Larger cracks, usually. From chemical weathering of the limestone by slightly acidic rainfall.
Limestone erodes with water. Limestone can also erode through water getting in to the cracks and then freezing. This causes the crack to expand and will begin to erode the limestone.
Mainly through expansion of cracks and fissures from frost expansion which leads to further and deeper cracks and fissures. Plant roots seeking moisture may extend roots into limestone cracks and fissures, prying the rock apart.
When run-off water from rain, lakes, homes, rivers and other forms of water pass through the limestone it causes potholes to form in the limestone regions.
Rainfall that seeps through cracks in the bedrock is slightly acidic. The acid reacts with the calcium carbonate in the limestone, causing dissolution of the rock.
The potholes and caverns formed in limestone by water seeping through limestone bedrock is an example of such weathering.
Limestone caves are formed through a process called chemical weathering. Rainwater, which is slightly acidic, dissolves the limestone rock over time, creating small cracks. These cracks then widen as more water flows through, eventually forming caves. Additionally, some limestone caves are formed through the erosion of underground rivers.
Limestone erodes with water. Limestone can also erode through water getting in to the cracks and then freezing. This causes the crack to expand and will begin to erode the limestone.
the beds have cracks and fissures in them
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.
Mainly through expansion of cracks and fissures from frost expansion which leads to further and deeper cracks and fissures. Plant roots seeking moisture may extend roots into limestone cracks and fissures, prying the rock apart.
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When run-off water from rain, lakes, homes, rivers and other forms of water pass through the limestone it causes potholes to form in the limestone regions.
Rainfall that seeps through cracks in the bedrock is slightly acidic. The acid reacts with the calcium carbonate in the limestone, causing dissolution of the rock.
Aquifers are formed when water chips away at the limestone causing holes to appear. The water then flows through the holes making them bigger.
Th water escapes through cracks in the ocean floor called hydrothermal vents.
Th water escapes through cracks in the ocean floor called hydrothermal vents.
The potholes and caverns formed in limestone by water seeping through limestone bedrock is an example of such weathering.