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  2. The Greenstone Flow - Wikipedia

    en.wikipedia.org/wiki/The_Greenstone_Flow

    The Greenstone Flow is one of the world's largest known lava flows, estimated at a volume ~1650 to ~6000 cubic kilometers of mafic lava. [2] [3] In places, the lava pooled to depth of 487 meters. [4] The flow was generated by a flood basalt eruption during the Midcontinental Rift, which occurred 1.1 billion years ago. [5]

  3. Lava field - Wikipedia

    en.wikipedia.org/wiki/Lava_field

    The two main types of lava field structures are defined as sheet flow lava and pillow lava. Sheet flow lava appears like a wrinkled or folded sheet, while pillow lava is bulbous, and often looks like a pile of pillows atop one another. [2] An important aspect of lava flow morphology is a phenomenon known as lava flow inflation. This occurs in ...

  4. Lava - Wikipedia

    en.wikipedia.org/wiki/Lava

    The word lava comes from Italian and is probably derived from the Latin word labes, which means a fall or slide. [2] [3] An early use of the word in connection with extrusion of magma from below the surface is found in a short account of the 1737 eruption of Vesuvius, written by Francesco Serao, who described "a flow of fiery lava" as an analogy to the flow of water and mud down the flanks of ...

  5. Llullaillaco - Wikipedia

    en.wikipedia.org/wiki/Llullaillaco

    Morphologically, these flows are reddish-black aa lava flows and feature blocks with sizes of 5 m. [34] The northern flow has prominent levee-like structures [41] and splits into a northwestern and northeastern branch [18] upon reaching an obstacle. [42] The southwestern [18] lava flow is 6 km long and was fairly viscous when it was erupted. [40]

  6. Ice-marginal lava flow - Wikipedia

    en.wikipedia.org/wiki/Ice-marginal_lava_flow

    An ice-marginal lava flow is a lava flow that comes into direct contact with a glacier or the margins of a large ice sheet. As the lava reaches the margins of an ice sheet, the front of the lava flow cools very quickly to form a barrier. Behind this barrier, the lava begins to pool, ceasing the contact between the hot lava and cold ice.

  7. Mount Garibaldi - Wikipedia

    en.wikipedia.org/wiki/Mount_Garibaldi

    Because dacite is the main type of lava erupted from Mount Garibaldi, lava flows are a low to moderate hazard. [3] Dacite is felsic [ d ] in composition, containing 62–69% silica content. [ 71 ] [ 72 ] This high percentage in silica content increases the viscosity of dacitic melts relative to that of andesite or basalt , generally resulting ...

  8. Bloomington, IL Weather - Hourly Forecasts and Local ... - AOL

    www.aol.com/weather/forecast/us/bloomington-12784757

    About 13 million people are under flood watches across California, where heavy rain is expected to produce flooding, mudslides and debris flows through Wednesday. Fox Weather 1 day ago

  9. 1980 eruption of Mount St. Helens - Wikipedia

    en.wikipedia.org/wiki/1980_eruption_of_Mount_St...

    The resulting deposits formed a fan-like pattern of overlapping sheets, tongues, and lobes. At least 17 separate pyroclastic flows occurred during the May 18 eruption, and their aggregate volume was about 0.05 cu mi (0.21 km 3). [9] The flow deposits were still at about 570 to 790 °F (300 to 420 °C) two weeks after they erupted. [9]