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Trough (geology)

Linear structural depression that extends laterally over a distance From Wikipedia, the free encyclopedia

Trough (geology)
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In geology, a trough is a linear structural depression that extends laterally over a distance. Although it is less steep than a trench, a trough can be a narrow basin or a geologic rift. These features often form at the rim of tectonic plates. There are various oceanic troughs on the ocean floors.

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Satellite image of the Cayman Trough
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Bathymetric features of the Rockall Trough northwest of Scotland and Ireland
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Examples of oceanic troughs

See also

References

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