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//-->{{Short description|Rock overlying a less resistant type}}{{for|the region in Texas|Caprock, Texas}}Caprock or cap rock is a more resistant rock type overlying a less resistant rock type,Kearey, Philip (2001). Dictionary of Geology, 2nd ed., Penguin Reference, London, New York, etc., p. 41.. {{ISBN|978-0-14-051494-0}}. analogous to an upper crust on a cake that is harder than the underlying layer.

Description

File:DSCN4413 horseshoefalls e.jpg|thumb|right|Horseshoe Falls, part of the Niagara EscarpmentNiagara EscarpmentThe Niagara Escarpment, over which Niagara Falls flows, is an example of a scarp or escarpment. At Niagara Falls, the caprock is the riverbed above the falls, and is what prevents the river from eroding the face of the falls very quickly. The Niagara caprock is made of dolomitic limestone. Other common types of caprock are sandstone and mafic rock.In processes such as scarp retreat, the caprock controls the rate of erosion of the scarp. As the softer rock is cut away, periodically the caprock shears off. Caprock is also found in salt domes and on the top of mesa formations.

Petroleum

In the petroleum industry, caprock is any nonpermeable formation that may trap oil, gas or water, preventing it from migrating to the surface. This caprock can prevent hydrocarbons from migrating to the surface, allowing them to accumulate in a reservoir of oil, gas and water. These structures, also known as petroleum traps, are a primary target for the petroleum industry.

Salt dome caprock

The tops of salt domes such as in the Gulf of Mexico dissolve in a characteristic manner, and can range between 0–1500 ft thick.JOURNAL, Walker, Charles W., Dec 1976, AAPG Bulletin, Origins of Gulf Coast Salt-Dome Cap Rock, 60, 12, 2162–2166,search.datapages.com/data/bulletns/1974-76/data/pg/0060/0012/2150/2162.htm, 2010-09-07, 10.1306/c1ea3aa0-16c9-11d7-8645000102c1865d, The halite (salt) is removed first, leaving behind gypsum and anhydrite. The anhydrite and gypsum react with organic material to form calcite. The classic Murray 1966 paperJOURNAL, Murray, Grover E., Mar 1966, Salt structures of Gulf of Mexico basin--a review, AAPG Bulletin, 50, 3, 439–478,search.datapages.com/data/bulletns/1965-67/data/pg/0050/0003/0400/0439.htm, 2010-09-07, 10.1306/5d25b49d-16c1-11d7-8645000102c1865d, describes the generalized sequence as sediments-calcite-gypsum-anhydrite-salt.

See also

• Caprock Canyons State Park and Trailway
• Caprock Escarpment
• Hoodoo (geology)
• Monadnock

References

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