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  2. 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.

  3. 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 ...

  4. 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 ...

  5. Magma - Wikipedia

    en.wikipedia.org/wiki/Magma

    Basalt lavas tend to produce low-profile shield volcanoes or flood basalts, because the fluidal lava flows for long distances from the vent. 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 ...

  6. Mono–Inyo Craters - Wikipedia

    en.wikipedia.org/wiki/Mono–Inyo_Craters

    [48]: 5 Mound-shaped features called lava domes are often created from these flows. Rock fragments thrown from a growing lava dome may reach 3.1 to 6.2 miles (5 to 10 km) from the dome. [ 47 ] A partial collapse of the steep-sided growing dome can send pyroclastic flows outward at least 3.1 miles (5 km). [ 47 ]

  7. What travelers to Hawaii can expect following Mauna Loa's ...

    www.aol.com/travelers-hawaii-expect-following...

    How can I see the lava flow on Hawaii Island? Hawaii Volcanoes National Park offers the best views of the lava flow. At night, the lava's glow is "currently visible from many areas and overlooks ...

  8. Geologists believe these basalt-lined table tops are the remains of ancient lava flow from a volcano that erupted 10 to 12 million years ago in what today is either eastern California or western ...

  9. Volcanic rock - Wikipedia

    en.wikipedia.org/wiki/Volcanic_rock

    The terms lava stone and lava rock are more used by marketers than geologists, who would likely say "volcanic rock" (because lava is a molten liquid and rock is solid). "Lava stone" may describe anything from a friable silicic pumice to solid mafic flow basalt, and is sometimes used to describe rocks that were never lava , but look as if they ...