Igneous rocks
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Mafic vs felsic
mafic- finely crystalline (cooled fast) (extrusive) felsic- coarsely crystalline (cooled slow) (intrusive) extrusive- basalt, obsidian intrusive- granite, diorite
Igneous Rocks
form from the cooling and solidification of magma (underneath the earth’s surface) or lava (outside of earth’s surface)
Cooling rate and texture
fast cooling=small or no crystals (ex: aphanitic (fine-grained) and glassy (obsidian)) slow cooling= large crystals (ex: phaneritic (coarse-grained))
composition
mafic: low silica/ rich in iron and magnesium/ dark color (ex: basalt, gabbro) andesitic: moderate sillica/ medium color (ex: andesite, diorite) felsic: high sillica/ light color/ rich in quartz and feldspar (ex: granite, rhyolite) ultramafic: very low sillica/ very high mg & fe/ rare at surface (ex: periodtite)
textures
aphanitic: fine grained phaneritic: coarse grained porphyritic: mixed crystal sizes glassy: no crystals (obsidian) vesicular: gas bubbles (pumice, scoria)
plutons/ intrusions
dike: vuts across rock layers (vertical or steep) sill: parallel to rock layers (horizontal) laccolith: dome-shaped intrusion pushing layers upward batholith: massive, deep intrusion (largest type)