The type or more accurately, age and lithology, of the limestone does not influence cave development within it significantly, though its structure will.
CALCITE, the mineral Calcium Carbonate, is deposited in caves as Stalactites, Stalagmites and related formations, having been dissolved from the limestone above.
The original answer said Travertine, but although that is the same mineral, it is a form deposited in the open air.
The type of limestone typically found in caves is called "travertine." It forms when water containing dissolved calcium carbonate drips from the cave's ceiling or walls and deposits as mineral coatings, creating various cave formations such as stalactites and stalagmites. These formations give caves their unique and intricate features.
Limestone is the type of rock that is commonly found in areas with a lot of caves. Limestone is made of calcium carbonate, which is soluble in water. Over time, as rainwater seeps into the ground, it dissolves the limestone and creates openings and caves in the rock.
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.
Most caves are found in areas with limestone bedrock, as it is easily dissolved by water, creating caves through a process called karst topography. These areas include regions like Kentucky in the United States, parts of China, and the Yucatan Peninsula in Mexico.
Limestone caves are common because limestone is a soluble rock that dissolves easily in water. Over time, groundwater flowing through cracks in the limestone gradually enlarges these passages to form caves. Additionally, limestone is often found in areas with karst topography, characterized by sinkholes, underground rivers, and other features that promote the formation of caves.
The rocks around Jenolan Caves are predominantly limestone, formed from ancient marine sedimentation. These rocks exhibit distinctive features such as cave formations due to the erosion by underground water over millions of years. Additionally, there are also dolomite and shale rocks present in the area surrounding the caves.
Limestone is the type of rock that is commonly found in areas with a lot of caves. Limestone is made of calcium carbonate, which is soluble in water. Over time, as rainwater seeps into the ground, it dissolves the limestone and creates openings and caves in the rock.
STALAGMITES
Most caves are found in areas with limestone bedrock, as it is easily dissolved by water, creating caves through a process called karst topography. These areas include regions like Kentucky in the United States, parts of China, and the Yucatan Peninsula in Mexico.
They usually grow from limestone. Mostly in caves.
It's found around them! The vast majority of the world's caves are formed in limestone (soluble in ground-water).
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.
Yes. There are substantial limestone beds in Israel. The Dead Sea Scrolls were found in limestone caves there.
It depends on the cave. Since many caves are limestone (water carves it nicely), you usually find limestone. But granite is common in New Hampshire & Vermont.
I think I know what you mean.The vast majority of the world's caves are formed in limestone by water dissolving the calcium carbonate that is the rock's main constituent. As for "type", well, almost any "type" by age or source of limestone physically capable of supporting itself above the developing void. Caves will also form in marble (metamorphosed limestone) and in gypsum (calcium sulphate), in the same way.So the limestone is not "often found in caves" - except as boulders that fallen from the roof, or re-precipitated as calcite stalactites etc - but is literally all around almost all caves!More to the point perhaps is the combination of factors that encourage or discourage caves to form in a given limestone area, and that is far more complex.
Limestone.
Karst caves (i.e. dissolutional features in limestone).
bacteria. +++ Ambiguous question - not clear if it means within pores in the surface of the rock or in cavities and caves.