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Bench (geology)

Plateaus and Highlands

In geomorphology, a bench or benchland is a long, narrow strip of fairly level or gently sloping land that is bounded above and below by distinctly steeper slopes. Benches have several different origins. Differences in hardness between rock or sediment layers can leave structural benches through differential erosion. Narrow fluvial terraces form when a river abandons its floodplain and cuts down into the valley. A narrow flat area at the base of a sea cliff, cut by waves or other erosion near the shoreline, is called a coastal bench, wave-cut bench or wave-cut platform. In mining the same word names a narrow, step-like strip cut into the wall of an open-pit mine to give access for working it.

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Source Bench (geology) (Wikipedia)
Source Bench (geology) (Wikipedia)
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Bench (geology) (Wikipedia)
  • Shaped By: Fluvial Erosion, Lead
    other benches are narrow fluvial terraces created by the abandonment of a floodplain by a river or stream and entrenchment of the river valley into it
  • Shaped By: Wave Erosion, Lead [shaped-by]
    a narrow flat area often seen at the base of a sea cliff created by waves or other physical or chemical erosion near the shoreline
  • In Group: Plateaus and Highlands (World), Lead
    is a long, relatively narrow strip of relatively level or gently inclined land bounded by distinctly steeper slopes above and below it
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