Dean's Blue Hole
A blue hole is a water-filled sinkhole with the entrance below the water level. They can be formed in different karst processes, for example, by rainwater soaking through fractures of limestone bedrock onto the watertable. Sea level here has changed: for example, during the glacial age during the Pleistocene epoch (ice age), some 15,000 years ago, sea level was considerably lower.
Dean's Blue Hole is roughly circular at the surface, with a diameter ranging from 25 to 35 metres (82–115 ft). After descending 20 metres (66 ft), the hole widens considerably into a cavern with a diameter of 100 metres (330 ft).
There are several fresh water sinkholes on land that are deeper than Dean's Blue Hole. These include the 270 m (890 ft) Boesmansgat in South Africa, Mexico's Zacatón at 335 m (1,099 ft) and the 392 m (1,286 ft) Pozzo del Merro in Italy.
||This article includes a list of references, related reading or external links, but its sources remain unclear because it lacks inline citations. (June 2016) (Learn how and when to remove this template message)|
- Wilson, William L. (1994). "Morphometry and Hydrology of Dean's Blue Hole, Long Island". Bahamas Journal of Science. 2 (1): 10–14. Archived from the original on 7 March 2012.