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Devil's Bath Cenote EarthCache

Hidden : 3/12/2011
Difficulty:
2 out of 5
Terrain:
2 out of 5

Size: Size:   large (large)

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Geocache Description:

A cenote is a sinkhole with exposed rocky edges that also contains groundwater. Devil's Bath is the only cenote in Canada, and it connects to the Benson River Cave via an underwater tunnel. Devil's Bath is found in the Quatsino Formation limestone deposits, which contains almost 1000-plus karst formations and cave systems. Karst formations occur by the dissolution of a layer or layers of soluble bedrock, usually carbonate rock such as limestone or dolomite.

To log this earthcache, you are going to have to e-mail me the answers to the following questions and post the optional photo(s). Information for the questions can be found on the cache page, and at the Earth Cache location.

1) What is the approximate width of Devil's Bath and distance from the ground surface to the water?

2) What type of rock would the walls of Devil's Bath most likely consist of? (igneous, sedimentary, or metamorphic)

3) Do you notice any rock overhangs around the circumference of the sinkhole?

4) Why do you think Devil's Bath is full of water, and not dry like some sinkholes can be?

5) What type of cenote do you think Devil's Bath is? (see cache page for information)

6) Also, you can take a photo of yourself with Devils Bath in the background and submit it when you log the Earth Cache if you want to share your adventure with others.

Bonus Question: Using your values from question 1, calculate the approximate volume of rock that would have been dissolved to make Devil's Bath.

Cenote

Cenotes are surface connections to subterranean water bodies. Cenote water is often very clear, as the water comes from rain water infiltrating slowly through the ground, and therefore contains very little suspended particulate matter. In many cases, cenotes are areas where sections of cave roof have collapsed revealing an underlying cave system.

Cenotes are formed by the dissolution of rock, and the resulting subsurface void results in the collapse of the rock ceiling above the void. The rock that falls into the water below will eventually also be slowly dissolved, which makes space for more rock to collapse into the void. Cenotes may be fully collapsed creating an open water pool, or only partially collapsed with a rock overhang above the water.

Types of Cenotes

A simple classification system for cenotes exists:
Jug, or Pit cenotes are those with a surface connection narrower than the diameter of the water body.
Cylinder cenotes are those with strictly vertical walls.
Basin cenotes are those with shallow water basins.
Cave cenotes are those having a horizontal entrance with dry sections.

Information Sources

http://en.wikipedia.org/wiki/Cenote
http://www.infohub.com/TRAVEL/SIT/sit_pages/11425.html
http://www.stormchaser.ca/Caves/BC_Caving/Vancouver_Island_Caves_2007.html

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