A sinkhole, also known as a sink, shake hole, swallow hole, swallet, doline or cenote, is a natural depression or hole in the surface topography caused by the removal of soil or bedrock, often both, by water. Sinkholes may vary in size from less than a meter to several hundred meters both in diameter and depth, and vary in form from soil-lined bowls to bedrock-edged chasms. They may be formed gradually or suddenly, and are found worldwide. These terms are often used interchangeably though many will distinguish between those features into which a surface stream flows and those which have no such input. Only the former would be described as sinks, swallow holes or swallets.
Sinkholes form on the surface because material below the surface has been removed by mining extraction or occurred naturally from dissolution of carbonate rock by naturally acidic water. At some point, the force of gravity can cause a collapse of the ceiling of the cave or shaft, creating a sinkhole on the surface.
Sinkholes are formed when the supporting water table runs dry and the ground no longer has this strata to stand on. This happens in the states of Florida and Georgia in the US because they have more underground rivers than most. The ground simply collapses down the now dry rivers that were once filled with water. These are the first real signs of a major drought.
When an underground cavity enlarges to the point that its ceiling can no longer support the weight of overlying sediments, the earth suddenly collapses into the cavity. A circular hole typically forms and grows over a period of minutes to hours. Slumping of the sediments along the sides of the sinkhole may take approximately a day's time to stop. Erosion of the edge of the sinkhole may continue for several days, and heavy rainfall can prolong the stabilization. In the less catastrophic cover subsidence type of sinkhole, a bowl-shaped depression forms at the surface, typically over longer periods of time (sometimes as long as years).
I'm not actually sure but i think some can be from 4 feet two maybe at least 100 feet
It can form in seconds.
They don't. Sinkholes are filled in.
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.
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
its called KARST TOPOGRAPHY
A type of landscape that features caves, deep valleys, and sinkholes is called a karst landscape. Karst landscapes are formed when soluble rocks such as limestone or dolomite are eroded by water, creating unique underground drainage systems and surface features.
You can find sinkholes in fl
sinkholes mostly happen at FLORIDA
Sinkholes, as we know it, can affect anyone.
They don't. Sinkholes are filled in.
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.
Karst landscape is a type of landscape where caves, deep valleys, and sinkholes are common. This type of landscape is formed by the dissolution of soluble rocks such as limestone, dolomite, or gypsum by groundwater. The result is distinctive topographical features like caves, sinkholes, and underground drainage systems.
Sinkholes are perminant but usually get filled in with debrie or dirt. Also sinkholes can become small ponds depending on the size.
The landscape you are referring to is likely characterized by karst topography. Karst landscapes are formed by the dissolution of soluble rocks such as limestone, creating features like caves, deep valleys, and sinkholes. These areas often have unique water drainage systems, as water flows underground through the porous rock layers.
Sinkholes could be prevented, but not without huge expenditures of money.