Karst

From Wikipedia, the free encyclopedia
Jump to: navigation, search
A karst spring in the Jura mountains near Ouhans in eastern France at the source of the river Loue
The Devil's Hole sinkhole near Hawthorne, Florida, USA.
The karst limestone, after surface rock has weathered away, makes a ground surface which is almost imposssibly difficult for humans. Velebit in Croatia.
From a World Heritage Site in Madagascar, the Tsingy de Bemaraha Strict Nature Reserve. Gradual erosion has produced vast fields of limestone spires known locally as tsingy, interspersed with dry forests, lakes and mangrove swamps inhabited by numerous endemic and threatened lemur and bird species.

Karst is a geological system of rocks where water has eroded (dissolved) the bedrock. If it is very extensive, karst can be a geographical or topographical feature. Is is classed as a badland if it difficult to travel through the environment, which it often is.

Almost always, karst is formed in carbonate rocks, such as limestone or dolomite. Since carbonate sedimentary rocks are very common, karst areas occur all over the world.

Many karst regions display distinctive surface features, with sinkholes being the most common. However, karst surface features may be absent where the soluble rock is mantled (covered), such as by a non-soluble rock strata on top of the carbonate strata. Some karst regions include thousands of caves, and the water is generally underground.

The world's largest karst area is the Nullarbor Plain, part of the area of flat, almost treeless, dry country of southern Australia. It is on the Great Australian Bight coast with the Great Victoria Desert to its north. It is the world's largest single exposure of limestone bedrock, and occupies an area of about 200,000 square kilometres (77,000 sq mi).[1] At its widest point, it stretches about 1,100 kilometres (684 mi) from east to west across the border region between South Australia and Western Australia.

Sinkholes[change | edit source]

Many parts of the world suffer from sinkholes which form when karsts are underground. Beneath the flat surface of the land in Florida, Guatemala City and elsewhwere are vast systems of limestone. Water running through the limestone is dissolving the limestone away, leaving huge caverns. Without warning, huge holes appear in the surface, causing great damage. Practically the whole of Florida is sitting on a gigantic karst system, as are several countries in Central America. The area round Tampa is especially at risk, and there is a huge karst system under Mexico City.[2] According to a senior geochemist, there are as many as 15,000 sinkholes in Illinois.[3]

The world's deepest sinkhole is China's Xiaozhai Tienkeng at 2172ft (662m). The Qattara Depression in Egypt is roughly 50 miles (80km) by 75 miles (121km) in surface size. It is an ancient sinkhole.[4]

Related pages[change | edit source]

References[change | edit source]

  1. "Across the Nullarbor Plain". Kevin's Wilderness Journeys. 7 June 2004. Archived from the original on 10 October 2007. http://web.archive.org/web/20071010135423/http://wilderness.esmartweb.com/Australia/nullabor.html.
  2. Stewart, Iain 2014. Sinkholes: a deadly threat from Florida's 'underworld'. BBC News Science & Environment. [1]
  3. Illinois golfer plunges down sinkhole on the 14th. BBC News 13 March 2013. [2]
  4. Who, What, Why: How are sinkholes formed? BBC News. [3]
Global distribution of major outcrops of carbonate rocks (mainly limestone, except evaporites)