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A stalactite (Greek stalaktos, (Σταλακτίτης), "dripping" or "dropped"), or dripstone, is a type of speleothem that hangs from the ceiling or wall of limestone caves.

Stalactites are formed from the deposition of calcium carbonate and other minerals, which is precipitated from mineralized water solutions. The corresponding formation on the floor underneath a stalactite is known as a stalagmite. Given enough time, these formations can meet, resulting in a formation known as a column or pillar.

Every stalactite begins with a single mineral-laden drop of water. When the drop falls, it leaves behind the thinnest ring of calcite. Each subsequent drop that forms and falls deposits another calcite ring. Eventually, these rings form a very narrow (0.5 mm), hollow tube commonly known as a "soda straw" stalactite. Soda straws can grow quite long, but are very fragile. If they become plugged by debris, water begins flowing over the outside, depositing more calcite and creating the more familiar cone-shaped stalactite.

The same water drops that fall from the tip of a stalactite deposit more calcite on the floor below, eventually resulting in a rounded or cone-shaped stalagmite. Unlike stalactites, stalagmites never start out as hollow "soda straws."

The longest stalactite known hangs in the Chamber of Rarities in the Gruta Rei do Mato (Sete Lagoas, Minas Gerais, Brazil). It is 20 metres long.

Stalactites and stalagmites can also form on concrete ceilings and floors, although they form much more quickly there than in the natural cave environment.

There are various mnemonics to help remember which formation hangs from the ceiling (stalactite) and which rises from the floor (stalagmite):

  • StalaCtite has a "c" for "ceiling".
  • StalaGmite has a "g" for "ground".

  • Stalactite is stretched "tite" (tight) by hanging from the ceiling.
  • Stalactites have to hang on tight to the ceiling.
  • Stalagmites might reach the ceiling.
  • Stalagmite pushes up with all its "mite" (might) from the floor.

  • "When the mites go up, the "tites" (tights) come down".

See also


http://www.goodearthgraphics.com/virtcave/staltite/staltite.html The Virtual Cave's page on stalactites

Cave geology

Estalactita | Stalaktit | Stalaktit | Tropfstein | Estalactita | stalaktita kaverno | Stalactite | Stalattite | נטיף | Druipsteen | 鍾乳石 | Stalaktyt | Estalactite | Sarkıt | 钟乳石

 

This article is licensed under the GNU Free Documentation License. It uses material from the "Stalactite".

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