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  2. List of rock types - Wikipedia

    en.wikipedia.org/wiki/List_of_rock_types

    Lamproite – Mantle rock expulsed to the surface in volcanic pipes; Lamprophyre – Type of ultrapotassic igneous rock – An ultramafic, ultrapotassic intrusive rock dominated by mafic phenocrysts in a feldspar groundmass; Latite – Type of volcanic rock – A silica-undersaturated form of andesite

  3. Pumice - Wikipedia

    en.wikipedia.org/wiki/Pumice

    Pumice has a porosity of 64–85% by volume and it floats on water, possibly for years, until it eventually becomes waterlogged and sinks. [5] [6] Scoria differs from pumice in being denser. With larger vesicles and thicker vesicle walls, scoria sinks rapidly. The difference is the result of the lower viscosity of the magma that forms scoria.

  4. Igneous rock - Wikipedia

    en.wikipedia.org/wiki/Igneous_rock

    In a simplified compositional classification, igneous rock types are categorized into felsic or mafic based on the abundance of silicate minerals in the Bowen's Series. Rocks dominated by quartz, plagioclase, alkali feldspar and muscovite are felsic. Mafic rocks are primarily composed of biotite, hornblende, pyroxene and olivine.

  5. Color index (geology) - Wikipedia

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

    According to the Encyclopædia Britannica, color indices, 0–50 are felsic, 50–90 are mafic, and 90–100 are ultramafic. [6] An online geology textbook provides an example of the use of another classification scheme, in which color indices 0–15 are felsic, 15–45 are intermediate, 45–85 are mafic, and 85–100 are ultramafic. [9]

  6. Felsic - Wikipedia

    en.wikipedia.org/wiki/Felsic

    Felsic magmas and lavas have lower temperatures of melting and solidification than mafic magmas and lavas. Felsic rocks are usually light in color and have specific gravities less than 3. The most common felsic rock is granite. Common felsic minerals include quartz, muscovite, orthoclase, and the sodium-rich plagioclase feldspars (albite-rich).

  7. Rock (geology) - Wikipedia

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

    Volcanic or extrusive rocks result from magma reaching the surface either as lava or fragmental ejecta, forming minerals such as pumice or basalt. [ 5 ] Magmas tend to become richer in silica as they rise towards the Earth's surface, a process called magma differentiation .

  8. Extrusive rock - Wikipedia

    en.wikipedia.org/wiki/Extrusive_rock

    Extrusive rock refers to the mode of igneous volcanic rock formation in which hot magma from inside the Earth flows out (extrudes) onto the surface as lava or explodes violently into the atmosphere to fall back as pyroclastics or tuff. [1] In contrast, intrusive rock refers to rocks formed by magma which cools below the surface. [2]

  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 ...