to extent that saturated mixture can actually flow

25
in mudflows and debris flows, since sediment/unconsolidated materials are saturated with water, the flow can occur even down ____
gentle slopes
26
mudflow
flow of (water) saturated unconsolidated materials down whose grains are sand-sized or smaller
27
debris flow
flow of (water) saturated unconsolidated material whose grinds are gravel-sized or larger
28
scientists classify soil into …. show the order biggest to smallest
gravel/stones, sand, silt, clay
29
what is pore space
the space that exists between soil particles
30
what is pore size
size of spaces that exist between soil particles
31
when all pore spaces (ie, the entire pore volume) is filled with water, the soil is __
saturated
32
as debris flows involve movement of ___ particles than mudflows, they typically require ___ than mudflows
larger steeper slopes
33
example of a common process resulting in debris flow
1. unconsolidated material from a stream or riverbank collapse into the water 2. unconsolidated materials initially blocks water flow, then becomes saturated, ultimately mixing and flowing with water 3. major and sudden downstream flow of previously blocked water + saturated unconsolidated materials occurs, potentially causing significant damage (downstream)
34
what can cause mudflows and debris flows
volcanoes
35
___ can suddenly melt ice/snow
volcanic activity
36
melted ice/snow can saturate unconsolidated materials, causing ____
causing said materials to flow downstream/down slope with water
37
lahar
mudflows and debris flows occurring on a volcano or associated with volcanic activity
38
__ is a flowing mixture of water, debris, volcanic and unconsolidated material
lahar
39
topple
- forward rotation and movement of a mass/slice of rock or unconsolidated material (earth, debris) our of a slope - can occur extremely slowly or rapidly - triggered by factors including ice/snow thaw, weathering, undercutting and fluvial erosion - results in formation of debris pile (ie. debris cone or talus cone) at base of slope
40
talus cone
a debris or rock pile at base of slope/mountain/hill
41
what is the head scarp and toe of a slump
head scarp is the top toe is the bottom (see image no slide 10)
42
debris
loose, natural material consisting especially of broken pieces of rock
43
erosion
geological process in which material are worn away and potentially transported naturally by wind or water
44
undercutting
erosion of material at the foot of cliff or steep slope
45
fluvial erosion
erosion caused by flowing water (on the adjacent rock/unconsolidated materials
46
weathering
breaking down or dissolving rocks and mineral on Earth’s surface
47
factors that drive weathering
- water - ice/snow - acids - salts - plants - animals - temperature fluctuations
48
once rocks broken down into its of rocks and minerals, ___ can transport these bits away
erosion
49
how are erosion and weathering different
both involve breakdown of materials erosion: generally implies worn-down materials are transported away weathering: materials are also worn down but not transported away
50
landslide
- failure and downslope movement of rock or unconsolidated materials due to gravity - movement of rock or unconsolidated material (debris or earth) mass down a slope due to gravity landslide = mass wasting (aka slope failure)