Physical Geology Chapter 9: Mass Wasting

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Vocabulary flashcards covering key definitions, mechanics, controlling factors, movement classifications, and stabilization techniques of mass wasting from Physical Geology (17th Edition), Chapter 9.

25 Terms

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Mass Wasting

The downslope movement of bedrock, rock debris, or soil in bulk or as a mass under the direct influence of gravity.

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Normal Force

The component of gravitational force acting perpendicular to a slope that acts to hold material in place against the slope.

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Shear Force

The component of gravitational force acting parallel to a slope that promotes downslope movement of rock and debris.

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Shear Strength

The internal resistance of slope material to movement and deformation, controlled by material cohesiveness and related to the normal force.

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Relief

The vertical elevation difference between the valley floor and the adjacent mountain summit.

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Debris

Unconsolidated surface material consisting of soil, rock fragments, earth, or mud.

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Flow

A type of mass movement in which descending material moves downslope by internal shearing, behaving as a viscous fluid.

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Fall

A mass movement process where rock or debris drops through the air, free-falling or bouncing down a steep cliff or slope.

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Slide

A type of mass movement where a coherent, relatively intact descending mass moves downslope along one or more discrete surfaces of failure.

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Translational Slide

A landslide in which a relatively intact mass moves downslope along a planar surface or weakness plane parallel to the slope face with little rotation.

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Rotational Slide (Slump)

A landslide occurring along a concave-upward, curved failure surface where the upper part rotates downward while the lower part moves outward.

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Block Slide

A translational landslide consisting primarily of a single coherent unit or block of surface material sliding downslope.

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Creep

The extremely slow, imperceptible downward movement of soil or unconsolidated regolith at rates typically less than 1 cm/year1\,\text{cm/year}, often facilitated by freeze-thaw cycles.

<p>The extremely slow, imperceptible downward movement of soil or unconsolidated regolith at rates typically less than $$1\,\text{cm/year}$$, often facilitated by freeze-thaw cycles.</p>
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Debris Flow

A relatively rapid downslope movement involving turbulent flow of soil and regolith containing large amounts of water and coarse material such as gravel and boulders.

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Earthflow

A slow to rapid downslope movement of thick debris as a viscous fluid, typically developing on hillsides after heavy rainfall saturates the soil beneath a blanket of vegetation.

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Solifluction

A cold-climate form of earthflow in which water-saturated surface soil and debris slowly creep over an underlying impermeable substrate, such as permafrost or solid bedrock.

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Permafrost

Ground, soil, or sediment that remains completely frozen continuously for several years, forming an impermeable barrier to water drainage.

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Mudflow

A rapidly flowing, channelized slurry composed of predominantly fine-grained debris (clay and silt) mixed with water, commonly triggered by heavy rain in sparsely vegetated regions.

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Debris Avalanche

The fastest variety of debris flow, consisting of a turbulent, chaotic mass of debris, trapped air, and water rushing down steep slopes at high velocities.

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Lahar

A dangerous, rapidly flowing mudflow or debris flow composed of volcanic ash, pyroclastic debris, and water on the flanks of a volcano.

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Rockfall

A mass wasting event where individual blocks or fragments of bedrock detach from a steep cliff face and plummet or bounce freely downslope.

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Talus

An apron or sloping pile of angular rock fragments and rubble that accumulates at the base of steep cliffs and slopes through rockfall.

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Rockslide

The rapid downslope movement of a coherent mass of bedrock along an inclined plane of weakness, such as a bedding plane, joint, or foliation plane.

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Rock Avalanche

An extremely high-velocity, turbulent mass of broken-up and shattered bedrock moving down a slope, often supported by a cushion of trapped air.

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Stitching

An engineering slope-stabilization method where holes are drilled through unstable rock layers into solid bedrock, secured with cemented steel cables, and tightened with surface steel plates to prevent sliding.

<p>An engineering slope-stabilization method where holes are drilled through unstable rock layers into solid bedrock, secured with cemented steel cables, and tightened with surface steel plates to prevent sliding.</p>