Alabaster Caverns is served by a dedicated spur from the Oklahoma state highway system, State Highway 50A.
The underground site was created naturally around 200 million years ago when the area of what is now north-western Oklahoma was covered by an inland sea. A perennial stream now flows through the cave and is fed by various lateral tunnels and seepage from the roof. However, the stream was once as big as a river. The evidence of this can be seen in the obviously water-sculptured gypsum formations. According to geologists, the river was once capable of completely filling the 3/4 mile (1.2 km) long caverns.
The cavern is home to five different species of bat. Some are solitary while others are colonial. The cavern provides roosting sites that serve as daytime shelter and a place for the non-migrating bats to hibernate during the winter months. The Mexican Free-tailed Bat migrates to Alabaster Caverns from Mexico in the spring to bear their young. They then return to Mexico in the fall.
Bat species found in the cave include the Cave Myotis, Western Big-eared Bat, Eastern Pipistrelle, Western Big Brown Bat, and the Mexican Free-tailed Bat.