English Deutsch Français Italiano Español Português 繁體中文 Bahasa Indonesia Tiếng Việt ภาษาไทย
All categories

4 answers

Water dissolves limestone under the surface which causes the top layer to collapse, which forms sinkholes & that is what is known as karst topography.

2006-07-28 11:20:48 · answer #1 · answered by Colleen S 2 · 1 3

Living in the Limestone Belt of Southern Indiana, we have Karst topography everywhere!

Limestone is essentially calcium carbonate (there are other carbonate minerals), which dissolves when exposed to acids. Rainfall is naturally slightly acidic, and dissolves the limestone - which is where the typical rounded shape of the land comes from. It is how sinkholes, caves, etc. form.

Try these for further information:
http://geography.about.com/od/physicalgeography/a/karst.htm
http://www.watersheds.org/earth/karst.htm
http://igs.indiana.edu/geology/karst/karstInIndiana/index.cfm

2006-07-28 12:06:03 · answer #2 · answered by Rockmeister B 5 · 1 0

Karst Topography is the equipment of underground caves and sinkholes in a (somewhat) flat limestone terrain. Carbonic acid (H2CO2) etches out limestone alongside fractures interior the limestone, interior the technique arising this topography.

2016-12-10 17:20:29 · answer #3 · answered by herzog 4 · 0 0

Karst Topography is the system of underground caves and sinkholes in a (relatively) flat limestone terrain. Carbonic acid (H2CO2) etches out limestone along fractures in the limestone, in the process creating this topography.

2006-07-28 11:36:59 · answer #4 · answered by Amphibolite 7 · 0 0

fedest.com, questions and answers