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Mass Movement

Once the original rock has been broken up by weathering and soil formation, it is now an unconsolidated mass of small fragments which can make its way downhill under the influence of gravity, very much assisted by water.

Some of the processes of mass movement occur steadily but gradually.

  • soil creep
Terracettes
  • frost heave
Frost heave

Other processes which occur on a regular basis include

  • solifluction
Solifluction
  • rain erosion
Earth pillars

Other processes which happen only occasionally, but then with greater impact on the land (and in the media), include

  • mud flows
    here causing damage to a road
Mudflow damage
  • landslides and slumps
Slumping
  • block slides
Block slide


In these various ways, the 'hillside' makes it way down to the river or glacier so that the weathered material can be tranported on the next part of its route. The hillside is lowered as the once-solid rock is removed, and new rock is exposed to the action of weathering.



Geopix Study Guide "Mass Movement"
  • gives a full image of each of these and other examples;
  • describes the main types movements;
  • describes the causes of the movement;
  • suggests methods of reducing movement;
  • suggests how to answer exam questions on this topic.



The Study Guide contains the following pages:

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'Mass Movement' is part of the Geopix Weathering and Erosion Study Guide CD.

To order this CD go to the Geopix Online Store