It is Carbolican weathering, not many people have heard of it but that is what it is called. Carbolican weathering is a rare kind of weathering that can be deadly, like sinkholes. Since not many people have heard of this weathering no one has come up with an explanation for when and why sinkholes will appear. This is very sad but true. As many fatal appearances happen we still try to figure out how to stop these sinkholes before they start.
Sinkholes are primarily formed by chemical weathering processes, specifically the dissolution of soluble rock such as limestone or gypsum by acidic water. However, physical weathering processes like erosion and the collapse of surface material can also contribute to sinkhole formation.
Erosion has the most impact on the formation of sinkholes. Sinkholes are typically formed when underground rock, such as limestone, is eroded by water over time, creating a void that can lead to the collapse of the surface layer into the empty space below. Deposition can also play a role in sinkhole formation by contributing sediments that fill in voids and stabilize the ground.
Weathering weakens the bedrock beneath the surface, making it susceptible to erosion. Water seeps into the cracks in the bedrock, dissolving it and creating underground caverns. Eventually, the roof of the cavern collapses due to gravity, creating a sinkhole.
Erosion typically has a greater impact on the formation of sinkholes than weathering. This is because erosion refers to the wearing away of rock and soil, which can create voids in the ground where sinkholes may form. Weathering, on the other hand, breaks down rocks and minerals but does not necessarily result in the formation of sinkholes.
Two features formed by underground weathering are caves and sinkholes. Caves are formed by the dissolution of limestone or other soluble rocks, creating underground chambers and passages. Sinkholes are depressions in the ground that form when the roof of an underground cavern collapses.
Sinkholes are primarily formed by chemical weathering processes, specifically the dissolution of soluble rock such as limestone or gypsum by acidic water. However, physical weathering processes like erosion and the collapse of surface material can also contribute to sinkhole formation.
Erosion has the most impact on the formation of sinkholes. Sinkholes are typically formed when underground rock, such as limestone, is eroded by water over time, creating a void that can lead to the collapse of the surface layer into the empty space below. Deposition can also play a role in sinkhole formation by contributing sediments that fill in voids and stabilize the ground.
When the rock above a cave collapses, it can form a sinkhole if the collapse creates a depression in the ground. This can sometimes lead to the formation of a sinkhole cave system underground.
Physical weathering
The 2 kinds of weathering are the Mechanical or Physical Weathering and the Mechanical Weathering.
physical weathering
Physical weathering
It is water weathering
Chemical weathering.
the sinkhole got bigger
Weathering weakens the bedrock beneath the surface, making it susceptible to erosion. Water seeps into the cracks in the bedrock, dissolving it and creating underground caverns. Eventually, the roof of the cavern collapses due to gravity, creating a sinkhole.
chemical weathering