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felsic

American  
[fel-sik] / ˈfɛl sɪk /

adjective

Geology.
  1. (of rocks) consisting chiefly of feldspars, feldspathoids, quartz, and other light-colored minerals.


felsic Scientific  
/ fĕlsĭk /
  1. Relating to an igneous rock that contains a group of light-colored silicate minerals, including feldspar, feldspathoid, quartz, and muscovite.

  2. Compare mafic


Etymology

Origin of felsic

First recorded in 1910–15; fel(dspar) + s(ilica) + -ic

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Example Sentences

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Although there are many exceptions to this trend, mafic magmas typically have 1% to 3% volatiles, intermediate magmas have 3% to 4% volatiles, and felsic magmas have 4% to 7% volatiles.

From Textbooks • Jan. 1, 2015

Figure 3.12 The chemical compositions of typical mafic, intermediate, and felsic magmas and the types of rocks that form from them.

From Textbooks • Jan. 1, 2015

The cooling behaviour of intermediate magmas lie somewhere between those of mafic and felsic magmas.

From Textbooks • Jan. 1, 2015

There it contributes to partial melting of crustal rock, and thus it assimilates much more felsic material.

From Textbooks • Jan. 1, 2015

Although mostly composed of felsic igneous rocks and gneisses, the Wopmay Orogen includes a body of mafic and ultramafic igneous rock called the Muskox Intrusion.

From Textbooks • Jan. 1, 2015

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