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  2. Stalactite - Wikipedia

    en.wikipedia.org/wiki/Stalactite

    A key difference with lava stalactites is that once the lava has ceased flowing, so too will the stalactites cease to grow. This means that if the stalactite were to be broken it would never grow back. [2] The generic term lavacicle has been applied to lava stalactites and stalagmites indiscriminately and evolved from the word icicle. [2]

  3. Stalagmite - Wikipedia

    en.wikipedia.org/wiki/Stalagmite

    Image showing the six most common speleothems The "Witch’s Finger" in the Carlsbad Caverns, New Mexico. A stalagmite (UK: / ˈ s t æ l ə ɡ ˌ m aɪ t /, US: / s t ə ˈ l æ ɡ m aɪ t /; from Greek σταλαγμίτης (stalagmítēs); from Ancient Greek σταλαγμίας (stalagmías) 'dropping, trickling' and -ίτης (-ítēs) 'one connected to, a member of') [1] is a type of ...

  4. Soda straw - Wikipedia

    en.wikipedia.org/wiki/Soda_straw

    Straws (stalactite precursors) in Gardner's Gut. Soda straw. A soda straw (or simply straw) is a speleothem in the form of a hollow mineral cylindrical tube. They are also known as tubular stalactites. Soda straws grow in places where water leaches slowly through cracks in rock, such as on the roofs of caves.

  5. Brinicle - Wikipedia

    en.wikipedia.org/wiki/Brinicle

    A brinicle (brine icicle, also known as an ice stalactite) is a downward-growing hollow tube of ice enclosing a plume of descending brine that is formed beneath developing sea ice. As seawater freezes in the polar ocean, salt brine concentrates are expelled from the sea ice, creating a downward flow of dense, extremely cold, saline water , with ...

  6. Calthemite - Wikipedia

    en.wikipedia.org/wiki/Calthemite

    Calthemite straw stalactite growing from the concrete ceiling of an undercover car-park Calthemite straw stalactites, the rightmost example demonstrating bending due to the direction of air currents during its formation. Calthemite is a secondary deposit, derived from concrete, lime, mortar or other calcareous material outside the cave environment.

  7. Lava tube - Wikipedia

    en.wikipedia.org/wiki/Lava_tube

    Lavacicles are the most common of lava tube speleothems. Drip stalagmites may form under tubular lava stalactites, and the latter may grade into a form known as a tubular lava helictite. A runner is a bead of lava that is extruded from a small opening and then runs down a wall.

  8. Speleothem - Wikipedia

    en.wikipedia.org/wiki/Speleothem

    Helictites are stalactites that have a central canal with twig-like or spiral projections that appear to defy gravity Include forms known as ribbon helictites, saws, rods, butterflies, hands, curly-fries, and "clumps of worms" Chandeliers are complex clusters of ceiling decorations; Ribbon stalactites, or simply "ribbons", are shaped accordingly

  9. Borra Caves - Wikipedia

    en.wikipedia.org/wiki/Borra_Caves

    There is an area in the caves with limited light penetration. The stalactites seen in the caves are about 0.1 to 3.5 m (0.3 to 11.5 ft) in length while the stalagmites are 1.2 m (3.9 ft) long and columns are 6 m (20 ft) in height and 0.75 m (2.5 ft) in width. The height of the cave is 12 m (39 ft) and the length is about 200 m (660 ft).