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Cave Fissure
cave fissure
The holes in the ceiling are called solution domes. These are rare formations because of the unique circumstances that are required. First the stone of the cave must be dissolved to form a cave or hollow chamber. The cave would then fill with water and the water would be forced up into the cracks. When the water starts to seep up the fissures and dissolve the rock the fisure will enlarge where the water is traveling, causing a circular or oval hole in the rock layer.
cave fissure
stalactites cave fissure

flowstone stalactite
cave formation
cave formation
 
 
drapery
The curtain at left is below what used to be a stalactite. The top of it has been broken off, not by humans because it was like this when Joe Petty first discovered it. One popular explaination is that the large concentration of iron in the calcite that expanded when wet and shrinks when dry caused the top to crack and fall away. The photo a the right shows stalactites that are mostly growing straight down but one is growing at an angle. Notice the more red color, indicating increased amounts of iron.  This expansion and contraction could be responsible for the tilt of this stalactite.
stalactites
Formations above of stalactites (cone shaped stone formed by water running down the formation), stalagmites ( cone shaped stone formed at the floor from water dripping down from above), columns (where stalactites and stalagmites 'grow' together), draperies sometimes called ribbons (above left where water flows down at a steep angle forming what looks like the edge of a drape for a window) and flowstone (formed when water flows slowly over a rather flat area) take hundreds or even thousands of years to form as they have here in the cave.

Many of the passages are too small for people to fit through. There is a great possibility that additional large cave areas lye beyond these small passages.
joint

 
 
 
 

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