Karst landforms develop at small. intermediate. and large scales. Karren is the general name given to small-scale forms-varieties of dissolutional pits. grooves. and runnels. Individuals are rarely greater than 10 meters (30 feet) in length or depth. but assemblages of them can cover hundreds of square kilometers. On bare rock. karren display sharp edges; circular pits or runnels extending downslope predominate. Beneath soil. edges are rounded and forms more varied and intricate.
Sinkholes. also known as dolines or closed depressions. are the diagnostic karst (and pseudokarst) landform. They range from shallow. bowllike forms. through steep-sided funnels. to vertical-walled cylinders. Asymmetry is common. Individual sinkholes range from about 1 to 1000 meters (3 to 3.300 ft) in diameter and are up to 300 meters (1.000 ft) deep. Many may become partly or largely merged.

Dry valleys and gorges are carved by normal rivers. but progressively lose their water underground (via sinkholes) as the floors become entrenched into karst strata. Many gradations exist. from valleys that dry up only during dry seasons (initial stage) to those that are without any surface channel flow even in the greatest flood periods (paleo-valleys). They are found in most plateau and mountain karst terrains and are greatest where river water can collect on insoluble rocks before penetrating the karst (allogenic rivers).

Poljes. a Serbo-Croatian term for a field. is the generic name adopted for the largest individual karst landform. This is a topographically closed depression with a floor of alluvium masking an underlying limestone floor beveled flat by planar corrosion.

Karst plains and towers are the end stage of karst topographic development in some regions. produced by long-sustained dissolution or by tectonic lowering. The plains are of alluvium. with residual hills (unconsumed intersinkhole limestone) protruding through. Where strata are massively bedded and the hills are vigorously undercut by seasonal floods or allogenic rivers. they may be steepened into vertical towers.

The South China Karst region

The South China Karst region extends over a surface of half a million square kilometers lying mainly in Yunnan. Guizhou and Guangxi Provinces. South China is unrivalled for the diversity of its karst features and landscapes. The site presents a coherent serial property comprising three clusters: Libo Karst. Shilin Karst and Wulong Karst. South China Karst represents one of the world`s most spectacular examples of humid tropical to sub-tropical karst landscapes. The stone forests of Shilin are considered superlative natural phenomena and a world reference. The cluster includes the Naigu stone forest occurring on dolomitic limestone and the Suyishan stone forest arising from a lake. Shilin contains a wider range of pinnacle shapes than other karst landscapes with pinnacles. and a higher diversity of shapes and changing colours. The cone and tower karsts of Libo. also considered the world reference site for these types of karsts. form a distinctive and beautiful landscape. Wulong Karst has been inscribed for its giant dolines. natural bridges and caves.
 

Libo Karst

The Libo Cone Karst Nominated Site of South China Karst application for World Natural Heritage lies in Libo County. South Guizhou Buyi and Miao Autonomous Prefecture. Guizhou Province. and has a mean altitude of 747 meters ranging from 385 to 1.109 meters.
 

Shilin Karst

The Stone Forest National Park is located in Shilin Yi Autonomous County of Yunnan Province. 80 kilometers southeast of Kunming City. It covers 350 square kilometers and consists of Major Stone Forest. Naigu Stone Forest. Changhu Lake. Grand Waterfall. etc.

Wulong Karst

The Wulong Karst is located at Wujiang River downriver of Southeastern Chongqing. and it includes three karst systems of Sanqiao Natural Bridges. Furong Jiang karst gorge and caves round. and Houping erosion tiankengs. which are distributed in mid-north. southeast and northeast of Wulong County respectively. It consists of gorges. natural bridges. tiankengs. caves. shafts subterranean streams and resurgences. developing in the carbonate rocks of Cambrian-Ordovician systems and Permian-Triassic systems.