Groundwater sapping

From Wikipedia, the free encyclopedia
Jump to: navigation, search
Scientists believe that groundwater sapping created these gullies in Noachis Terra on Mars. NASA image.
The two canyons at center-left in this photo from Canyonlands National Park in Utah have the theater-shaped heads typical of valley features shaped by groundwater sapping. The Green River is at right.

Groundwater sapping is the geomorphic process in which groundwater exits a bank or hillslope laterally as seeps and springs and erodes soil from the slope. This often causes the slope to be undermined and undergo mass wasting, hence the word sapping.

This is one of the processes involved in the formation of gullies, such as lavaka. Erosion by sapping tends to produce steep-sided U-shaped valleys of fairly uniform width with box-like, "theater-shaped" headwalls. This contrasts with the more common branching or dendritic pattern of V-shaped valleys produced by overland flows that become wider with distance from their source. Groundwater sapping has been suggested as the cause for erosion of the valley and channel networks on Mars, although studies show that groundwater alone can not excavate and transport the material required to create these canyons.[1]

See also[edit]


  1. ^ Lamb, M. P.; Dietrich, W. E.; Aciego, S. M.; Depaolo, D. J.; Manga, M. (2008). "Formation of Box Canyon, Idaho, by Megaflood: Implications for Seepage Erosion on Earth and Mars". Science 320 (5879): 1067–1070. Bibcode:2008Sci...320.1067L. doi:10.1126/science.1156630. PMID 18497296. 

External links[edit]