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The question has answered itself! The generic name for such landscape is 'karst', from the Slovac name for the type-area.
acidic groundwater
Carbonic Acid
Carbonic Acid
a.) Sinkholes b.) sinking streams c.) caverns d.) all of the above
caverns, sinkholes, etc.
The question has answered itself! The generic name for such landscape is 'karst', from the Slovac name for the type-area.
acidic groundwater
Carbonic Acid
When limestone is eaten away, it forms various features such as sinkholes, caves, and underground tunnels. This process occurs due to the dissolution of the limestone by acidic groundwater. The result is the creation of unique and sometimes expansive underground landscapes.
Carbonic Acid
a.) Sinkholes b.) sinking streams c.) caverns d.) all of the above
In limestone and sandstone areas, especially, ground water filtering through the rock and dissolving the limestone or sandstone, creates potholes, caverns and caves.
Limestone
Caves, caverns, and sinkholes are typically formed by the dissolution of soluble rocks such as limestone, dolomite, or gypsum by water. Over time, water erodes and dissolves the rock, creating underground cavities and passages. Eventually, these cavities can collapse or become exposed at the surface, forming caves, caverns, and sinkholes.
The limestone caverns themselves are formed by groundwater gradually dissolving the limestone rock. In this process, some of the limestone is taken into solution, and under favourable conditions, it will form a drip on the roof of a cavern. This may eventually build to form a stalactite above, and perhaps also a stalagmite below it.
Sinkholes and caverns are formed from carbolic acid. This carbolic acid dissolves rock which creates the spaces that form the sinkholes and caverns. The carbolic acid is created when carbon dioxide dissolves in water.