Erythrite

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Erythrite crystallizes in the monoclinic system and forms prismatic crystals. The color is crimson to pink and occurs as a secondary coating known as cobalt bloom on cobalt arsenide minerals. Well-formed crystals are rare, with most of the mineral manifesting in crusts or small reniform aggregates.

Erythrite was first described in 1832 for an occurrence in Grube Daniel, Schneeberg, Saxony, and takes its name from the Greek έρυθρος (erythros), meaning red. Historically, erythrite itself has not been an economically important mineral, but the prospector may use it as a guide to associated cobalt and native silver.[citation needed]
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  • Erythrin

    Erythrin

    Erythrin (veraltet auch...

    Object information
    Image: Museum für Naturkunde Chemnitz - CC BY-SA

  • Eritrin

    Eritrin

    Rózsaszín, fénytelen bevonatok

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    Image: Herman Ottó Múzeum - CC BY-NC-SA

  • Eritrin

    Eritrin

    Halványvörös, mm alatti tűs...

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    Image: Herman Ottó Múzeum - CC BY-NC-SA

  • Eritrin

    Eritrin

    Rózsaszín kivirágzások

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    Image: Herman Ottó Múzeum, Miskolc - CC BY-NC-SA

  • Eritrin

    Eritrin

    Rózsaszín bevonatok

    Object information
    Image: Herman Ottó Múzeum, Miskolc - CC BY-NC-SA

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