Cave Deposits

Beautiful mineral deposits occur in some natural caves. Deposits that

look like icicles, called _stalactites_, are found hanging from the

ceiling of a cave. Other deposits, _stalagmites_, are like the

stalactites except that they jut upward from the floor. _Columns_ are

formed from stalactites and stalagmites that have joined together. In

addition, some caves contain sheet-like deposits that are spread along

the ceiling, floor, and walls. These deposits are called _flowstone_.

Calcite is one of the minerals that commonly form cave deposits.

Just a few of the caves in Texas contain these deposits. They occur

mostly in the limestone rocks that are south and southwest of the Llano

uplift area of central Texas. Some of the commercial caves that contain

good examples of calcite deposits are located near Boerne in Kendall

County and near Sonora in Sutton County. Calcite deposits also occur in

Longhorn Cavern, a large cave located in the Longhorn Cavern State Park

of Burnet County. These caves were formed by underground waters that

moved through cracks and pores in the limestone rocks and dissolved

passageways in them. After the cave passages were made, water containing

dissolved calcium carbonate dripped into the cave. As it evaporated,

this water left behind a deposit of calcium carbonate—the mineral

calcite.

You can better understand how the cave deposits are formed by watching

icicles grow in wet, freezing weather. First, small hanging drops of

water freeze, and a small icicle forms. Then, as more water drips over

it and freezes, the icicle grows longer and wider. Some of the water

drips completely over the icicle and falls to the ground. There, it

either freezes into a sheet of ice, or it begins to build upward to form

an upside-down icicle. The water dripping down in the caves evaporates

instead of freezing, and in doing so it leaves behind a deposit of

calcite.

[Illustration: Calcite stalactites and stalagmites in the Caverns of

Sonora, Sutton County, Texas. Photograph courtesy of the Travel and

Information Division of the Texas Highway Department.]

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