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  2. Blue lava - Wikipedia

    en.wikipedia.org/wiki/Blue_lava

    "Blue lava" is an electric-blue fire that burns when sulfur combusts, producing a neon-blue flame. Sulfur burns when it comes into contact with hot air at temperatures above 360 °C (680 °F), which produces the energetic flames. [2] Actual lava is red-orange in color, given its temperature.

  3. Ijen - Wikipedia

    en.wikipedia.org/wiki/Ijen

    The blue fire is ignited sulfuric gas, which emerges from cracks at temperatures up to 600 °C (1,112 °F). The flames can be up to five meters (16 feet) high; some of the gas condenses to liquid and is still ignited. [9] [10] Ijen is the largest blue flame area in the world. Local people refer to it as Api Biru (Blue Fire). [11]

  4. Black-body radiation - Wikipedia

    en.wikipedia.org/wiki/Black-body_radiation

    The temperature of a Pāhoehoe lava flow can be estimated by observing its color. The result agrees well with other measurements of temperatures of lava flows at about 1,000 to 1,200 °C (1,830 to 2,190 °F). When the body is black, the absorption is obvious: the amount of light absorbed is all the light that hits the surface.

  5. Lava - Wikipedia

    en.wikipedia.org/wiki/Lava

    The lava's viscosity mostly determines the behavior of lava flows. While the temperature of common silicate lava ranges from about 800 °C (1,470 °F) for felsic lavas to 1,200 °C (2,190 °F) for mafic lavas, [16] its viscosity ranges over seven orders of magnitude, from 10 11 cP (10 8 Pa⋅s) for felsic lavas to 10 4 cP (10 Pa⋅s) for mafic ...

  6. Magma - Wikipedia

    en.wikipedia.org/wiki/Magma

    When erupted, the temperature of the molten iron oxide magma is about 700 to 800 °C (1,292 to 1,472 °F). [42] Sulfur lava flows up to 250 metres (820 feet) long and 10 metres (33 feet) wide occur at Lastarria volcano, Chile. They were formed by the melting of sulfur deposits at temperatures as low as 113 °C (235 °F). [16]

  7. Igneous rock - Wikipedia

    en.wikipedia.org/wiki/Igneous_rock

    Igneous rock (igneous from Latin igneus 'fiery'), or magmatic rock, is one of the three main rock types, the others being sedimentary and metamorphic. Igneous rocks are formed through the cooling and solidification of magma or lava. The magma can be derived from partial melts of existing rocks in either a planet 's mantle or crust.

  8. Sudarsky's gas giant classification - Wikipedia

    en.wikipedia.org/wiki/Sudarsky's_gas_giant...

    Sudarsky's classification of gas giants for the purpose of predicting their appearance based on their temperature was outlined by David Sudarsky and colleagues in the paper Albedo and Reflection Spectra of Extrasolar Giant Planets [1] and expanded on in Theoretical Spectra and Atmospheres of Extrasolar Giant Planets, [2] published before any successful direct or indirect observation of an ...

  9. Volcanic gas - Wikipedia

    en.wikipedia.org/wiki/Volcanic_gas

    Volcanic gas. Volcanic gases are gases given off by active (or, at times, by dormant) volcanoes. These include gases trapped in cavities (vesicles) in volcanic rocks, dissolved or dissociated gases in magma and lava, or gases emanating from lava, from volcanic craters or vents. Volcanic gases can also be emitted through groundwater heated by ...