caverns
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.
Limestone is dissolved by carbonic acid through a process called chemical weathering. Carbonic acid forms when rainwater combines with carbon dioxide in the atmosphere or soil, creating a weak acid that gradually breaks down the calcium carbonate in limestone over time.
Acidic ground water (rain-water that has absorbed atmospheric carbon dioxide to form carbonic acid) forms caves by dissolving the limestone as it flows through the joints & other discontinuities in the rock mass.
Surface runoff that cannot penetrate the ground forms streams, rivers, or lakes.
When melted rock cools and hardens in or under the Earth's surface, it forms igneous rock. This process can happen above ground, forming volcanic rocks, or below ground, forming intrusive rocks.
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.
No. Stalactites are formed of limestone that is dissolved in slightly acidic ground water that precipitates and deposits a fraction of the dissolved limestone where the solution drips from the roof of a cavern to the floor. On the floor, below the stalactite, a stalagmite forms. The stalactite grows downward, and the stalagmite grows upward. This whole process requires a limestone cavern.
The primary one is calcite precipitated from the ground-water that had dissolved it from the surrounding limestone, and though the deposits themselves take various forms such as stalactites and stalagmites they are all still calcite formations.
Ground water I think you meant! It is slightly acidic, primarily from dissolved atmospheric CO2, so can dissolve limestone given enough time.
igneous rock and/or limestone
The forests that grows over the limestone forms mulch that produces the acid required. That's true but the prime solvent is Carbonic Acid: atmospheric carbon dioxide dissolved into rain-water.
caves
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.
No, limestone is a sedimentary rock that is the basis for marble if it is compressed by millions of years of pressure. Limestone consists of calcium carbonate, CaCO3. Limestone dissolved in slightly acidic water forms the basis of stalactites and stalagmites in limestone caves.
Limestone is dissolved by carbonic acid through a process called chemical weathering. Carbonic acid forms when rainwater combines with carbon dioxide in the atmosphere or soil, creating a weak acid that gradually breaks down the calcium carbonate in limestone over time.
Florida has a lot of porous limestone underneath the surface. It can hold lots of water in underground aquifers. As groundwater flows through the limestone, it forms an eroded landscape called karst, known for caves, springs and sinkholes.
Carbon dioxide dissolved in rain water forms a weak acid which slowly weathers limestone, a carbonate which reacts with acids.