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Basalt is mainly made of two minerals: Plagioclase feldspar and pyroxene . Basalt has several textural varieties such as glassy, massive, porphyritic, vesicular, scoriaceous.
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Application. The color of basalt is commonly black, dark brown, or dark green. The texture is dense, and its specific gravity is heavier than that of ordinary granite, limestone, sandstone, and shale.
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Type Igneous Rock Texture Aphanitic (Fine-grained) Origin Extrusive/Volcanic Chemical Composition Mafic Color Black Mineral Composition Calcium Plagioclase, Pyroxene, Olivine Tectonic Environment Divergent Boundary or Intra-oceanic hot spots
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Basalt is usually grey to black in colour, but rapidly weathers to brown or rust-red due to oxidation of its mafic (iron-rich) minerals into hematite and other iron oxides and hydroxides. Although usually characterized as "dark", basaltic rocks exhibit a wide range of shading due to regional geochemical processes.
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Basalt's texture is fine-grained due to its rapid cooling at or near the Earth's surface, resulting in an aphanitic texture where individual mineral grains are not visible to the naked eye.
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Example: Basalt porphyry. Vesicular volcanic rocks: Vesicular is the adjective used to modify the name of any fine-grained igneous (volcanic) rock which has vesicles (holes from gas bubbles), making a cinder-like or clinker-like appearance. Example: Vesicular basalt. Scoria: Basalt with over 50% vesicles. It looks like cinders.
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A seamless stone texture with a basalt surface. The image represents a physical area of 2200 x 1730 mm (86.6 x 68.1 inches) in total. Basalt is a distinctive, dark natural stone used commonly within architecture and construction. While historically used as a crushed aggregate material in roads, concrete, and railways, basalt has also become.
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Type Igneous Rock Texture Porphyritic Origin Extrusive/Volcanic Chemical Composition Mafic Color Dark Gray to Black Mineral Composition Calcium Plagioclase, Pyroxene Miscellaneous Calcium Plagioclase phenocrysts in an aphanitic (Fine-grained) groundmass Tectonic Environment Divergent Boundary or Intra-oceanic hot spots
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Black basalt (a kind of basalt) is created inland, mostly from enormous vents and fissures that deposit vast volumes of basaltic lava to the Earth's surface. These eruptions last for a long time and eventually result in vertical stacks or columns. Basalt Rock Cycle
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Basalt Basalt ( UK: / ˈbæsɔːlt, - əlt /; [1] US: / bəˈsɔːlt, ˈbeɪsɔːlt /) [2] is an aphanitic (fine-grained) extrusive igneous rock formed from the rapid cooling of low- viscosity lava rich in magnesium and iron ( mafic lava) exposed at or very near the surface of a rocky planet or moon. More than 90% of all volcanic rock on Earth is basalt.
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Basalt is a dark-colored, fine-grained, igneous rock composed mainly of plagioclase and pyroxene minerals. It most commonly forms as an extrusive rock, such as a lava flow, but can also form in small intrusive bodies, such as an igneous dike or a thin sill. It has a composition similar to gabbro.
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Basalt is known for its dark color, typically ranging from black to dark gray, and its fine-grained texture. It is composed mostly of minerals such as pyroxene, plagioclase feldspar, and sometimes olivine. Basalt can have a range of compositions, but it is typically rich in iron and magnesium, and low in silica. Vesicular and Amygdaloidal Textures
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Figure 4.1.1 4.1. 1: Granite is a classic coarse-grained (phaneritic) intrusive igneous rock. The different colors are unique minerals. The black colors are likely two or three different minerals. If magma cools slowly, deep within the crust, the resulting rock is called intrusive or plutonic.
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Black Basalt. Basalt is an igneous rock that forms when hot lava from a volcano cools down and hardens. It's made up of multiple minerals, including feldspar, quartz, and mica. Basalt is dark in color, ranging from black to dark grey, and has a very fine-grained texture. It's this unique combination of properties that gives basalt its many.