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Most anthodites are made of the mineral aragonite (a variety of calcium carbonate, CaCO 3), although some are composed of gypsum (CaSO 4 ·2H 2 O). The term anthodite is first cited in the scientific literature in 1965 by Japanese researcher N. Kashima, [1] who described "flower-like dripstone" composed of "an alternation of calcite and ...
A cave pearl is a small, usually spherical, speleothem (cave formation) found in limestone caves. Cave pearls are formed by a concretion of calcium salts that form concentric layers around a nucleus. Exposure to moving water polishes the surface of cave pearls, making them glossy; if exposed to the air, cave pearls can degrade and appear rough.
Calcite cannot persist without carbon dioxide, and chemical reactions are reversing. Ca+2 +2(HCO − 3) (in solution) --> CO 2 (gas) + H 2 O(water) + CaCO 3 (calcite) Calcite is then deposited. Calcite is known by various names depending on the shape it acquires. The calcite in the Diamond Caverns is known as Travertine. Dripstone is a phrase ...
Calcite is a carbonate mineral and the most stable polymorph of calcium carbonate (CaCO 3). It is a very common mineral, particularly as a component of limestone. Calcite defines hardness 3 on the Mohs scale of mineral hardness, based on scratch hardness comparison. Large calcite crystals are used in optical equipment, and limestone composed ...
The cavity, which measured 8.0 by 1.8 by 1.7 metres (26.2 ft × 5.9 ft × 5.6 ft), was, at the time, the largest crystal cave ever found. Following its discovery, the entrance to the cave was blocked by five tons of rock, with an additional police presence to prevent looters.
Amethyst crystals – a purple quartz Apophyllite crystals sitting right beside a cluster of peachy bowtie stilbite Aquamarine variety of beryl with tourmaline on orthoclase Arsenopyrite from Hidalgo del Parral, Chihuahua, Mexico Aurichalcite needles spraying out within a protected pocket lined by bladed calcite crystals Austinite from the Ojuela Mine, Mapimí, Durango, Mexico Ametrine ...
Peridotite (US: / ˈ p ɛ r ɪ d oʊ ˌ t aɪ t, p ə ˈ r ɪ d ə-/ PERR-ih-doh-tyte, pə-RID-ə-) is a dense, coarse-grained igneous rock consisting mostly of the silicate minerals olivine and pyroxene.
Calcite rafts are thin accumulations of calcite that appear on the surface of cave pools; Hells Bells, a particular speleothem found in the El Zapote cenote of Yucatan in the form of submerged, bell-like shapes; Lava tubes contain speleothems composed of sulfates, mirabilite or opal. When the lava cools, precipitation occurs.