Basaltic magma usually forms a black rock.
Generally dark with shades of green and black.
baslt
False. Light colored rocks with lower densities typically form from felsic magma, which has a higher silica content compared to basaltic magma. Felsic rocks include granite and rhyolite, which are commonly light in color and less dense.
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dark
Dark green to black.
Basaltic Magmas are dark colored, heavy and are ferromagnesian in composition, so they most times do not form light colored rocks, rather, the Felsic Granitic Magma forms the light colored rocks with lower densities.
magma can be classified into two,magma of granitic composition(originates from lower continental crust) and magma of basaltic composition (which originates from upper mantle).Both can form intrusive rocks.
False. Light-colored rocks with lower densities, such as granite, typically form from granitic magma, which is more viscous and contains higher concentrations of silica. Basaltic magma, on the other hand, produces darker, denser rocks like basalt. Therefore, the statement is incorrect.
Basaltic igneous rocks are fine-grained and have a low silica content. They are typically dark in color, ranging from black to dark gray. They form from the rapid cooling of basaltic magma and are commonly found in oceanic crust and volcanic islands.
Pyroclasts can be formed by both basaltic and andesitic magma. Basaltic magma typically forms pyroclastic materials like scoria and ash, while andesitic magma can produce a variety of pyroclasts including volcanic bombs and pumice. The type of pyroclasts produced depends on factors such as the composition of the magma and the eruption style.
Igneous rocks containing mostly plagioclase feldspar and a significant percentage of dark silicate minerals are typically classified as basaltic rocks. These rocks have a composition that is intermediate between mafic and felsic rocks, with a silica content of around 50-60%. Basaltic rocks often form from the solidification of magma with a basaltic composition.