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Granodiorite, tonalite, Syenite
kimberlite
Olivine gabbro
pegmatite
Leucogranite (light colored granite)
Red Granite (alkali feldspars))
Spilite Pillow Basalt
Dacite
felsic extrusive; composed of plagioclase feldspar and Qtz, and hornblende
formed rapid solidification of lava along subduction zones
Diabase Porphyry
“Porphyritic texture” larger crystals in a fine grained matrix
Formed by magma cooling slowly underground allowing (phenocrysts) crystals to grow, followed by rapid cooling near surface resulting in fine grained groundmass
Diabase: intrusive igneous rock with basaltic composition
Aplite
fine grained light colored intrusive igneous rock (Qtz, and feldsbar)
Leftover magma fills in fractures of surrounding rock, resulting in. quick cooling.
Dunite
Primary composed of olivine
dense early crystalizing grains of olivine
Amygdaloidal Basalt
basalt with Amygdaloidal which are vesicles filled by small mineral (calcite, Qtz), originally gas bubbles.
Pumice
glassy lava solidifies rapidly trapping gas bubbles
Obsidian
volcanic glass,
formed when lava cools rapidly, sharp edges becasue of conchoidal fracture.
Basalt (porphyritic)
Epidosite
Augen gneiss
graphite schist
Metachert (hornblende)
gneiss (foliated banding) bio, garnet, Qtz, with sill intergrowths
Garnetite
serpentine
Spotted Phylitte
Eclogite
Blue Calcite
Marble; Dolomite meta to octahedral
Muscovite
Metaquartz chert Carbonate rock
Greenstone
Eclogite
Blueschist
Spotted slate
Chloritoid Schist
Mica Schist
Eclogite (christmas tree)
Amphibolite (hornblende) Schist
gabbro
dark colored, course grained igneous (plag, pyroxene, and minor amounts of olivine)
Kimberlite
Ultramafic: olivine, serpentine, calcite, mice