| Igneous rock | |
 A sample of andesite (dark groundmass) with amygdaloidal vesicles filled with zeolite. Diameter of view is 8 cm. | |
| Composition | |
|---|---|
| Primary | Intermediate: plagioclase (often andesine) and pyroxene or hornblende |
| Secondary | Magnetites, biotite, sphene, and quartz |
Andesite (/ˈændəzaɪt/)[1] is a volcanic rock of intermediate composition. In a general sense, it is the intermediate type between silica-poor basalt and silica-rich rhyolite. It is fine-grained (aphanitic) to porphyritic in texture, and is composed predominantly of sodium-rich plagioclase plus pyroxene or hornblende.[2]
Andesite is the extrusive equivalent of plutonic diorite. Characteristic of subduction zones, andesite represents the dominant rock type in island arcs. The average composition of the continental crust is andesitic.[3] Along with basalts, andesites are a component of the Martian crust.
The name andesite is derived from the Andes mountain range, where this rock type is found in abundance. It was first applied by Christian Leopold von Buch in 1826.[4]
- ^ "andesite". Merriam-Webster.com Dictionary. Merriam-Webster.
- ^ Macdonald, Gordon A.; Abbott, Agatin T.; Peterson, frank L. (1983). Volcanoes in the sea : the geology of Hawaii (2nd ed.). Honolulu: University of Hawaii Press. p. 127. ISBN 0824808320.
- ^ Rudnick, Roberta L.; Fountain, David M. (1995). "Nature and composition of the continental crust: A lower crustal perspective". Reviews of Geophysics. 33 (3): 267–309. Bibcode:1995RvGeo..33..267R. doi:10.1029/95RG01302.
- ^ Jackson, Julia A., ed. (1997). "andesite". Glossary of geology (Fourth ed.). Alexandria, Virginia: American Geological Institute. ISBN 0922152349.