John Alan Glennon

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John Alan Glennon (born September 24, 1970) is an American geographer and explorer. His work has been mapping and describing caves and geysers.

Contents

Discoveries and research

Caves

In 1996, Glennon and Jon Jasper discovered an entrance to the Martin Ridge Cave System, Kentucky, and explored connections to nearby Jackpot and Whigpistle Caves (Groves, C.G. 1998). The combined cave system is 51 kilometers (32 mi) long (Gulden, B. 2005). The cave is hydrologically connected to Mammoth Cave---the world's longest cave (Quinlan J.F. and Ray, J. 1989). Glennon also was involved in the discovery of one of the largest cave chambers in Kentucky (Yonker, R. 2003).

Geysers

In 2002, Glennon led an American expedition to El Tatio Geyser Field, Chile. The team produced the first comprehensive inventory and description of the geysers' behaviors. The resulting report concluded that the site was the world's third largest geyser field (Glennon, J.A. and Pfaff, R.M. 2003).

Hoffman Environmental Research Institute (HERI)

With Dr. Chris Groves, president of the Cave Research Foundation (2004-2006), Glennon cofounded HERI in 1999. The Institute's mission is to study the environmental and geologic aspects of caves and karst landscapes. Headquartered at Western Kentucky University, HERI's major scientific focus has been on the karst issues of China.

Background

Glennon was a geography Ph.D. student of Dr. Michael Frank Goodchild at the University of California, Santa Barbara and received his PhD in 2013. Goodchild is a pioneer in Geographic Information Science and discoverer of Castleguard Cave, Canada's longest cave. Glennon received a Master of Science in Geoscience from Western Kentucky University, 2001, and Bachelor of Science in Park Administration from Texas A&M University, 1994.

For his cave discoveries in Kentucky, Alan has been commissioned in the Honorable Order of Kentucky Colonels.

Works authored

Articles

Related Research Articles

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Floyd Collins 1925 American cave explorer death

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Cold-water geyser

Cold-water geysers have eruptions similar to those of hot-water geysers, except that CO
2
-bubbles drive the eruption instead of steam from the proximity to magma. In cold-water geysers, CO
2
-laden water lies in a confined aquifer, in which water and CO
2
are trapped by less permeable overlying strata. This water and CO
2
can escape this strata only in weak regions like faults, joints, or drilled wells. A drilled borehole provides an escape for the pressurized water and CO
2
to reach the surface. The magnitude and frequency of such eruptions depend on various factors such as plumbing depth, CO
2
concentrations, aquifer yield etc. The column of water exerts enough pressure on the gaseous CO
2
so that it remains in the water in small bubbles. When the pressure decreases due to formation of a fissure, the CO
2
bubbles expand. This expansion displaces the water and causes the eruption. Cold-water geysers may look quite similar to their steam-driven counterparts; however, often CO
2
-laden water is more white and frothy. The best known of these are probably Saratoga Springs, New York, or Crystal Geyser, near Green River, Utah. There are also three cold-water geysers in Germany, named Wallender Born, Wehr Geyser and Andernach Geyser ; two in Slovakia, one in the village of Herľany and a very small one in Sivá Brada; and one in Brazil, in the municipality of Caxambu.

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