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  2. Igneous textures - Wikipedia

    en.wikipedia.org/wiki/Igneous_textures

    The individual crystals in an aphanitic igneous rock are not distinguishable to the naked eye. Examples of aphanitic igneous rock include basalt, andesite, and rhyolite. Glassy or vitreous textures occur during some volcanic eruptions when the lava is quenched so rapidly that crystallization cannot occur. The result is a natural amorphous glass ...

  3. Phanerite - Wikipedia

    en.wikipedia.org/wiki/Phanerite

    Close-up of granite, a phanerite rock, from Yosemite National Park in California, U.S. Phaneritic diorite from Massachusetts. A phanerite [1] is an igneous rock whose microstructure is made up of crystals large enough to be distinguished with the unaided human eye. In contrast, the crystals in an aphanitic rock are

  4. Igneous rock - Wikipedia

    en.wikipedia.org/wiki/Igneous_rock

    For textural classification, igneous rocks that have crystals large enough to be seen by the naked eye are called phaneritic; those with crystals too small to be seen are called aphanitic. Generally speaking, phaneritic implies an intrusive origin or plutonic, indicating slow cooling; aphanitic are extrusive or volcanic, indicating rapid cooling.

  5. Texture (geology) - Wikipedia

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

    In geology, texture or rock microstructure [1] refers to the relationship between the materials of which a rock is composed. [2] The broadest textural classes are crystalline (in which the components are intergrown and interlocking crystals), fragmental (in which there is an accumulation of fragments by some physical process), aphanitic (in which crystals are not visible to the unaided eye ...

  6. Aphanite - Wikipedia

    en.wikipedia.org/wiki/Aphanite

    An aphanitic volcanic sand grain, with fine-grained groundmass, as seen through a petrographic microscope Aphanites (adj. aphanitic ; from Ancient Greek αφανης (aphanḗs) 'invisible') are igneous rocks that are so fine-grained that their component mineral crystals are not visible to the naked eye [ 2 ] (in contrast to phanerites , in ...

  7. Phonolite - Wikipedia

    en.wikipedia.org/wiki/Phonolite

    Its coarse grained (phaneritic) intrusive equivalent is nepheline syenite. Phonolite is typically fine grained and compact. The name phonolite comes from the Ancient Greek meaning "sounding stone" due to the metallic sound it produces if an unfractured plate is hit; hence, the English name clinkstone is given as a synonym.

  8. Rhyolite - Wikipedia

    en.wikipedia.org/wiki/Rhyolite

    Rhyolite (/ ˈ r aɪ. ə l aɪ t / RY-ə-lyte) [1] [2] [3] [4] is the most silica-rich of volcanic rocks.It is generally glassy or fine-grained in texture, but may be ...

  9. Dacite - Wikipedia

    en.wikipedia.org/wiki/Dacite

    Aphanitic QAPF diagram denoting dacite TAS diagram with the dacite (O3) field highlighted in yellow. Dacite consists mostly of plagioclase feldspar and quartz with biotite, hornblende, and pyroxene (augite or enstatite). The quartz appears as rounded, corroded phenocrysts, or as an element of the ground-mass. [3]