Not a helpful question - unclear meaning.
Limestone is a sedimentary rock and the exposure or burial of any given limestone formation depends on its regional, subsequent geological processes.
It is also soluble in weakly-acid ground-water, giving rise to karst lansdcapes and features.
As for "use" by humans, it has long been quarried for various purposes by both open-cast and underground techniques.
it rains and sinks into limestone and over to starts to corrode at the vulnerable limestone
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 rock that is easily dissolved by water, forming cavities and underground features like caves, sinkholes, and underground rivers. Over time, the natural processes of erosion and chemical weathering create these unique geological formations in limestone terrain.
we wouldn't have these- -Limestone is used in buildings and roads. - Limestone can be used in glass making. - Limestone is used in toothpaste. - Limestone is used in cement and mortar. - Limestone is used in bread and cereals as a source of calcium. - Limestone is used to make paper white. -Limestone is used to purify sugar. -Pulverized limestone is used to neutralize acidic soils. -Limestone can be used to make brake pads. -Limestone is used in the preparation of wools and dyes. -Limestone is used to make antacids. -Limestone is used in climbing walls. -Limestone is used a suppression of methane explosions in underground coalmines. -Limestone is added to plastics, paint, tiles and other materials as both white pigment and cheap filler. -Limestone is used in the manufacture of quicklime (calcium oxide) and slaked lime (calcium hydroxide). -Limestone can be used to create steel by using it in a blast furnace.
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.
Karst topography forms when underground layers of limestone are dissolved by groundwater. This process creates unique landforms such as sinkholes, caves, and underground drainage systems. The dissolution of limestone occurs due to its chemical composition and the acidic nature of groundwater.
Water flows underground in limestone areas due to the rock's solubility, which allows it to dissolve and create cavities and channels over time. This process, known as karstification, forms underground rivers and aquifers. The porous nature of limestone facilitates the movement of water, enabling it to travel through these subterranean pathways. As a result, groundwater systems in limestone regions can be extensive and complex.
>Limestone is used in buildings and roads. >Limestone can be used in glass making. >Limestone is used in toothpaste. >Limestone is used in cement and mortar. >Limestone is used in bread and cereals as a source of calcium. >Limestone is used to make paper white. >Limestone is used to purify sugar. >Pulverized limestone is used to neutralize acidic soils. >Limestone can be used to make brake pads. >Limestone is used in the preparation of wools and dyes. >Limestone is used to make antacids. >Limestone is used in climbing walls. >Limestone is used a suppression of methane explosions in underground coalmines. >Limestone is added to plastics, paint, tiles and other materials as both white pigment and cheap filler. >Limestone is used in the manufacture of quicklime (calcium oxide) and slaked lime (calcium hydroxide). >Limestone can be used to create steel by using it in a blast furnace.
Yes, in some cases, limestone is used in drainage of harappan civilization. The main channels were made of bricks set in mortar and were covered with loose bricks that could be removed for cleaning.
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.
If too much limestone dissolves in an underground cave, it can weaken the structural integrity of the cave and lead to collapse or sinkholes. This process is known as karstification and can occur over a long period of time as water continuously dissolves the limestone rock.
Caves and sinkholes are formed when limestone is dissolved by underground water, creating underground spaces. Karst topography, characterized by these features, is a landscape formed by the dissolution of soluble rocks like limestone.