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A karst topography is that which composes of limestone and its associated features and structures.

•Karst topography and caves develop in limestone rocks due to their solubility in dilute acidic groundwater.

•The solubility of limestone in water and weak acid solutions leads to karst landscapes.

•Regions overlying limestone bedrock tend to have fewer visible above-ground sources (ponds and streams), as surface water easily drains downward through joints in the limestone.

•While draining, water and organic acid from the soil slowly (over thousands or millions of years) enlarges these cracks, dissolving the calcium carbonate and carrying it away in solution.

•Most cave systems are through limestone bedrock.

•Cooling groundwater or mixing of different groundwater will also create conditions suitable for cave formation.


Karst topography occurs when the underlying bedrock is dissolved. The bedrock is made of gypsum, limestone or dolomite. This causes sinkholes and caverns to form.

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What is an area with many sinkholes?

An area with many sinkholes is called a sinkhole-prone region. These regions often have underlying soluble rock such as limestone or gypsum that can dissolve over time, leading to the formation of sinkholes. It is important to be cautious in such areas to prevent accidents or property damage.


What is a karst specialist?

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.


Which features are common in areas of karst topography?

Common features in karst topography include sinkholes, caves, underground rivers, and disappearing streams. Karst landscapes are characterized by the dissolution of soluble rocks such as limestone, resulting in unique surface and subsurface landforms.


What are common karst landforms?

Common karst landforms include sinkholes, caves, disappearing streams, and karst towers. These landforms are a result of the dissolution of soluble rocks such as limestone, dolomite, and gypsum by groundwater. Karst landscapes are known for their unique and often fragile features created by the erosion of these types of rocks.


Is magma required to form karst topography?

No, magma is not required to form karst topography. Karst topography is primarily formed by the dissolution of soluble rocks such as limestone, dolomite, and gypsum by water, leading to the creation of sinkholes, caverns, and underground drainage systems.