Stalagmite

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Calthemite Stalagmite on concrete floor
Seven stars cave
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Herault stalagmite2

Stalagmite

A stalagmite in a cave

A stalagmite is a type of rock formation that rises from the floor of a cave due to the accumulation of material deposited on the floor from ceiling drippings. Stalagmites are typically composed of calcium carbonate (CaCO3) in the form of travertine or aragonite, but they can also consist of other minerals such as gypsum, halite, and sulfur.

Formation[edit | edit source]

Stalagmites form through the deposition of minerals from water dripping onto the cave floor. When water containing dissolved calcium carbonate drips from the ceiling of a cave, it leaves behind a small deposit of calcite. Over time, these deposits accumulate and grow upward from the floor, forming a stalagmite. The rate of growth can vary significantly depending on factors such as the amount of water dripping, the concentration of minerals in the water, and the cave's temperature and humidity.

Types of Stalagmites[edit | edit source]

Stalagmites can vary greatly in shape and size. Some common types include:

  • Conical stalagmites: These have a broad base and taper to a point.
  • Columnar stalagmites: These are more cylindrical and can grow to connect with stalactites, forming a column.
  • Candle-shaped stalagmites: These are slender and have a more uniform width.

Differences Between Stalagmites and Stalactites[edit | edit source]

Stalagmites and stalactites are often confused, but they have distinct differences. Stalactites hang from the ceiling of a cave, while stalagmites grow from the floor. A useful mnemonic to remember this is that stalactites "hang tight" to the ceiling, and stalagmites "might" reach the ceiling if they grow long enough.

Notable Stalagmites[edit | edit source]

Some of the world's most famous stalagmites can be found in caves such as:

Related Pages[edit | edit source]

See Also[edit | edit source]

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Contributors: Prab R. Tumpati, MD