Search results
Results from the WOW.Com Content Network
H 2 O + CO 2 → H 2 CO 3. As the acidic water travels through the calcium carbonate bedrock from the surface to the cave ceiling, it dissolves the bedrock via the reaction: CaCO 3 + H 2 CO 3 → Ca 2+ + 2 HCO 3 −. When the solution reaches a cave, the lower pCO 2 in the cave drives the precipitation of CaCO 3 via the reaction: Ca 2+ + 2 HCO ...
Mineralogy applies principles of chemistry, geology, physics and materials science to the study of minerals. Mineralogy [n 1] is a subject of geology specializing in the scientific study of the chemistry, crystal structure, and physical (including optical) properties of minerals and mineralized artifacts.
Orthoclase feldspar (KAlSi 3 O 8) is a mineral commonly found in granite, a plutonic igneous rock. When exposed to weathering, it reacts to form kaolinite (Al 2 Si 2 O 5 (OH) 4, a sedimentary mineral, and silicic acid): 2 KAlSi 3 O 8 + 5 H 2 O + 2 H + → Al 2 Si 2 O 5 (OH) 4 + 4 H 2 SiO 3 + 2 K +
Rocks are composed primarily of grains of minerals, which are crystalline solids formed from atoms chemically bonded into an orderly structure. [4]: 3 Some rocks also contain mineraloids, which are rigid, mineral-like substances, such as volcanic glass, [5]: 55, 79 that lack crystalline structure. The types and abundance of minerals in a rock ...
Nacre is composed of hexagonal platelets of aragonite (a form of calcium carbonate) 10–20 μm wide and 0.5 μm thick arranged in a continuous parallel lamina. [2] Depending on the species, the shape of the tablets differs; in Pinna , the tablets are rectangular, with symmetric sectors more or less soluble.
Ringwoodite is polymorphous with forsterite, Mg 2 SiO 4, and has a spinel structure.Spinel group minerals crystallize in the isometric system with an octahedral habit. Olivine is most abundant in the upper mantle, above about 410 km (250 mi); the olivine polymorphs wadsleyite and ringwoodite are thought to dominate the transition zone of the mantle, a zone present from about 410 to 660 km
It can be represented by the chemical formula of Fe Cr 2 O 4. It is an oxide mineral belonging to the spinel group. The element magnesium can substitute for iron in variable amounts as it forms a solid solution with magnesiochromite (Mg Cr 2 O 4). [6] Substitution of the element aluminium can also occur, leading to hercynite (Fe Al 2 O 4). [7]
Trachyte (/ ˈ t r eɪ k aɪ t, ˈ t r æ k-/) is an extrusive igneous rock composed mostly of alkali feldspar.It is usually light-colored and aphanitic (fine-grained), with minor amounts of mafic minerals, [1] and is formed by the rapid cooling of lava (or shallow intrusions) enriched with silica and alkali metals.