Geography: Mass Wasting Events
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Questions and Answers

What is the angle of repose in the context of mass wasting?

  • The maximum height a mountain can reach without collapsing.
  • The angle at which water will flow downhill.
  • The steepest angle a hillside can maintain before sediments begin to move. (correct)
  • The temperature at which materials begin to melt.

Which of the following is the fastest type of mass-wasting event?

  • Creep
  • Fall (correct)
  • Flow
  • Slide

What are talus slopes typically composed of?

  • Vegetation and organic matter.
  • Water and soil layers.
  • Clay and silt deposits.
  • Sediments accumulated at the base of a hill or mountain. (correct)

What is a lahar?

<p>A mudflow of volcanic origin. (C)</p> Signup and view all the answers

Which mass-wasting event is characterized as occurring at a slow rate?

<p>Creep (B)</p> Signup and view all the answers

What causes a mass-wasting event to occur when a slope becomes steeper than the angle of repose?

<p>Gravity acting on the aggraded sediments. (B)</p> Signup and view all the answers

What is the term used for steep cliffs left behind after a mass-wasting event?

<p>Escarpments (D)</p> Signup and view all the answers

Which of the following can NOT trigger a mass-wasting event?

<p>Dense vegetation growth (C)</p> Signup and view all the answers

Flashcards

Mass wasting

The downward movement of rock, soil, and other materials due to gravity.

Angle of repose

The maximum steepness a slope can withstand before gravity causes material to move downward.

Fall

The fastest type of mass wasting event where material falls freely.

Slide or flow

A slower type of mass wasting where material slides or flows downhill.

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Creep

The slowest type of mass wasting where material creeps downhill very gradually.

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Avalanche

A large and rapid flow of snow, ice, and rock down a mountain slope.

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Lahar

A flow of volcanic debris, primarily mud and ash, down a volcano's slopes.

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Talus slope

Accumulation of rock fragments at the base of a slope, formed by mass wasting events.

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Study Notes

Mass Wasting

  • Mass wasting is the action of gravity as a geomorphic agent
  • Common terms for mass wasting events are landslides, but this is not a technical term
  • Mass wasting can be triggered by various events like heavy rain, snowmelt, earthquakes, and forest fires, but not always a large event
  • Maximum steepness of the hillside/mountain is called angle of repose. When hillside/mountainside steepness exceeds angle of repose, gravity moves regolith downward until angle of repose is restored
  • Different types of mass wasting events exist, including falls, slides, flows, and creeps
  • A fall is the fastest type, followed by slides and flows
  • Creep is the slowest type, can be glacier-related (solifluction)
  • Mass wasting events can involve various materials like rock, debris, earth, or mud
  • Avalanche can be rock, mud, or a glacier-related snow avalanche
  • Accumulation of sediment from mass wasting events can create talus slopes or escarpments - steep cliffs at the base of a slope

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Mass Wasting PDF

Description

Explore the fascinating phenomenon of mass wasting in this quiz. Learn about the different types, triggers, and effects of these gravity-driven events on landscapes. Test your knowledge on concepts like the angle of repose and the various materials involved in mass wasting processes.

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