A sinkhole that develops over a period of hours or days and forms from a collapse through the roof of an underground cavern is known as a

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A collapse sinkhole forms gradually as the roof of an underground cavern weakens and eventually collapses, whereas solution sinkholes form more slowly over time as acidic groundwater dissolves the rock beneath the surface. Dolines are another type of sinkhole that can form from the dissolution of limestone or other soluble rocks, but they typically have a more gradual formation process and are not necessarily associated with the collapse of an underground cavern. Karst valleys and towers are also features of karst landscapes, but they are not specifically related to sinkhole formation.

A Sinkhole That Develops Over a Period of Hours or Days