Scarp (landform)

A fault scarp created by the 1983 Borah Peak earthquake
Escarpment face broken by a fault, Cumberland Plateau, Tennessee

Scarp is a term in geology and geography with several similar meanings.

Formation

Scarps are generally formed by one or both:

  1. differential erosion of sedimentary rocks, or by
  2. vertical movement of the Earth's crust along a geologic fault.

Most commonly, an escarpment is a transition from one series of sedimentary rocks to another series of a different age and composition.

Escarpments are also frequently formed by faults. When a fault displaces the ground surface so that one side is higher than the other, a fault scarp is created. This brings a piece of high ground next to an area of lower ground.

More loosely, the term scarp describes the zone between coastal lowlands and continental plateaus. A marked, abrupt change in height is caused by coastal erosion at the base of the plateau.

Schematic cross section of a cuesta, dip slopes facing left, and harder rocklayers in darker colors than softer ones.

References

  1. ↑ Easterbrook, D. J. 1999. Surface processes and landforms. 2nd ed, Prentice Hall, New Jersey.
  2. ↑ Summary: Escarpments Archived 2010-12-01 at the Wayback Machine, US Army Corps of Engineers.
  3. ↑ scarp - Definition from the Merriam-Webster Online Dictionary