The reaction of carbon dioxide in rainwater creates a weak carbonic acid, which dissolves limestone over time. This process, known as carbonation, leads to the formation of caves in limestone formations. Over thousands of years, the acidic water dissolves the limestone, creating underground tunnels and chambers.
Limestone is the rock type most easily dissolved by groundwater, due to its high solubility in acidic water. This process results in the formation of features such as caves, sinkholes, and underground streams.
An acid cave forms when acidic groundwater dissolves limestone or other carbonate rocks, creating underground voids and passageways. Over time, the acidic water enlarges these cavities and forms unique underground features such as stalactites and stalagmites. Factors like the presence of carbon dioxide in the water contribute to the acidic conditions that lead to cave formation.
Rain water + atmospheric CO2 gives Carbonic Acid - very weak but over time able to dissolve limestone.
Caves, their stalactite and stalagmite formations (calcite by precipitation & crystallising of the calcium carbonate) - and scale in kettles etc using water that has passed through the limestone uplands.
Sedimentary rocks can be formed by chemical reactions when minerals in water precipitate out and settle to form rock layers. Examples of sedimentary rocks formed by chemical reactions include limestone and halite.
Rain water + atmospheric CO2 gives Carbonic Acid - very weak but over time able to dissolve limestone.
Primarily in their mode of formation: dissolution of limestone by water acidified by atmospheric CO2 (forming carbonic acid).
Underground limestone caves form through the chemical weathering of limestone rock by water that is slightly acidic. Over time, this process dissolves the rock and creates caverns and passageways underground. Factors such as the presence of cracks and fissures in the limestone, as well as the flow of water, contribute to the formation of these caves.
Limestone is a type of rock that is easily eroded by water, which can create caves over time. Water dissolves the limestone rock to form caves through a process known as chemical weathering. Additionally, limestone can also be carved out by underground rivers or other natural forces, resulting in the formation of caves.
Limestone is susceptible to dissolution by acidic water, which is common in most natural environments. Over time, this dissolution process carves out cavities underground, leading to the formation of caves. Additionally, limestone is a common and widespread rock type, which contributes to the prevalence of limestone caves.
You'd need to consult the area's geology map to understand fully, but very simply there must be a bed of impervious & impermeable rock lying below the limestone that actually holds the caves, to keep the cave-forming water up in the limestone's formation.
Other way round! Water and/or air are in caves.:-) Most of the world's caves have formed / are forming in limestone.
Limestone is a type of rock commonly associated with the formation of stalactites and stalagmites in caves. It is composed primarily of calcium carbonate, which is soluble in water, allowing for the slow formation of these mineral formations over thousands of years.
As weathering erodes limestone underground, it can form caves, sinkholes, and underground rivers. Over time, the chemical reactions between water and limestone can result in the dissolution and reshaping of the rock into unique structures and landscapes.
When limestone dissolves, the dissolved material forms ions, primarily calcium and bicarbonate ions, in the water. These ions can then be carried away by the water through rivers or groundwater. Over time, this process can lead to the formation of caves and sinkholes.
Karst caves, and it is the majority of caves; formed by acidic ground-water dissolving the limestone.
Air! They are voids IN limestone formed by dissolution by water.