alb3843533

Hornblende Gabbro, Massachusetts

Gabbro is a coarse grained, equigranular igneous rock composed mainly of plagioclase feldspar (labradorite or bytownite) and orthoclase, a pyroxene such as augite, sometimes also nepheline and olivine, and a large percentage of hornblende (in hornblende gabbro). Rocks of this type are sometimes known as essexite. Gabbro forms as a result of the slow and undisturbed cooling of magma (molten rock) deep underground.
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Title: Hornblende Gabbro, Massachusetts
Caption: Gabbro is a coarse grained, equigranular igneous rock composed mainly of plagioclase feldspar (labradorite or bytownite) and orthoclase, a pyroxene such as augite, sometimes also nepheline and olivine, and a large percentage of hornblende (in hornblende gabbro). Rocks of this type are sometimes known as essexite. Gabbro forms as a result of the slow and undisturbed cooling of magma (molten rock) deep underground.
Credit: Album / Science Source / JOEL AREM
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Image size: 3841 × 2550 px | 28.0 MB
Print size: 32.5 × 21.6 cm | 1512.2 × 1003.9 in (300 dpi)
Keywords: AREM COLLECTION COOLING EQUIGRANULAR ESSEXITE FEATURE GABBRO GEOLOGIA GEOLOGIC GEOLOGICAL GEOLOGY GRAIN GRAINS HISTORY HORNBLENDE IGNEOUS MASSACHUSETTS MINERALOGY NECK NECKS NEPHELINE ORTHOCLASE PROPERTIES REPORTAGE ROCK ROCKS SALEM SIZE SPECIMEN TEXTURE THROAT