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  2. Stalactite - Wikipedia

    en.wikipedia.org/wiki/Stalactite

    Image showing the six most common speleothems with labels. Enlarge to view labels. A stalactite (UK: / ˈ s t æ l ə k ˌ t aɪ t /, US: / s t ə ˈ l æ k t aɪ t /; from Ancient Greek σταλακτός (stalaktós) 'dripping', from σταλάσσειν (stalássein) 'to drip') [1] is a mineral formation that hangs from the ceiling of caves, hot springs, or man-made structures such as ...

  3. Stalagmite - Wikipedia

    en.wikipedia.org/wiki/Stalagmite

    3) but the common point is that it remains driven by gravity. Drops of molten lava (siliceous material, SiO 2) solidify onto the floor of the already emptied lava tube, when the lava temperature sufficiently decreases after the passage and the complete purge of the main lava flow. Essentially, it is still the gravity deposition of material onto ...

  4. Speleothem - Wikipedia

    en.wikipedia.org/wiki/Speleothem

    Speleothem. A speleothem (/ ˈspiːliəθɛm /; from Ancient Greek σπήλαιον (spḗlaion) 'cave' and θέμα (théma) 'deposit') is a geological formation by mineral deposits that accumulate over time in natural caves. [1] Speleothems most commonly form in calcareous caves due to carbonate dissolution reactions.

  5. Flowstone - Wikipedia

    en.wikipedia.org/wiki/Flowstone

    Flowstone. Flowstones are sheetlike deposits of calcite or other carbonate minerals, formed where water flows down the walls or along the floors of a cave. [1] They are typically found in "solution caves", in limestone, where they are the most common speleothem. However, they may form in any type of cave where water enters that has picked up ...

  6. Blanchard Springs Caverns - Wikipedia

    en.wikipedia.org/wiki/Blanchard_Springs_Caverns

    Blanchard Springs Caverns is a three-level cave system, all of which can be viewed on guided tours. The Dripstone Trail runs through the uppermost level of caverns for about a 0.5 miles (0.80 km) and opened in 1973. [2] The Discovery Trail opened in 1977 and loops through a 1.2 miles (1.9 km) section of the cavern, descending to the lower level ...

  7. Natrocarbonatite - Wikipedia

    en.wikipedia.org/wiki/Natrocarbonatite

    Natrocarbonatite is a rare carbonatite lava which erupts from the Ol Doinyo Lengai volcano in Tanzania within the East African Rift of eastern Africa. Natrocarbonatite lavas were first documented in 1962, by J. B. Dawson. [1][2]

  8. Augustine Volcano - Wikipedia

    en.wikipedia.org/wiki/Augustine_Volcano

    Augustine Volcano (Sugpiaq: Utakineq; [3] Dena'ina: Chu Nula) is a stratovolcano in Alaska consisting of a central complex of summit lava domes and flows surrounded by an apron of pyroclastic, lahar, avalanche, and ash deposits. The volcano is frequently active, with major eruptions recorded in 1883, 1935, 1963–64, 1976, 1986, and 2006.

  9. Merrill Cave - Wikipedia

    en.wikipedia.org/wiki/Merrill_Cave

    41.72872°N 121.54890°W. / 41.72872; -121.54890. Length. 650 foot (200 m) Difficulty. Easy. Merrill Cave is a 650 foot (200 m) former ice cave in Lava Beds National Monument in California. It was known for the pool of ice that was found year-round in the lower chamber of the cave, which fully disappeared due to compounding factors by 2005.