A helictite is a speleothem found in limestone caves that changes its axis from the vertical at one or more stages during its growth. They have a curving or angular form that looks as if they were grown in zero gravity. They are most likely the result of capillary forces acting on tiny water droplets, a force often strong enough at this scale to defy gravity.

Helictites are, perhaps, the most delicate and most beautiful of cave formations. They are usually made of needle-form calcite and aragonite. Forms of helictites have been described in several types: ribbon helictites, saws, rods, butterflies, "hands", curly-fries, and "clumps of worms." They typically have radial symmetry. They can be easily crushed or broken by the slightest touch. Because of this, helictites are rarely seen within arm's reach in tourist caves.


The growth of helictites is still quite enigmatic. Until now, there has been no satisfactory explanation for how they are formed. Currently, formation by capillary forces is the most likely theory, but another theory based on wind formation is also viable.

Capillary forces

The most likely theory explains helictites as a result of capillary forces. If the helictite has a very thin central tube where the water flows like it does in straws, capillary forces would be able to transport water against gravity. This theory was inspired by some hollow helictites. However, the majority of helictites are definitely not hollow. Despite this, droplets can be drawn to the tips of existing structures and deposit their calcite load almost anywhere thereon. This can lead to the wandering and curling structures seen in many helictites.


Another theory names the wind in the cave as main reason for the strange look. Drops hanging on a stalactite are blown to one side, so the dripstone grows in that direction. If the wind changes, the direction of growth changes too. However this theory is very problematic, because wind directions change very often. The wind in caves depends on air pressure changes outside, which in turn depend on the weather. Wind caves are known to experience these windy conditions. The wind direction changes as often as the weather conditions outside change. But the dripstones grow very slowly - several centimeters in 100 years - meaning the wind direction would have to stay steady for long periods of time, changing for every fragment of a millimeter of growth. A second problem with this theory is that many caves with helictites have no natural entrance where wind could enter.

Helictite growth

A helictite starts its growth as a tiny stalactite. The direction of the end of the straw may wander, twist like a corkscrew, or the main part may form normally while small helictites pop out of its side like rootlets or fishhooks. In some caves, helictites cluster together and form bushes as large as six feet tall. These bushes grow from the floor of the cave. When helictites are found on cave floors, they are referred to as heligmites, though there is debate as to whether this is a genuine subcategory.

For an unknown reason, when the chemical composition of the water is slightly altered, the single crystal structure can change from a cylindrical shape to a conical one. In some of these cases, each crystal fits into the prior one like an inverted stack of ice cream cones.


The first detailed description of helictites was made in 1665 by Olaus Worm.


* [http://www.goodearthgraphics.com/virtcave/helictit/helictit.html The Virtual Cave: Helictites]
* [http://www.showcaves.com/english/explain/Speleothem/Helictite.html Helictite or Eccentric?]
* [http://cmug.com/chintimp/splitting.htm Does crystal splitting play a part in the curvature of helictites? (Abstract)] By George W. Moore, Journal of Cave and Karst Studies, v. 62, p. 37 (2000).

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Look at other dictionaries:

  • helictite — [hə lik′tīt΄] n. a thin, stony, curling cave deposit, usually of calcite, slowly formed as tiny water drops emerge from its tip and evaporate * * * …   Universalium

  • helictite — [hə lik′tīt΄] n. a thin, stony, curling cave deposit, usually of calcite, slowly formed as tiny water drops emerge from its tip and evaporate …   English World dictionary

  • helictite —    1. Generally small variety of stalactitic calcite growth that is twisted and contorted with no apparent regard for gravity. Helictites form on cave walls, ceilings, and on stalactites. The growth develops as seepage water loses carbon dioxide… …   Lexicon of Cave and Karst Terminology

  • helictite — noun A speleothem found in limestone caves that changes its axis from the vertical at one or more stages during its growth …   Wiktionary

  • helictite — he·lic·tite …   English syllables

  • helictite — hə̇ˈlikˌtīt, ˈhelə̇k noun ( s) Etymology: helict (from Greek heliktos twisted, rolled, from helik , helix spiral) + ite : an irregular stalactite with branching convolutions or spines …   Useful english dictionary

  • Abrakurrie Cave — is a wild cave on the Nullarbor Plain in Western Australia. It is reported to have the largest single cave chamber in the southern hemisphere, [cite web | title=South Australia: Whales Wildcaves | work=Diverse Travel Australia |… …   Wikipedia

  • Caverns of Sonora — The Caverns of Sonora, a National Natural Landmark [http://www.nature.nps.gov/nnl/Registry/USA Map/States/Texas/NNL/CS/index.cfm] , is a unique cave located eight miles (13 km) west of the town of Sonora, Texas. It is a world class cave due to… …   Wikipedia

  • anemolite —    A helictite in which the eccentricity is ascribed to the action of air currents [10]. The word is derived from wind control theory of helictite formation [9] …   Lexicon of Cave and Karst Terminology

  • helictită — HELICTÍTĂ s.f. (geol.) Denumire dată unor concreţiuni calcaroase în formă de spirală care se formează pe pereţii peşterilor, ramificându se în toate direcţiile. [< fr. hélictite]. Trimis de LauraGellner, 20.04.2005. Sursa: DN  HELICTÍTĂ s. f …   Dicționar Român

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