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Faulting

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Faulting

Common types of faults.

Common types of faults. Image via Noaa.gov

ZIMSEC O Level Geography Notes: Faulting.

  • Lateral earth movements often produce very great stresses due to compressional forces (when plates move towards one another) and tensional forces (pulling apart).
  • These forces can cause fractures or breaks in the earth’s crust.
  • When breaks occur in the earth’s crust where no rocks are displaced the breaks are called joints.
  • If the rocks are displaced on both or either side of the crack it is called a fault.
  • Faulting refers to the fracturing or breaking of the earth’s crust due to both compression and tension forces as a result of the tectonic movements.
  • Faulting normally displaces the crustal block along lines.
  • The end result is that rocks are either heaved (pushed) above or dropped below the general level of land.

Features of a simple fault

  • Heave-the forward horizontal displacement of the sediments.
  • Throw-the vertical displacement of the sediments or strata (layer).
  • When rocks are folded and tilted they do so in many ways and the following terms are used to describe these tilts.
  • Dip-refers to the direction the sediment tilts in.
  • Bedding plane-refers to the surface or plane that separates one sediment layer from another. This is normally a line that follows the weaknesses between sediments (layers) of different compositions.
Features of a simple fault.

Features of a simple fault.

Types of faults

  • There are several types of faults viz:
  1. Normal faults
  2. Reverse faults.
  3. Tear fault

1 Normal faults

A normal fault.

A normal fault.

  • Is caused by tension forces which cause part of the earth to move downwards.
  • That is the central block (the one to the right in the picture, not shown in the picture is a fault plane to the right of the central block) is displaced downwards.

2. Reverse fault.

Reverse fault. Original image by Artinaid.

Reverse fault. Original image by Artinaid.

  • Are caused by compressional forces i.e pushing towards each other.
  • When rocks are subjected to compression the central block is forced upwards (heaved upwards) relative to the level ground and adjoining blocks.
  • That is the central block (the one to the right in the picture) is displaced upwards.

3. The Tear fault.

A tear fault. Image by Aibn

A tear fault. Image by Artinaid.

  • It is produced by tear forces which move in opposite direction of past each other.
  • It usually results in rift valleys.

Please go to this page to read on the landforms resulting from faulting.

To access more topics go to the Geography Notes page.

 

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By | 2017-01-17T11:22:26+00:00 June 4th, 2015|Landform Studies, Notes, O Level Geography|0 Comments

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