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Crystal Geyser

A cache by Baldin' Eagle Send Message to Owner Message this owner
Hidden : 04/28/2008
1.5 out of 5
2.5 out of 5

Size: Size: not chosen (not chosen)

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Geocache Description:

Crystal Geyser, a cold water, CO2 geyser

Crystal Geyser

Cold Water Geysers are normally man-made, where a hole is drilled through a confining layer into a CO2-laden aquifer. The borehole provides a path for the pressurized water and CO2 to reach the surface. Only in a handful of places, such as at faults, joints, or drilled wells, can the water and CO2 readily escape the underlying aquifer. Aquifer and plumbing attributes, including plumbing depth, CO2 concentrations, aquifer yield, and so on, combine to provide the differing scales and frequencies of eruptions.

In the same way that steam bubbles expand to displace water in a hot water geyser, the column of water in a cold water geyser is pushed up by the expanding of CO2. This "boiling" deep in the system is comparable to water flashing to steam in a hot water geyser. As the CO2 out-gasses, it displaces water and starts the eruption.

At Crystal Geyser, in southeast Utah, after a geyser eruption, the geyser vent is calm and the water level is below the surface; like many cold water geysers, Crystal Geyser is a drilled well and was unintentionally created in the 1930s while drilling for oil. As time passes, water begins to fill the well column. The well itself penetrates a confined aquifer with a hydraulic head above the level of the ground surface, thus the well, if not for the geyser-like behavior, the well would be expected to possess artesian discharge. When CO2 and water make it to the surface, CO2 degassing manifests as increasingly agitated boiling at the vent. Each of these agitations causes a pressure release for the CO2 below in the plumbing. Eventually, one of the agitated boils is large enough to create a chain reaction of CO2 degassing and expansion down the well: an eruption.

In summary, CO2 and water are competing to get out of the ground and the effect with limited, small openings, is occasional eruptions. Aquifer and plumbing attributes (like plumbing depth, CO2 concentrations, depth to confined aquifer, aquifer yield, etc.) combine to provide the differing scales and frequencies of eruptions.

To log this cache you must visit this site and answer the questions by sending me an email (please do not post answers, they will be deleted) and post a photo of the geyser.
1. What is the texture of the ground covered by the geyser water?
2. What is the temperature of the water?

If you witnessed an eruption, describe what you saw.

While posting a photo of the geyser, include whether the geyser erupted while you were there, and if so, what time of day was it?

  • Crystal Geyser is the largest cold geyser in the world.
  • The geyser erupts sometimes to a height of 40 meters or more. During 2005, a study of the timing of the eruptions found them to be bimodal with about 66% of the eruptions about 8 hours after the previous eruption, and the rest about 22 hours after.
  • The current form of the geyser was created by an exploration well drilled circa 1930 in attempt to locate oil. A large diameter pipe was installed in the 1990s to prevent people from falling into the well after the well known story of Jessica McClure.
  • The first written record of Crystal Geyser comes from the report of the John Wesley Powell river expedition, July 13, 1869:
  • For more information about Cold Water Geysers, see: Glennon, J.A. and Pfaff. R.M. (2005) The operation and geography of carbon-dioxide-driven, cold-water geysers. GOSA Transactions, vol. 9, pp. 184-192.

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Coordinates are in the WGS84 datum

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