Same as in any caves of the same types anywhere in the world, which in karst caves is dissolution of the host limestone by weakly-acidic ground-water.
chemical weathering called karsting and it createskarst topography. ... Dissolution of soluble limestone creates limestone cavessource yahoo answers
The most common cause of chemical weathering is oxygen
The most common cause of chemical weathering is oxygen
Chemical weathering is the most effective in hot and dry climates. This is because this climate accelerates and intensifies the chemical weathering.
Plant growth is both a chemical and mechanical process. The roots secrete mild acids that dissolve minerals in rocks, and the plant's roots and stems can increase in size and force rocks apart inside cracks and crevices.
Most caves are made out of limestone, which is a sedimentary rock composed of calcium carbonate. This rock is easily dissolved by acidic water, leading to the formation of caves through a process called chemical weathering and erosion. Other types of caves can also form in volcanic or igneous rock, such as lava tubes.
Caves can form in a variety of ways, but most caves are dissolutional and are initially formed by chemical weathering of surface rock, usually limestone, by carbonic acid contained in rainwater. As chemical weathering continues, mechanical weathering joins in the fun to further attack and widen joints and fissures in what is usually soluble sedimentary rock, like limestone.Some other types of caves are formed by percolating sulfuric acid, flowing lava, flowing water in glaciers, wave action, and particle abrasion.
Chemical weathering is most common in warm and wet climate.
Most limestone caves are created through a process called chemical weathering, specifically carbonation. This occurs when rainwater combined with carbon dioxide in the atmosphere creates a weak acid that dissolves the calcium carbonate in the limestone bedrock, gradually forming caves over time.
The most important factors in chemical weathering are water and carbon dioxide.THIS IS TRUE
Weak acids seep into the ground until they reach a zone soaked with water. As the ground water become more acidic, it dissolves calcite and other minerals in the rock. Over time, the action of the acidic water produces holes in the rock. The holes grow, creating passages, chambers, and pits, and eventually become caves.
The chemical weathering process responsible for cave formation is called carbonation. Carbonation occurs when rainwater, which is slightly acidic due to dissolved carbon dioxide, reacts with limestone or other carbonate rocks to form soluble bicarbonate ions that dissolve the rock over time, creating caves.