Lavacicle

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Close-up of a skylight on coastal plain, with lava stalactites forming on the roof of the tube

Lavacicles are geological formations resembling small round-tipped stalactites that are found in lava tubes, the name comes from their resemblance to icicles. Lavacicle is really a generic term that encompasses several different types of stalactites found in lava tubes, which differ in their shape and morphology (from Bunnell, 2008):


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[edit] Shark Tooth Stalactites

The shark tooth stalactite is broad and tapering in appearance. It may begin as a small driblet of lava from a semi-solid ceiling, but then grows by accreting layers as successive flows of lava rise and fall in the lava tube, coating and recoating the stalactite with more material. They can vary from a few millimeters to over a meter in length.

[edit] Splash Stalactites

As lava flows through a tube, material will be splashed up on the ceiling and ooze back down, hardening into a stalactite. This type of formation results in a very irregularly shaped stalactite, looking somewhat like stretched taffy. Often they may be of a different color than the original lava that formed the cave.

[edit] Tubular lava stalactites

When the roof of a lava tube is cooling, a skin will form that traps semi-molten material inside. Trapped gases force lava to extrude out through small openings that result in hollow, tubular stalactites analogous to the soda straws formed as depositional speleothems in solution caves, The longest known is almost 2 meters in length. These are common in Hawaiian lava tubes and are often associated with a drip stalagmite that forms below as material is carried through the tubular stalactite and piles up on the floor beneath. Sometimes the tubular form collapses near the distal end, most likely when the pressure of escaping gases decreased and still-molten portions of the stalactites deflated and cooled. Often these tubular stalactites will acquire a twisted, vermiform appearance as bits of lava crystallize and force the flow in different directions. These tubular lava helictites may also be influenced by air currents through a tube and point downwind.

[edit] Examples of Different Lavacicles

[edit] See also

[edit] References

Bunnell, D. (2008) Caves of Fire:Inside America's Lava Tubes. National Speleological Society, Huntsville, AL.ISBN: 9781879961319

[edit] External links

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