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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:
Stalactites
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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. |
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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." |
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Columns
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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. |
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Rimstone Pools
The humidity level in caves is very high. Water in caves without a flow of air,
generally does not 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.
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