Amazonit<\/a> ist eine auff\u00e4llige Feldspatart, die f\u00fcr ihre charakteristische blaugr\u00fcne Farbe bekannt ist. Der Stein ist nach dem Amazonas benannt, obwohl es in diesem Gebiet keine bekannten Vorkommen gibt. Die Farbe reicht von zartem T\u00fcrkis bis zu tiefem Gr\u00fcnblau und wird durch das Vorhandensein von Blei und Wasser in der Kristallstruktur verursacht. H\u00e4ufig weist Amazonit ein leicht gestreiftes oder gesprenkeltes Muster auf, was zu seinem einzigartigen Aussehen beitr\u00e4gt.<\/p>\n Belangrijke vindplaatsen van amazoniet zijn onder andere Brazili\u00eb, Madagaskar, Rusland, China en de Verenigde Staten. De meest heldere en intens gekleurde exemplaren komen vaak uit Colorado en Madagaskar. Geologisch gezien ontstaat amazoniet in pegmatieten, grofkorrelige magmatische gesteenten die rijk zijn aan mineralen. De chemische formule van amazoniet is K(AlSi\u2083O\u2088), en het behoort tot de microklien-feldspaten. Met een hardheid van 6 tot 6,5 op de schaal van Mohs.<\/p>\n Quellen: <\/strong>Mindat.org<\/a>, Gemdat.org<\/a>, Wikipedia \u2013 Amazonit<\/a><\/small><\/p>","protected":false},"excerpt":{"rendered":" Amazoniet Amazoniet is een opvallende vari\u00ebteit van veldspaat die bekend staat om zijn kenmerkende blauwgroene kleur. De steen is genoemd naar de Amazone, hoewel er geen afzettingen in dat gebied bekend zijn. De kleur varieert van zacht turquoise tot diep groenblauw en wordt veroorzaakt door de aanwezigheid van lood en water in de kristalstructuur. 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