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Basalt is a hard, fine-grained, dark-colored volcanic or extrusive rock. It has primarily calcium-rich plagioclase and augite. Also, it may have minor amounts of other minerals like quartz, olivine, foids, alkali feldspar, biotite, and amphibole. This rock is undoubtedly popular, only rivaled by granite.


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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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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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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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This Dark Basalt has a flamed and waterjet finish. It is ideal for those wanting a natural look for their tiles. The surface of the stone is initially heated to an extremely high temperature causing the little crystals on the surface of the tile to split. The effect is a slightly textured, soft-toned Basalt.


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Basalt is an extrusive igneous rock composed primarily of plagioclase feldspar and large amounts of mafic minerals like pyroxene. It has an aphanitic texture, meaning its interlocking crystals cannot be seen by the naked eye. It is usually dark gray, black, or dark greenish, and is often vesicular or porphyritic.


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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 (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 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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Yes, Italys Pietra Lavica Basalt can be used in landscaping. Pietra Lavica Basalt is a volcanic stone that is known for its durability and natural beauty. Its dark color and unique texture make it a popular choice for various landscaping applications such as paving, wall cladding, decorative features, and outdoor furniture.


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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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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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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.