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  2. Alkali feldspar granite - Wikipedia

    en.wikipedia.org/wiki/Alkali_feldspar_granite

    Alkali feldspar granite, some varieties of which are called 'red granite', [1] is a felsic igneous rock and a type of granite rich in the mineral potassium feldspar (K-spar). It is a dense rock with a phaneritic texture. The abundance of K-spar gives the rock a predominant pink to reddish hue; peppered with minor amounts of black minerals. [2] [3]

  3. Granite - Wikipedia

    en.wikipedia.org/wiki/Granite

    Mafic enclave in granite rock, at Yosemite National Park Granite forms from silica-rich ( felsic ) magmas. Felsic magmas are thought to form by addition of heat or water vapor to rock of the lower crust , rather than by decompression of mantle rock, as is the case with basaltic magmas. [ 20 ]

  4. I-type granite - Wikipedia

    en.wikipedia.org/wiki/I-type_Granite

    Color index, or the modal abundance of minerals other than quartz, plagioclase and alkali feldspar (e.g., mafic silicates, oxides, sulfides, phosphates, etc.), can be used to infer the maturity of a granite. Juvenile I-type granites have a higher color index. Amphibole, biotite, sphene, allanite, and oxides are typically more abundant. In ...

  5. 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).

  6. Mysterious hair ice phenomenon explained - AOL

    www.aol.com/news/2015-07-25-mysterious-hair-ice...

    Hair ice looks like incredibly fine, billowing strands massed together. Lasting merely hours or only a few days before melting, its exact cause has been a mystery for nearly 100 years.

  7. 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]

  8. The best leave-In conditioners for 2024 to help your hair - AOL

    www.aol.com/lifestyle/best-smelling-leave-in...

    Ceremonia uses the superpowers of the guava fruit to protect hair from UV rays and free radicals and combines it with avocado, safflower extract and tamarind to hydrate hair and combat frizz.

  9. Mafic - Wikipedia

    en.wikipedia.org/wiki/Mafic

    The mafic rocks also typically have a higher density than felsic rocks. The term roughly corresponds to the older basic rock class. [9] Mafic lava, before cooling, has a low viscosity, in comparison with felsic lava, due to the lower silica content in mafic magma. Water and other volatiles can more easily and gradually escape from mafic lava.