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Staircase Cave EarthCache

Hidden : 9/5/2008
Difficulty:
1 out of 5
Terrain:
3.5 out of 5

Size: Size:   not chosen (not chosen)

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Geocache Description:

Staircase Cave is located on the Birch Knob Section of Pine Mountain Trail. This cave is one of many rock formations on this section of the trail. This section of trail Traverses the Kentucky/Virginia State line.

A cave is a natural underground void large enough for a human to enter. Some people suggest that the term cave should only apply to cavities that have some part that does not receive daylight; however, in popular usage, the term includes smaller spaces like sea caves, rock shelters, and grottos.
The formation and development of caves is known as speleogenesis. Caves are formed by various geologic processes. These may involve a combination of chemical processes, erosion from water, tectonic forces, microorganisms, pressure, atmospheric influences, and even digging. Most caves are formed in limestone by dissolution. Solutional caves may form anywhere with rock that is soluble, and are most prevalent in limestone, but can also form in other material, including chalk, dolomite, marble, granite, salt, sandstone, fossilized coral and gypsum. The largest and most abundant solutional caves are located in limestone. Limestone dissolves under the action of rainwater and groundwater charged with H2CO3 (carbonic acid) and naturally occurring organic acids. The dissolution process produces a distinctive landform known as karst, characterized by sinkholes, sinking streams, and underground drainage. Limestone caves are often adorned with calcium carbonate formations produced through slow precipitation. This include: flowstones, stalactites, stalagmites, helictites, draperies, soda straws and columns. These secondary mineral deposits in caves are called speleothems. The world's most spectacularly decorated cave is generally regarded to be Lechuguilla Cave in New Mexico. Lechuguilla and nearby Carlsbad Caverns are now believed to be examples of another type of solutional cave. They were formed by H2S (hydrogen sulfide) gas rising from below, where reservoirs of oil give off sulfurous fumes. This gas mixes with ground water and forms H2SO4 (sulfuric acid). The acid then dissolves the limestone from below, rather than from above, by acidic water percolating from the surface. To claim this earthcache plese answer the following questions and include a picture of yourself in front of Staircase Cave with your GPS 1. Estimate the length of this cave 2. Estimate the size of the opening? 3. What do you think formed this cave. (The answer may be found in the cave)

Additional Hints (Decrypt)

Gur pbeqf jrer gnxra nccebk 30 srrg sebz gur zbhgu bs gur Fgnvepnfr Pnir qhr gb cbbe fvtany nebhaq gur ebpxf. Gur pnir bcravat znl or fyvtugyl uvqqra ol oehfu qhevat gur fhzzre zbaguf

Decryption Key

A|B|C|D|E|F|G|H|I|J|K|L|M
-------------------------
N|O|P|Q|R|S|T|U|V|W|X|Y|Z

(letter above equals below, and vice versa)