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  2. Felsic - Wikipedia

    en.wikipedia.org/wiki/Felsic

    Felsic refers to silicate minerals, magma, and rocks which are enriched in the lighter elements such as silicon, oxygen, aluminium, sodium, and potassium. Molten felsic magma and lava is more viscous than molten mafic magma and lava. Felsic magmas and lavas have lower temperatures of melting and solidification than mafic magmas and lavas.

  3. Granite - Wikipedia

    en.wikipedia.org/wiki/Granite

    Granite. Granite (/ ˈɡrænɪt / GRAN-it) is a coarse-grained (phaneritic) intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase. It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies underground.

  4. 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.

  5. Felsite - Wikipedia

    en.wikipedia.org/wiki/Felsite

    Felsite is a field term for a light-colored rock that typically requires petrographic examination or chemical analysis for more precise definition. Color is generally white through light gray, or red to tan and may include any color except dark gray, green or black (the colors of trap rock). [1] The mass of the rock consists of a fine-grained ...

  6. Igneous textures - Wikipedia

    en.wikipedia.org/wiki/Igneous_textures

    Igneous textures are used by geologists in determining the mode of origin of igneous rocks and are used in rock classification. The six main types of textures are phaneritic, aphanitic, porphyritic, glassy, pyroclastic, and pegmatitic. Aphanitic (a = not, phaner = visible) rocks, in contrast to phaneritic rocks, typically form from lava which ...

  7. Orthoclase - Wikipedia

    en.wikipedia.org/wiki/Orthoclase

    References. [2][3][4] Orthoclase, or orthoclase feldspar (endmember formula K Al Si 3 O 8), is an important tectosilicate mineral which forms igneous rock. The name is from the Ancient Greek for "straight fracture", because its two cleavage planes are at right angles to each other. It is a type of potassium feldspar, also known as K-feldspar.

  8. Category:Felsic rocks - Wikipedia

    en.wikipedia.org/wiki/Category:Felsic_rocks

    Pages in category "Felsic rocks" The following 9 pages are in this category, out of 9 total. This list may not reflect recent changes. A. Adakite; Aplite; Appinite;

  9. Tonalite - Wikipedia

    en.wikipedia.org/wiki/Tonalite

    Tonalite is an igneous, plutonic (intrusive) rock, of felsic composition, with phaneritic (coarse-grained) texture. Feldspar is present as plagioclase (typically oligoclase or andesine) with alkali feldspar making up less than 10% of the total feldspar content. Quartz (SiO 2) is present as more than 20% of the total quartz-alkali feldspar ...