what is a hypocarbonite?
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it appears to be the name of the CO-2 ion. (-2 is the charge).
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B, though its even more common as K2Cr2O7\n\nby coincidence, C, Na and H2 happen to be quite good reducing agents.
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Mecaline is a chemical compound, not a mineral. I am unaware of any mineral which has hallucinatory properties.
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cation, a negatively charged ion would be an anion...
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All three are found as extrusive igneous rocks, meaning they are formed by volcanic activity. Carbonatites are mostly intrusive, meaning they formed beneath the surface by igneous processes. \n\nPhonolite is intermediate between felsic and mafic in composition. \nTrachyte is mostly sanidine feldspar, with little or no quartz, and mafic minerals such as augite and hornblende. \nCarbonatites contain more than 50% carbonate minerals.
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CaSO4\nIt's also known as Plaster of Paris or Gypsum.
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Igneous rocks in which the molecular proportion of aluminum oxide is less than that of sodium and potassium oxides combined
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calcium carbonate...\n\ncalcium and carbon....
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It is the other way around. Calcium atoms ARE present in bones.
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A mineraloid is a mineral-like substance that does not demonstrate crystallinity. Mineraloids possess chemical compositions that vary beyond the generally accepted ranges for specific minerals.\n\n Some examples of mineraloids are: Obsidian, Opal and Limonite.
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phosphorous acid--\n\na yellowish hygroscopic solid, H3PO3; a mild reducing agent
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Bleach\nsodium hyporchlorite has HCL in it\nMuritic acid
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A meteorite is an extraterrestrial body that survives its impact with the Earth's surface without being destroyed. While in space it is called a meteoroid. When it enters the atmosphere, air resistance causes the body to heat up and emit light, thus forming a fireball, also known as a meteor or shooting star.
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sodium bicarbonate \nits chemical compound, NaHCO3, which is a white crystalline or granular powder, commonly known as bicarbonate of soda or baking soda. It is soluble in water and very slightly soluble in alcohol.
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Saprolite ? -- a soft, earthy, clay-rich thoroughly decomposed rock formed in place by chemical weathering of igneous or metamorphic rocks\n\nC-horizon (soils) ? -- partially disintegrated parent material and mineral particles are in this horizon. C horizons may also be called "parent material".\n\nOverburden ? - engineering term for anything not bedrock\n\nOh, yeah, generally decomposed rocks are called soils.  Maybe I'm being too specific.
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check out the wikipedia link below:\n\nBauxite is a naturally occurring, heterogeneous material composed primarily of one or more aluminium hydroxide minerals, plus various mixtures of silica, iron oxide, titania, aluminium silicates, and other impurities in minor or trace amounts.\n\nThe bulk of world bauxite production (approximately 85%) is processed into aluminium oxide (Al2O3, also known as alumina) via a wet chemical, caustic leach method (the Bayer process).
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Attached source has an array of information:\n\nA xenocryst is an individual foreign crystal included within an igneous body. Examples of xenocrysts are quartz crystals in a silica deficient lava and diamonds within kimberlite diatremes.\n\nAlthough xenolith is most commonly associated with igneous inclusions, a broad definition could include rock fragments which have become encased in sedimentary rock. Xenoliths are sometimes found in recovered meteorites.\n\n \nA xenolith in Larchmont, New YorkTo be considered a true xenolith, the included rock must be identifiably different from the rock in which it is enveloped; an included rock of similar type is called an autolith.\n\nXenoliths and xenocrysts provide important information about the composition of the otherwise innacessible mantle. Basalts, kimberlites, lamproites and lamprophyres which have their source in the upper mantle often contain fragments and crystals assumed to be a part of the originating mantle mineralogy.