When.com Web Search

Search results

  1. Results From The WOW.Com Content Network
  2. Laze (geology) - Wikipedia

    en.wikipedia.org/wiki/Laze_(geology)

    [1] [2] The term laze is a portmanteau of lava and haze. Laze, created by the interaction of lava and cold seawater, differs from vog, which originates from volcanic vents. [3] [4] The extremely high temperatures of lava flows 1,200 °C (2,200 °F) causes sea water to decompose into hydrogen and oxygen.

  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. Volcanic gas - Wikipedia

    en.wikipedia.org/wiki/Volcanic_gas

    Molten rock (either magma or lava) near the atmosphere releases high-temperature volcanic gas (>400 °C). In explosive volcanic eruptions, the sudden release of gases from magma may cause rapid movements of the molten rock. When the magma encounters water, seawater, lake water or groundwater, it can be rapidly fragmented.

  5. Lava delta - Wikipedia

    en.wikipedia.org/wiki/Lava_delta

    Lava deltas, similar to river deltas, form wherever sufficient sub-aerial flows of lava enter standing bodies of water. The lava cools and breaks up as it encounters the water, with the resulting fragments filling in the adjacent seabed topography such that the flow can move further offshore sub-aerially.

  6. Magma - Wikipedia

    en.wikipedia.org/wiki/Magma

    Magma that is extruded as lava is extremely dry, but magma at depth and under great pressure can contain a dissolved water content in excess of 10%. Water is somewhat less soluble in low-silica magma than high-silica magma, so that at 1,100 °C and 0.5 GPa , a basaltic magma can dissolve 8% H 2 O while a granite pegmatite magma can dissolve 11% ...

  7. Tectonic–climatic interaction - Wikipedia

    en.wikipedia.org/wiki/Tectonic–climatic...

    Tectonic–climatic interaction is the interrelationship between tectonic processes and the climate system. The tectonic processes in question include orogenesis , volcanism , and erosion , while relevant climatic processes include atmospheric circulation , orographic lift , monsoon circulation and the rain shadow effect .

  8. Cryovolcano - Wikipedia

    en.wikipedia.org/wiki/Cryovolcano

    Leviathan Patera (center) and Ruach Planitia (upper left), two large cryovolcanic features on Neptune's moon Triton. A cryovolcano (sometimes informally referred to as an ice volcano) is a type of volcano that erupts gases and volatile material such as liquid water, ammonia, and hydrocarbons.

  9. Steam explosion - Wikipedia

    en.wikipedia.org/wiki/Steam_explosion

    Littoral explosion at Waikupanaha ocean entry at the big island of Hawaii was caused by the lava entering the ocean. A steam explosion is an explosion caused by violent boiling or flashing of water or ice into steam, occurring when water or ice is either superheated, rapidly heated by fine hot debris produced within it, or heated by the interaction of molten metals (as in a fuel–coolant ...