Additional Information for Falling Waters State Park
Resources
A sinkhole is created when rainwater containing weak acids (derived from carbon dioxide and organic material) seeps down through cracks in the limestone. The acid slowly dissolves away the limestone, creating caverns. Occasionally, the surface over a cavern will collapse; and a sinkhole is formed. Usually, it is a funnel-shaped depression which is less striking than the smooth-walled "chimney" of Falling Waters. The sinkholes here were designated in May 1980 as a State Natural Feature. An overlook platform provides an excellent view of the waterfall and sink. In addition to the main sink, the hilly terrain is honeycombed with other limestone sinks visible from the boardwalk.
The fall’s flow is dependent upon the uplands watershed. Consequently, during dry periods, the water flow will decrease dramatically.
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