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.
They don't. Sinkholes are filled in.
do not know and do not care
Michigan is a state that is very familiar with sinkholes. On their lower peninsula alone there are close to 200 sinkholes.
subsidence sinkholes are different from collapse sinkholes in two ways . first,subsidence sinkholes ocer when there is almost no overburn,or material,above the limestone. collapse sinkholes happen when there is thick overburn. secondly, subsidence sinkholes occur slowly, over time, while collapse foms quckly beacause of human activity , such as well drilling.
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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.
5
sinkholes mostly happen at FLORIDA
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Sinkholes are perminant but usually get filled in with debrie or dirt. Also sinkholes can become small ponds depending on the size.
Sinkholes could be prevented, but not without huge expenditures of money.
a subsidence sink hole they are in common with two other types of sinkholes called solution and collapse sinkholes they have in common thick dirt
The Yucatan Peninsula. These "sinkholes" are called "cenotes" over there.
Sinkholes cause flooding, underground system damage, building damage, and human casualties.
many people died
Sinkholes comes from expansion of dissolution hollows formed from action of water on bottoms of limestone formations.