Crystal Onyx Cave

Crystal Onyx Cave

We're not Mammoth, but we are Spectacular!

Diagram of local geologic formations

Crystal Onyx Cave shares the same geology with Mammoth Cave. The sandstone cap has protected the cave from being dissolved by carbonic acid.

Knob deposition

Prewitts Knob is the pink spot in the center of this map.  Cave City is to the north and Mammoth Cave to the west.  The map shows the Big Clifty limestone in pink, Girkin in light green, St. Genevive in gray-green and St, Louis in green.  It shows how the knob stands alone above the Pennyroyale Plateau.  Caves are the rule in limestone, rather than the exception.

The limestone was deposited in layers hundreds of feet thick from 350 to 320 million years ago.  It is made of animal shells, bones, coral, and calcite precipitates called “oolites”. We were a shallow sea near the equator, but continental drift caused us to move northward and rise above sea level.  The Big Clifty sandstone cap was deposited on top of the limestone. The cap protected Crystal Onyx and others from being eroded away.

Cave Chemistry

Water in the air and flowing through soil picks up carbon dioxide and forms carbonic acid. That is the carbonation that gives soda pop its fizz.  It very effectively dissolves calcite, including limestone, animal shells, teeth and bones. Water gets saturated with calcium and when it is exposed to air can’t hold as much so gives it up to make our beautiful secondary cave formations.  Stalactites start as “soda straws” where the drip leaves a small ring of calcite before it falls to its mate stalagmite below.  Once the straw is clogged, the water either flows down from the top or is pushed out of the formation.  That creates a rough surface known as “cave coral”. Flow stone is formed when water flows over surfaces in sheets.  Draperies are made when the water flows as drips down a knife edge, leaving a bit of calcite along the way.

The underground river.

Millions of years ago, there was a river flowing atop the Big Clifty sandstone.  It found a hole and entered the underlying limestone.  There it started dissolving the limestone, and relocated below the surface.  Our entry sink hole is one place the water entered, also the sink hole located along the Lake Trail.  

As we continued to be raised above sea level, the water table dropped, and the river dug lower into the limestone, ending at the lake level.  Here it found another path and abandoned the tunnel. It ended up below to carve the Palace Room. Subsequent deposits of flow stone closed up the water channels.

Once the cave was exposed to air, the water couldn’t hold as much calcium and it started to be deposited as our beautiful secondary formations.

This an interactive 360 view of the Moon Room. You can see the “moon milk” on the ceiling, an old light fixture from the 60s, and where stalactites have been broken and are now regrowing soda straws.

Close Menu