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  2. Peridotite - Wikipedia

    en.wikipedia.org/wiki/Peridotite

    Peridotite. Peridotite (US: / ˈpɛrɪdoʊˌtaɪt, pəˈrɪdə -/ PERR-ih-doh-tyte, pə-RID-ə-) is a dense, coarse-grained igneous rock consisting mostly of the silicate minerals olivine and pyroxene. Peridotite is ultramafic, as the rock contains less than 45% silica. It is high in magnesium (Mg 2+), reflecting the high proportions of ...

  3. Peridot - Wikipedia

    en.wikipedia.org/wiki/Peridot

    Peridot. Peridot (/ ˈpɛrɪˌdɒt, - ˌdoʊ / PERR-ih-dot, -⁠⁠doh), sometimes called chrysolite, is a yellow-green transparent variety of olivine. Peridot is one of the few gemstones that occur in only one color. Peridot can be found in mafic and ultramafic rocks occurring in lava and peridotite xenoliths of the mantle.

  4. Diplodactylus vittatus - Wikipedia

    en.wikipedia.org/wiki/Diplodactylus_vittatus

    Diplodactylus vittatus are insectivores, meaning their primary diet consists of insects which the species actively hunt by either catching their prey with their tongue or closing their jaw. [ 3 ] [ 10 ] Diplodactylus vittatus foraging activity is temperature dependent having a narrow air and substrate temperature range of between 17°C and 26 ...

  5. How To Cleanse and Recharge Crystals at Home, According to ...

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  6. Kimberlite - Wikipedia

    en.wikipedia.org/wiki/Kimberlite

    Kimberlite occurs in the Earth's crust in vertical structures known as kimberlite pipes, as well as igneous dykes and can also occur as horizontal sills. Kimberlite pipes are the most important source of mined diamonds today. The consensus on kimberlites is that they are formed deep within the mantle.

  7. Gemstone irradiation - Wikipedia

    en.wikipedia.org/wiki/Gemstone_irradiation

    Gemstone irradiation is a process in which a gemstone is exposed to artificial radiation in order to enhance its optical properties. High levels of ionizing radiation can change the atomic structure of the gemstone's crystal lattice, which in turn alters the optical properties within it. [1] As a result, the gem­stone's color may be ...