How Are Caves Decorated?
As slightly acidic water passes through limestone, it dissolves away calcite, a portion of the calcium carbonate rock, and carries it in solution. When a super-saturated water droplet enters a cave a chemical reaction takes place. The CO2 dissolved in the water, which formed dissolved H2CO3, comes out of solution. The water becomes less acidic (lower pH), and the calcite (CaCO3) previously held in solution is deposited in formations called speleothems.
There are several types of speleothems. Flowstone forms as water flows over walls, floors, or other formations and builds up sheets of calcite that look like a rock waterfall. Stalagmites rise upward from the floor of the cave passage and are usually formed by water dripping from ceiling. Stalactites hang from the cave ceiling and form as water flows down the formation deposits layers of calcite. You can remember the difference between stalagmites and stalactites by remembering that stalactites cling “tight” to the ceiling. When a stalactite and a stalagmite join they form a column.
In general, all ceiling formations are stalactites, but because there are so many distinctive types, there are more specific terms. For instance, a drapery develops when water deposits calcite in thin sheets that hang in delicate folds like a curtain. The tiny, hollow stalactites known as soda straws are particularly fascinating. They grow as water runs down inside them and deposits a ring of calcite at the tip. Helectites, or delicate, twisted speleothems, form as air movement within particularly humid cave passages causes the calcite formations to project at odd angles from the ceiling or walls of caves. They have a curving or angular form that makes them look like they formed in zero gravity.
Why Are Speleothems Useful?
Speleothems are not only beautiful, they’re useful, too. Examining the location of speleothems within a cave can help explain how the cave formed. A cluster of soda straws on the cave ceiling can indicate diffuse flow—where water passes through the rock. A long, sinuous drapery hints at fracture flow—when water flows through cracks in the rock. Even the color and composition of the speleothems can be informative. It suggests what types of rocks and minerals exist along the recharge flow path.
As the speleothems grow, they record atmospheric information such as climatic conditions and ocean levels. Scientists at the University of Texas have found speleothems in central Texas caves that are more than 350,000 years old (Musgrove, 2000). Growth rates are hypothesized to correlate to rainfall: the more rainfall the faster the formations grow. By examining growth rates scientists are able to reconstruct regional climactic conditions (Musgrove et al., 2001).
Banner, J. L., Guilfoyle, A., James, E., Stern, L. A. and Musgrove, M., 2007, Seasonal variations in modern speleothem calcite growth in Central Texas, U.S.A. Journal of Sedimentary Research 77, 615-622.
Musgrove, M., 2000, Temporal Links Between Climate and Hydrology: Insights from Central Texas Cave Deposits and
Groundwater, unpublished Ph.D. Dissertation, University of Texas, Austin, TX, 432p.
Musgrove, M., Banner, J.L., Mack, L.E., Combs, D.M., James, E.W., Cheng, H., and Edwards, R.L., 2001, Geochronology
of late Pleistocene to Holocene speleothems from central Texas: implications for regional paleoclimate: Geological
Society of America Bulletin, v. 113(12), p. 1532-1543.
Through UT’s former UTOPIA program, ESI developed this cave resource. We hope you find it useful!