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  2. Felsic - Wikipedia

    en.wikipedia.org/wiki/Felsic

    Felsic. In geology, felsic is a modifier describing igneous rocks that are relatively rich in elements that form feldspar and quartz. [1] It is contrasted with mafic rocks, which are relatively richer in magnesium and iron. Felsic refers to silicate minerals, magma, and rocks which are enriched in the lighter elements such as silicon, oxygen ...

  3. Lava - Wikipedia

    en.wikipedia.org/wiki/Lava

    Felsic or silicic lavas have a silica content greater than 63%. They include rhyolite and dacite lavas. With such a high silica content, these lavas are extremely viscous, ranging from 10 8 cP (10 5 Pa⋅s) for hot rhyolite lava at 1,200 °C (2,190 °F) to 10 11 cP (10 8 Pa⋅s) for cool rhyolite lava at 800 °C (1,470 °F). [ 13 ]

  4. Felsite - Wikipedia

    en.wikipedia.org/wiki/Felsite

    Felsite is a very fine-grained volcanic rock that may or may not contain larger crystals. 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 ...

  5. Internal structure of Earth - Wikipedia

    en.wikipedia.org/wiki/Internal_structure_of_Earth

    Earth's inner core is the innermost geologic layer of the planet Earth. It is primarily a solid ball with a radius of about 1,220 km (760 mi), which is about 19% of Earth's radius [0.7% of volume] or 70% of the Moon 's radius. [32][33] The inner core was discovered in 1936 by Inge Lehmann and is generally composed primarily of iron and some nickel.

  6. Volcano - Wikipedia

    en.wikipedia.org/wiki/Volcano

    Felsic lavas (dacites or rhyolites) are highly viscous and are erupted as domes or short, stubby flows. [40] Lassen Peak in California is an example of a volcano formed from felsic lava and is actually a large lava dome. [41] Because felsic magmas are so viscous, they tend to trap volatiles (gases) that are present, which leads to explosive ...

  7. Archean felsic volcanic rocks - Wikipedia

    en.wikipedia.org/wiki/Archean_felsic_volcanic_rocks

    Archean felsic volcanic rocks are felsic volcanic rocks that were formed in the Archean Eon (4 to 2.5 billion years ago). [2] The term "felsic" means that the rocks have silica content of 62–78%. [3] Given that the Earth formed at ~4.5 billion year ago, [4] Archean felsic volcanic rocks provide clues on the Earth's first volcanic activities ...

  8. Geochemistry - Wikipedia

    en.wikipedia.org/wiki/Geochemistry

    Organic geochemistry, the study of the role of processes and compounds that are derived from living or once-living organisms. [13] Photogeochemistry is the study of light-induced chemical reactions that occur or may occur among natural components of the Earth's surface. [14]

  9. 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.