Partial melting results in a magma that is nearer the felsic end of the compositional spectrum than the parent rock from which it was derived.
Although there are many different types of rocks in the Earth's crust, they may all be divided into two main groups: mafic rocks and felsic rocks. The composition of these rocks varies, and typically, their formation from lava or magma depends on their location.
Felsic rock
The words "feldspar" and "silica," which are frequently found in the makeup of felsic rocks, are the ancestors of the phrase "felsic." Felsic refers to igneous rocks that crystallize from magma or lava and are enriched with ingredients that can produce quartz and feldspar.
Rocks that are felsic can usually be distinguished by their color, texture, and other physical characteristics. The majority of felsic igneous rocks are pale in color, however, their textures can differ significantly.
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