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sinkholes.
Karst topography is a landscape shaped by the dissolution of a layer or layers of soluble bedrock, usually carbonate rock such as limestone or dolomite.[1]Due to subterranean drainage, there may be very limited surface water, even to the absence of all rivers and lakes. Many karst regions display distinctive surface features, with sinkholes or dolines being the most common. However, distinctive karst surface features may be completely absent where the soluble rock is mantled, such as by glacial debris, or confined by a superimposed non-soluble rock strata. Some karst regions include thousands of caves, even though evidence of caves that are big enough for human exploration is not a required characteristic of karst.
A karst environment, or karst topography.
The physical weathering and chemical weathering process creates Karst topography and landscapes. Caves and Caverns are common of Karst topography.
There are models that show the development of caves under specific conditions in limestone rocks. Of course there are figures that show the formation and the development of a variety of passageways in caves. You can find all these staff in literature related with karst geomorphology.
Sinkholes are common in areas of karst topography
sinkholes.
Karst caves (i.e. dissolutional features in limestone).
It is called a karst topography.
William J Wolfe has written: 'Hydrology and tree-distribution patterns of karst wetlands at Arnold Engineering Development Center, Tennessee' -- subject(s): Geographical distribution, Hydrology, Karst, Karst Hydrology, Trees, Wetlands
A Karst topography displays a variety of large or small scale features both on the surface and beneath. On exposed surfaces, small features may include flutes, runnels, clints and grikes, collectively called karren or lapiez. Medium-sized surface features may include sinkholes or dolines (closed basins), vertical shafts, disappearing streams, and reappearing springs. Large-scale features may include limestone pavements, poljes and blind valleys. Mature karst landscapes, where more bedrock has been removed than remains, may result in karst towers or haystack/eggbox landscapes. Beneath the surface, complex underground drainage systems (such as karst aquifers) and extensive caves and cavern systems may form.
It is an area of exposed, mechanically and chemically weathered and eroded limestone landscape terrain and may contain sinkholes, caves, and other features. See the link below for pictures of an extreme karst terrain.
Karst, not "karts"! Yes, almost by definition. Karst landscape is that formed in limestone by the action, particularly chemical-weathering (solution) of the rock by rain-water. If the structural nature of the massif, and its hydrology, are suitable then caves will form as part of that the entire suite of karst features.
Karst topography is characterized by a lack of surface water, with land containing sinkholes and often caves as well. There may also be disappearing and reappearing springs due to complex underground drainage systems.
Adam Karst's birth name is Adam Jordan Karst.
Britni Karst's birth name is Britni Nicole Karst.
A karst specialist is a geologist who is expertized in Karst Geomorphology. This type of scientists study the conditions and the procedures that lead to the formation of karst in limestone rocks.