Blowhole (geology)
In geology, a blowhole is formed as sea caves grow landwards and upwards into vertical shafts and expose themselves towards the surface, which can result in blasts of water from the top of the blowhole[1] if the geometry of the cave and blowhole and state of the weather are appropriate.
A blowhole is also the name of a rare geologic feature in which air is blown through a small hole at the surface due to pressure differences between a closed underground system and the surface. The blowholes of Wupatki National Monument are an example of such a phenomenon. It is estimated that the closed underground passages have a volume of at least seven billion cubic feet. Wind speeds can approach 30 miles per hour.[2] Another well known example of the blowhole is the natural entrance to the Wind Cave[3]
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Blowholes, north coast of Barbados
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Nakalele blowhole, located near Nakalele Point in north western Maui, Hawaii.
References
- ↑ Bell, F. G.; Frederic Gladstone Bell (2007). Engineering geology. Elsevier. p. 140. ISBN 978-0-7506-8077-6.
- ↑ Sartor, James Doyne; Lamar, D. L. (1962). Meteorological-Geological Investigations of the Wupatki Blowhole System. Santa Monica, CA: RAND Corporation. OCLC 22486021.
- ↑ Rodney D. Horrocks and Bernard W. Szukalski; Using geographic information systems to develop a cave potential map for Wind Cave, South Dakota; Journal of Cave and Karst Studies 64 (1): 63-70.
