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Eos 101 Test 3 Verified Study Guide

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EOS 101 TEST 3 VERIFIED STUDY GUIDE

mass wasting - Answers - the downslope movement of rock, regolith, and soil under
the direct influence of gravity

weathering - Answers - The breaking down of rocks and other materials on the
Earth's surface

erosion - Answers - the removal and transport of material by wind, water, or ice

reasons to study mass wasting - Answers - 1. major geologic hazard - mass wasting
causes thousands of deaths each year
2. landform development - mass wasting, combined with actions of water, wind, and
ice, plays a major role in shaping the earth's surface

angle of repose - Answers - the maximum angle of a stable slope for loose
(unconsolidated) material; it is a function of grain size, shape, moisture

grain size and grain shape - Answers - larger grains can have a greater angle of
repose; more angular grains can have a greater angle of repose

moisture - Answers - dry grains are bound together by friction; small amounts of
water increase the cohesiveness among sand grains (greatest angle of repose);
saturation reduces friction and causes the sand to flow

controls and triggers of mass wasting - Answers - 1. water - reduces cohesion
between particles and adds weight to material
2. over-steeping of slope
3. vegetation removal - roots stabilize soil; removal by human or natural actions
leads to slope failure
4. earthquakes - ground shaking and/or liquefaction may trigger slope failure

risk factors for landslides - Answers - primary - elevation, rainfall
secondary - earthquakes, volcanoes
*greater than 30,000 mass wasting fatalities from 2004-2010

classification of types of mass wasting - Answers - 1. type of material - rock
(unconsolidated) vs. earth, mud, or debris
2. type of motion - fall vs. slope. vs. flow
3. rate of movement - fast vs. slow

fast forms of mass wasting (up to ~100km/hr) - Answers - - rockslide or rockfall
- debris flow, lahar

intermediate forms of mass wasting - Answers - - earthflow
- slump

slow forms of mass wasting (imperceptible: mm or cm/year) - Answers - - creep (ex.
frost heave)

, - solifluction (ex. regions of permafrost)

rockslide - Answers - fragments of detached rock slip along a planar surface

rockfall - Answers - fragments of detached rock fall from irregular surface

debris flow - Answers - water-laden masses of soil and rock fragments that rush
down mountainsides (often confined to canyons); result in alluvial fans

lahar - Answers - debris flow composed mostly of volcanic pyroclastic material (ash
and rock) in a slurry of water (can be initiated by volcanic eruptions that melt snow)

earthflow - Answers - commonly form on hillsides during heavy precipitation, material
moves as a viscous fluid

slump - Answers - movement of a mass of rock or unconsolidated material as a unit
along a curved surface of rupture

creep - Answers - The gradual downslope movement of soil or regolith

frost heave - Answers - an example of creep

solifluction - Answers - gradual downslope flow of water-saturated soil during warm
seasons in areas with permafrost; creates solifluction lobes

permafrost - Answers - permanently frozen layer of soil beneath the surface of the
ground; very sensitive to. heat

submarine landslides - Answers - landslides that take place underwater, can lead to
tsunamis; ex. Monterey Bay, California

the hydrologic cycle - Answers - the movement of water through the biosphere

total hydrosphere - Answers - - 97% ocean water
- 3% freshwater

total freshwater - Answers - - ~69% glaciers
- ~1% surface water
- ~30% groundwater

drainage basin - Answers - the land area that contributes water to a particular stream
or river

tributary - Answers - stream or river that flows into a larger stream/river

divide - Answers - an imaginary line, at highest surface elevation, separating one
basin from another

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Subido en
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