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Sinkholes can be classified on the basis of the processes by which they are formed: dissolution, cover-subsidence, and cover-collapse. Formation of sinkholes can be accelerated by intense withdrawals of groundwater over short periods of time, such as those caused by pumping for frost-protection of winter crops in west-central Florida.
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Citrus County, Florida location Florida during the Pleistocene. The Inglis quarry or Inglis quarry sites 1A and 1C are assemblages of vertebrate fossils dating from the Pleistocene ~1.8 Mya—300,000 years ago, located in the phosphate quarries near the town of Inglis, Citrus County, northern Florida.
The map above shows areas of the U.S. with bedrock types that are prone to sinkholes. It's not just Florida that needs to worry about them. Think sinkholes like the one that opened up under a ...
Citrus County is a county located on the northwest central coast of the U.S. state of Florida. As of the 2020 census, the population was 153,843. [1] Its county seat is Inverness, [2] and its largest community is Homosassa Springs. Citrus County comprises the Homosassa Springs, Florida Metropolitan Statistical Area. [3]
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Little Salt Spring is a feature of the karst topography of Florida, specifically an example of a sinkhole.It is classified as a third magnitude spring. [4] The numerous deep vents at the bottom of the sinkhole feed oxygen-depleted groundwater into it, producing an anoxic environment below a depth of about 5 m (16.4 ft). [4]