Landslides & Mass Movement

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Vocabulary flashcards covering mass movement causes, stresses, weak planes, mass wasting types, case studies, and mitigation techniques.

Last updated 3:39 PM on 10/10/26
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20 Terms

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Yungay, Peru Disaster

A catastrophic mass movement event where an earthquake triggered a massive ice slab to break off a glacier and shoot down a mountain, burying the town in debris within 44 minutes and resulting in 20,00020{,}000 deaths.

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Steep Slope Angle Threshold

A slope angle greater than 35⊥35^\bot (>35⊥> 35^\bot) that significantly increases the likelihood of mass movement.

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Gentle Slope Angle Threshold

A slope angle of less than 5⊥5^\bot (<5⊥< 5^\bot).

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Downslope Shear Stress (σd\sigma_d)

The downslope driving stress acting on rock and regolith that is driven by gravity.

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Normal Stress (σn\sigma_n)

The resistance stress (or shear strength) that resists downslope movement, governed by cohesion and friction.

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Parallel Weak Planes

Geological planes of weakness oriented parallel to the slope angle, which increases the probability of surface failure.

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Perpendicular Weak Planes

Geological planes of weakness oriented perpendicular to the slope angle, which decreases the probability of surface failure.

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Angle of Repose

The steepest angle that granular material can maintain without collapsing downslope.

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Talus

Loose rock material accumulated at a cliff's base that forms a steep angle of repose.

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Creep

The slow, gradual downslope movement of regolith caused by repeated cycles of expansion and contraction (freezing/thawing, wetting/drying, warming/cooling), causing trees and tombstones to tilt.

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Slump

A type of mass wasting where rock and regolith remain mostly coherent as they slide downslope along a failure surface.

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Translational Slump

A slump in which rock and regolith move downslope along a planar failure surface.

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Rotational Slump

A slump in which rock and regolith move downslope along a concave failure surface.

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Portuguese Bend Slump

A massive translational slump in Southern California where clay overlies shale bedrock; activated in 19561956 following a 1950s1950\text{s} housing boom, moving at 1 to 2 cm1\text{ to }2\,\text{cm} per day and destroying 150150 homes.

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Mudflow

A non-coherent, viscous downslope flow consisting of a slurry of mud saturated with excessive water.

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Debris Flow

A non-coherent, viscous downslope flow composed of a slurry mixture of mud and large rocks saturated with excessive water.

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Rockslide

The sudden downslope movement of rocks and debris along a non-vertical slope, which breaks into a chaotic jumble and leaves a visible scar on the slope with a debris pile at its base.

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Rockfall

A mass wasting event where rock freely falls down a vertical cliff or slope and shatters upon impact; commonly observed in exposed road cuts and during spring due to ice wedging.

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Riprap

A layer of loose stones or boulders added to a slope to stabilize it and mitigate mass wasting risk.

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Nevado del Ruiz Eruption (1985)

A volcanic eruption in Colombia with a VEI=3\text{VEI} = 3 whose pyroclastic debris melted glacier ice caps, triggering far-reaching lahars that caused over 24,00024{,}000 deaths.