i dint know.
Limestone caves are sometimes called solution caves because they are formed through a process called solution weathering. This occurs when water containing carbon dioxide dissolves the limestone rock, creating cave systems over time. The dissolved limestone is carried away in the form of a solution, hence the term "solution cave."
Swallow holes, or sinkholes, in limestone areas of the Caribbean are formed through a process called chemical weathering. Rainwater, which is slightly acidic due to dissolved carbon dioxide, seeps into the ground and reacts with the limestone, gradually dissolving it. Over time, this dissolution creates underground voids and cavities. When the roof of these cavities collapses, it results in the formation of a swallow hole on the surface.
Limestone caves at Carlsbad Caverns were formed through a process known as chemical weathering, primarily involving the dissolution of limestone by slightly acidic water. Rainwater absorbs carbon dioxide from the atmosphere and soil, forming a weak carbonic acid that seeps into the ground. As this acidic water flows through cracks in the limestone, it gradually dissolves the rock, creating cavities and passages over millions of years. This process, combined with the subsequent erosion and the formation of stalactites and stalagmites, has shaped the stunning caverns we see today.
It's found around them! The vast majority of the world's caves are formed in limestone (soluble in ground-water).
Caverns are formed when rain, run-off, or surface water mixes with the topsoil, then Carbon acid and Carbon Dioxide mix with the soil where plants grow, making an acid so powerful that it eats away at the limestone that is underground; making cracks. Over millions of years, this process makes caves, which also concludes that caves are made up of lots of other caves.
Limestone is formed in caves through a process called cave formation or speleogenesis. This occurs when water containing dissolved minerals, like calcium carbonate, seeps through cracks in the rock and evaporates, leaving behind deposits of limestone. Over time, these deposits can accumulate to form intricate cave structures.
They don't! Deposits don't form caves, but limestone is a sedimentary rock formed from marine or lacustrine deposits. Caves form within limestone by dissolution of its calcium carbonate by ground-water flowing through the rock's joints, bedding-planes and faults.
Carbonic acid can dissolve limestone, a common rock type in many regions, which then forms caves through a process of chemical weathering. When rainwater, containing carbon dioxide from the atmosphere, seeps through the ground and comes into contact with limestone rocks, it forms carbonic acid. This carbonic acid slowly dissolves the limestone over time, creating cave systems underground.
Precipitation and crystallisation of calcite (calcium carbonate) from the ground-water that has dissolved it from the limestone above the cave.
Two features formed by underground weathering are caves and sinkholes. Caves are formed through the dissolution of limestone by groundwater, while sinkholes are created when the roof of a cave collapses, causing a depression on the surface.
Limestone, CaCO3 decomposes into quicklime, CaO, and carbon dioxide, CO2, when heated. The reaction is: CaCO3 + heat --> CaO + CO2.
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.