A special sight in any cave are the strange and one-of-a-kind formations known as speleothems!
Fragile and Slow
Both the calcite and gypsum formations in Mammoth Cave took thousands of years to form. In addition, many formations are incredibly fragile and can break or be forever damaged by a simple touch of the hand. Some of the park caves have been looted of their formations by past visitors looking to sell them for a profit. This destruction has forever robed us of seeing these sections of cave in their full beauty as the damage cannot be reversed within our lifetimes.
Stalagmites, Stalactites and Columns
Stalagmites and stalactites are some of the best known cave formations. They are icicle-shaped deposits that form when water dissolves overlying limestone then re-deposits calcium carbonate along the ceilings or floors of underlying caves.
Other Calcite Formations
Depending on how water flows in a cave, many unique shapes and formations are possible.
Flowstone refers to sheets of calcium carbonate that form along cave walls. Flowstone hangs downward and may create curtain-like sheaves along ledges, better known as draperies. The most notable flowstone formation in Mammoth Cave is the Frozen Niagara.
Helictites form in cave areas with minimal water seepage. Because water does not drip off of the helictite, as would happen with a stalactite, the water coats its surface creating strange, branch-like shapes. Helictites can be seen along the Great Onyx Lantern Tour.
Cave Popcorn refers to knobs of calcite that form where water seeps through pores in limestone, creating clusters that resemble popcorn, peas, or grapes. Cave Popcorn can be seen along the Grand Avenue and Domes and Dripstone Tour.
Rimstone dams form along floors where calcite rich water pool. These dams grow larger as more calcite is deposited and water continues to flow over the edge of the dam. Rimstone dams can be seen in the Frozen Niagara section.
Prehistoric American Indians utilized minerals from Mammoth Cave about 2000-3000 years ago. They came in and collected gypsum, epsomite, and mirabilite from the walls and sediments of the cave.
Gypsum is a mineral that forms in the dry areas of the cave. It is a calcium sulfate mineral that is soluble in water. It is most commonly seen as delicate white crystal found along tour routes such as Cleveland Avenue and Kentucky Avenue. Along Broadway in historic section of Mammoth Cave you can also see gypsum, but it is covered with a dark coating (so it looks dark brown instead of white).The coating on this gypsum is from smoke from the torches that people used in the cave 2000 – 3000 years ago. This discoloration can be seen particularly well near Giant’s Coffin and the historic Tuberculosis Huts. Gypsum will also grow as crystals in the dirt along some cave passages.
Types of Gypsum Formations
Crusts — Crusts are where gypsum lines the walls as thin (or sometimes thick) plate covering (actually extruding from) the limestone. Crusts are common along the Historic Tour, Grand Avenue, and Great Onyx routes.
Mirabilite and Epsomite
Mirabilite and Epsomite are two other minerals that occur in dry sections of the cave. They can form in areas in the winter (when the air is drier) and dissolve away when more humid air comes in. They form a sprinkling on the floor that gives the Snow Room on the Lantern Tour its name.
Last updated: April 16, 2021