Extrusive Igneous Rocks

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Extrusive igneous rocks, additionally referred to as volcanic rocks, are fashioned on the crust’s surface due to the partial melting of rocks within the mantle and crust. Extrusive Igneous Rocks are listed below.

Volcanic Bomb

Volcanic bomb is pyroclastic rock that is a cooling of a mass of lava it flies thorough...

Agglomerate

Andesite agglomerate Agglomerate is a pyroclastic coarse accumulation of blocks of volcanic metarial that contains atl least 75%...

Scoria

Red scoria Scoria is vesicular and dark colored igneous rock that have or have not contain any crystals. ...

Pumice

Pumice is a volcanic rock that consists of highly vesicular rough textural rock glass. It generally light...

Lamprophyre

Camptonite lamprophyre (Mesozoic, 100-200 Ma; Campton Falls, Grafton County
Lamprophyre is ultrapotassic igneous rock that is occurring as dikes, lopoliths, loccoliths, stocks and small intrussion. It...

Pyroxenite

Pyroxenite (Stillwater Complex, Neoarchean)
Microcline-bearing pyroxenite Pyroxenite (Stillwater Complex, Neoarchean) Pyroxenite is an ultramafic igneous rock that contain pyroxene group minerals...

Obsidian

Obsidian is an igneous rock that forms when molten rock material cools so rapidly that atoms are unable to arrange themselves into a crystalline structure. It is an amorphous material known as a "mineraloid." The result is a volcanic glass with a smooth uniform texture that breaks with a conchoidal fracture .

Basalt

Basalt Columns in Boyabat, Sinop, Turkey
Basalt is the most common rock on Earth’s surface. Specimens are black in color and weather to dark green or brown. Basalt is rich in iron and magnesium and is mainly composed of olivine, pyroxene, and plagioclase. Most specimens are compact, fine-grained, and glassy. They can also be porphyritic, with phenocrysts of olivine, augite, or plagioclase. Holes left by gas bubbles can give basalt a coarsely porous texture.