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  2. Listwanite - Wikipedia

    en.wikipedia.org/wiki/Listwanite

    Listwanite (also sometimes spelled listvenite, listvanite, or listwaenite) is a rock type that forms when the groundmass of ultramafic rocks, most commonly mantle peridotites, is partially altered to carbonate minerals and cut by ubiquitous carbonate veins containing one or more of magnesite, calcite, dolomite, ankerite, and/or siderite.

  3. Dragon's blood - Wikipedia

    en.wikipedia.org/wiki/Dragon's_blood

    Dragon's blood. Dragon's blood is a bright red resin which is obtained from different species of a number of distinct plant genera: Calamus spp. (previously Daemonorops) also including Calamus rotang, Croton, Dracaena and Pterocarpus. The red resin has been in continuous use since ancient times as varnish, medicine, incense, pigment, and dye .

  4. Orpiment - Wikipedia

    en.wikipedia.org/wiki/Orpiment

    Orpiment, also known as ″ yellow arsenic blende ″ is a deep-colored, orange-yellow arsenic sulfide mineral with formula As. 2S. 3. It is found in volcanic fumaroles, low-temperature hydrothermal veins, and hot springs and may be formed through sublimation . Orpiment takes its name from the Latin auripigmentum ( aurum, "gold" + pigmentum ...

  5. Orogenic gold deposit - Wikipedia

    en.wikipedia.org/wiki/Orogenic_gold_deposit

    An orogenic gold deposit is a type of hydrothermal mineral deposit. More than 75% of the gold recovered by humans through history belongs to the class of orogenic gold deposits. [ 1] Rock structure is the primary control of orogenic gold mineralization at all scales, as it controls both the transport and deposition processes of the mineralized ...

  6. Cristobalite - Wikipedia

    en.wikipedia.org/wiki/Cristobalite

    Specimen from California, US; size: 5.9 cm × 3.8 cm × 3.8 cm (2.3 in × 1.5 in × 1.5 in). Cristobalite ( / krɪˈstoʊbəˌlaɪt /) is a mineral polymorph of silica that is formed at very high temperatures. It has the same chemical formula as quartz, SiO 2, but a distinct crystal structure. Both quartz and cristobalite are polymorphs with ...

  7. Epidote - Wikipedia

    en.wikipedia.org/wiki/Epidote

    Epidote is an abundant rock-forming mineral, but one of secondary origin. It occurs in marble and schistose rocks of metamorphic origin. It is also a product of hydrothermal alteration of various minerals ( feldspars, micas, pyroxenes, amphiboles, garnets, and others) composing igneous rocks. A rock composed of quartz and epidote is known as ...

  8. Category:Metaphysical properties - Wikipedia

    en.wikipedia.org/wiki/Category:Metaphysical...

    Main page; Contents; Current events; Random article; About Wikipedia; Contact us; Donate; Pages for logged out editors learn more

  9. CAS won't reconsider ruling that effectively stripped Jordan ...

    www.aol.com/jordan-chiles-wont-keep-bronze...

    After disputed score on floor exercise triggered series of conflicting rulings, Court of Arbitration for Sport won't reconsider decision on Chiles.

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