granodiorite - teaching student specimens - Unit of 5 specimens
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This granitic rock differs from granite, since it normally has very little orthoclase, and with plagioclase being the predominant feldspar. In granite, orthoclase is the predominant feldspar and it is this feldspar that gives many granites their pink color. Quartz makes up more than 20% of the composition of both granite and granodiorite and both rocks can have the dark minerals biotite and hornblende, though these dark minerals make up a greater percentage of the composition of granodiorite. This granodiorite has abundant biotite, some hornblende and has a surprisingly large amount of orthoclase feldspar. Its quartz content is about 15%.
Granodiorite typically originates above a subduction zone from the fractional melting of the iron and magnesium-rich mantle wedge above the subducting plate. It forms large batholiths covering thousands of square miles. This granodiorite is from the Sierra Nevada batholith in California, which was intruded during the Jurassic and subsequently uplifted over five miles. The top two miles have been stripped off by erosion and weathering to expose this rock.
When a granodiorite magma reaches the surface it forms the andesite lavas of composite volcanos such as Mount St. Helens, Vesuvius and Mt. Fuji.
The irregular black mineral in these specimens is biotite mica. The rectangular black crystals are hornblende. For beginning geology or grade school students, recognizing this as a "granitic rock," in the family of granite, is an acceptable outcome. They should be able to tell the biotite from hornblende. Geology majors in a petrology course should be able to come up with the exact name.
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