Acidic ground water (rain-water that has absorbed atmospheric carbon dioxide to form carbonic acid) dissolving the limestone as it flows through the joints & other discontinuities in the rock mass.
chemical weathering called karsting and it createskarst topography. ... Dissolution of soluble limestone creates limestone cavessource yahoo answers
It causes chemical weathering because when it touches rocks, the rocks dissolve, forming caves.
In all limestone caves, the same as as is "evident" - by the cave's very existence - as in all the limesrtone caves and other karst features in your country - chemical weathering! (Dissolution by carbonic acid.)
When acid rain falls on limestone, chemical weathering called dissolution occurs. The acidic rainwater reacts with the calcium carbonate in the limestone, causing it to dissolve and gradually wear away the rock over time. This process can result in the formation of features such as caves and sinkholes.
Carbonic acid, formed when carbon dioxide dissolves in rainwater, is the main driver of chemical weathering in limestone. As the carbonic acid comes into contact with the limestone, it reacts to dissolve and break down the rock, leading to the formation of features such as caves, sinkholes, and karst landscapes.
chemical weathering called karsting and it createskarst topography. ... Dissolution of soluble limestone creates limestone cavessource yahoo answers
Chemical weathering, particularly when acidic water dissolves and erodes the rock, can create caves or caverns over time. This process is common in limestone regions where the rock is easily dissolved by carbonic acid found in rainwater.
The formation of caves due to the dissolution of limestone by acidic rainwater is an example of chemical weathering. This process results in the gradual breakdown of the rock through chemical reactions.
The caves were primarily formed due to chemical weathering. The process of carbonation involving the dissolution of limestone by acidic rainwater played a significant role in the development of these caves. This type of weathering gradually breaks down the calcium carbonate in limestone, creating underground cavities and cave systems.
The process that hollows out limestone in caves is called chemical weathering. This occurs when rainwater combines with carbon dioxide in the atmosphere to create a weak carbonic acid, which gradually dissolves the limestone over time, resulting in the formation of caves and caverns.
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.
It causes chemical weathering because when it touches rocks, the rocks dissolve, forming caves.
In all limestone caves, the same as as is "evident" - by the cave's very existence - as in all the limesrtone caves and other karst features in your country - chemical weathering! (Dissolution by 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.
The same type evident in all limestone caves, and in your country too!Chemical weathering - the limestone is dissolved by weakly acid water flowing through them. Some mechanical erosion by abrasion in high water, but this is a secondary mechanism.
When acid rain falls on limestone, chemical weathering called dissolution occurs. The acidic rainwater reacts with the calcium carbonate in the limestone, causing it to dissolve and gradually wear away the rock over time. This process can result in the formation of features such as caves and sinkholes.
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.