Cave Formations

Up Cave Formations Arkansas Caves Cave Life Class Activities

Cave formations are deposits on the ceiling, floor, and walls of a cave. They are called speleothems.The creation of these formations depends upon the following:

bulletthe type of rocks in and around the cave
bulletthe dissolved materials contained in the water as it enters the cave, and
bulletthe cave environment -- amount of moisture in the air, amount of air flow through the cave, and the cave terperature.



Most caves have enough openings to allow air movement, which does evaporate some of the moisture and causes the precipitation of calcite and aragonite from the seeping waters. Nature creates formations in a cave very slowly. It may take one hundred to one hundred fifty years to form an inch of material to the speleothems. These speleothems may take the form of icicles, trees, statues, or the delicate design of lacy flowers. The coloration of these structures varies from white or cream, to yellowish or dark brown which is due to the presence of limonite that is dissolved from the overlaying rocks. The red and orange hue comes from dissolved iron mixing with water to form iron oxide. The blue is derived from manganese. "Cave onyx" is made up of a variety of calcite. It has a banded, rich brown appearance. Speleothems that are white are almost pure calcite. The color variations and the configurations of the cave’s gradual deposits create the beautiful wonderland of this under explored area of our earth.

Stalactites

mvc-015f.jpg (31940 bytes) Stalactites are the formations that form on the ceilings of caves which look like icicles. To remember their location, think of holding on "tite" to a ceiling.  Stalactites begin their life as a single drop of water which has been combined with carbon dioxide, calcium carbonate, and calcite. The water drop is squeezed from between the rocks and drops to the floor leaving behind a minute deposit of the dissolved calcite in the shape of a ring. Ring forms upon ring until a small drop like tube hangs from the ceiling called a  "soda straw." The dissolved calcite deposit process continues until beautiful stalactites are formed.

Stalagmites

Stalagmites are the formations found on the floor of caves,  reaching upward towards the stalacites hanging from the ceiling. In order to remember the stalagmite, remember the word stalagmite has a ‘g’ which could stand for ground. Stalagmites are the result of the excess water dropping from its parent, the stalactite. A stalagmite is more rounded, smoother, and has no central tube as the stalactite does. Straight formations of stalagmites are called "broomsticks." If the cave ceiling is very high the water droplet will splatter over a larger area, a stubby, flat formation will occur that may resemble a stack of "pancakes." mvc-021f.jpg (44458 bytes)

Columns

column.jpg (54534 bytes) Columns are formed when the stalactite and the stalagmite continue to build and grow. When the two join, they form a single pillar or column reaching from the floor to the ceiling.

Rimstone Pools

The humidity level in caves is very high. Water in caves without a flow of air, generally does notpool.jpg (31811 bytes) evaporate. The excess water flowing from the surface area is collected in small underground pools. Naturally the collected water is rich in mineral deposits. Any sort of disturbance of these pools results in  collections of calcite around the rim, which are called stalagmite ridges with horizontal crests. These crests act like small dams that hold back the pools of water. These dams are referred to as rimstone pools.  Continued growth of these rimstone pools tend to reinforce the cave against collapse.

 

Up Cave Formations Arkansas Caves Cave Life Class Activities

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