-40%

Rare Rutilated Quartz Golden included,18.42ct 25x12mm,Brazil,flat, slice

$ 6.33

Availability: 100 in stock
  • Country of Manufacture: Brazil
  • Carat Range: Greater than 6.00
  • Restocking Fee: No
  • Refund will be given as: Money Back
  • Country/Region of Manufacture: Brazil
  • Condition: Stone is brand new never set in Jewelry, rare type of Rutilated needles.
  • Return shipping will be paid by: Buyer
  • Treatment: Not Enhanced
  • Color: Rutilated
  • All returns accepted: Returns Accepted
  • Item must be returned within: 30 Days

    Description

    Quartz grows in many environments along with many different minerals. These minerals, as well as watery solutions and gas bubbles, can be enclosed by the growing crystal.
    Many minerals that would otherwise be chemically altered or dissolved when the local conditions change are protected from aggressive chemical agents when they have been embedded inside quartz crystals. Likewise, fragile minerals that are very soft, crumbly or that occur as fibers or thin needles survive inside. Other partially embedded minerals might get dissolved at a later stage and leave ghostlike hollow forms behind.
    There are basically three ways inclusions can "get into the crystal":
    The minerals have formed before the quartz. The growing quartz crystals engulfs them and the original form of the included minerals is preserved. These inclusions are called
    protogenetic
    . Included fibers than run through the entire crystal at random orientations are typical examples.
    Quartz crystals and the included minerals grow simultaneously. These inclusions are called
    syngenetic
    . The shape of the included minerals often deviates from the typical forms and habits that develop during unhindered growth. Crystals may be distorted beyond recognition and a non-destructive identification may pose a real problem even for a mineralogist.
    Sometimes inclusions cause the formation of phantoms. Here the quartz crystal might have been partially encrusted by another mineral when growth halted transiently and continued later, such a case could be considered a syngenetical formation that got overgrown.