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  2. List of lava tubes - Wikipedia

    en.wikipedia.org/wiki/List_of_Lava_Tubes

    Kazumura Cave, Hawaii – Not only the world's most extensive lava tube, but at 65.5 kilometres (40.7 mi), it has the greatest linear extent of any cave known. [11] Kuna Caves – Idaho; Lava Beds National Monument – California; Newberry National Volcanic Monument – Oregon Arnold Lava Tube System; Boyd Cave – Oregon; Horse Lava Tube ...

  3. Type 1 Chi-He medium tank - Wikipedia

    en.wikipedia.org/wiki/Type_1_Chi-He_medium_tank

    The gun could be elevated and depressed between +20 and -15 degrees. This gun was used in the Type 97 ShinHōtō Chi-Ha medium tank, and on the Type 3 Ka-Chi amphibious tank. [11] The Type 1 Chi-He was also the first Japanese tank to carry a radio as standard equipment in each tank, eliminating the need to use signal flags. [12]

  4. Pillow lava - Wikipedia

    en.wikipedia.org/wiki/Pillow_lava

    The tongue continues to lengthen and inflate with more lava, forming a lobe, until the pressure of the magma becomes sufficient to rupture the skin and start the formation of a new eruption point nearer the vent. This process produces a series of interconnecting lobate shapes that are pillow-like in cross-section. [8]

  5. Lava cave - Wikipedia

    en.wikipedia.org/wiki/Lava_cave

    One other form a lava tube can take is the tube-in-tube which can form inside lava tubes if the linings of the walls are weak enough to lean inward, forming a new floor above the old. Tube-in-tubes are generally noted to form during the last lava draining through the main lava tube. [1] [2] [3]

  6. Siberian Traps - Wikipedia

    en.wikipedia.org/wiki/Siberian_Traps

    Large volumes of basaltic lava covered a large expanse of Siberia in a flood basalt event. Today, the area is covered by about 7 million km 2 (3 million sq mi) of basaltic rock, with a volume of around 4 million km 3 (1 million cu mi).

  7. Magma - Wikipedia

    en.wikipedia.org/wiki/Magma

    The thickness of a basalt lava, particularly on a low slope, may be much greater than the thickness of the moving lava flow at any one time, because basalt lavas may "inflate" by supply of lava beneath a solidified crust. [31] Most basalt lavas are of ʻAʻā or pāhoehoe types, rather than block lavas.