- Mafic
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Mafic is an adjective describing a silicate mineral or rock that is rich in magnesium and iron; the term is a portmanteau of the words "magnesium" and "ferric".[1] Most mafic minerals are dark in color and the relative density is greater than 3. Common rock-forming mafic minerals include olivine, pyroxene, amphibole, and biotite. Common mafic rocks include basalt, dolerite and gabbro.
In terms of chemistry, mafic rocks are on the other side of the rock spectrum from the felsic rocks. The term roughly corresponds to the older basic rock class.
Mafic lava, before cooling, has a low viscosity, in comparison to felsic lava, due to the lower silica content in mafic magma. Water and other volatiles can more easily and gradually escape from mafic lava, so eruptions of volcanoes made of mafic lavas are less explosively violent than felsic-lava eruptions. Most mafic-lava volcanoes are oceanic volcanoes, like those in Hawaii.
Rock Texture Name of Mafic Rock Pegmatitic Gabbro pegmatite Coarse grained (phaneritic) Gabbro Coarse grained and porphyritic Porphyritic gabbro Fine grained (aphanitic) Basalt Fine grained and porphyritic Porphyritic basalt Pyroclastic Basalt tuff or breccia Vesicular Vesicular basalt Amygdaloidal Amygdaloidal basalt Many small vesicles Scoria Glassy Tachylyte, sideromelane, palagonite See also
References
Igneous rocks by composition Type Ultramafic
< 45% SiO2Mafic
45-52% SiO2Intermediate
52–63% SiO2Intermediate-Felsic
63–69% SiO2Felsic
>69 % SiO2Volcanic rocks:
Subvolcanic rocks:
Plutonic rocks:Categories:- Mineralogy
- Igneous petrology
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