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kolbeckite

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Also known as scandium phosphate dihydrate, eggonite, sterrettite

Kolbeckite (scandium phosphate dihydrate) is a mineral with formula: ScPO4·2H2O. It was discovered originally at Schmiedeberg, Saxony, Germany in 1926 and is named after Friedrich L. W. Kolbeck, a German mineralogist. Kolbeckite is usually found as small clusters of crystals associated with other phosphate minerals.

In the Vinony graph

Vinony's link graph records 10 inbound references to kolbeckite, and connects out to phosphate mineral, Germany and Saxony.

It sits within the topics Minerals in space group 14, Monoclinic minerals and Phosphate minerals.

Vinony links it to 12 Wikipedia language editions.

Key facts

Mineral.name
Kolbeckite
Mineral.image
Kolbeckite-215063.jpg
Mineral.imagesize
260px
Mineral.caption
Light-green spherical aggregates of microcrystals of Kolbeckite, to just over 1mm in size. Locality: Schlarbaum quarry, Klause, Bad Gleichenberg, Styria, Austria. Size: 4.9 x 3.9 x 2.3 cm.
Mineral.category
Phosphate minerals
Mineral.formula
ScPO4·2H2O
Mineral.IMAsymbol
Kbe
Mineral.strunz
8.CD.05
Mineral.system
Monoclinic
Mineral.class
Prismatic (2/m) (same H-M symbol)
Mineral.symmetry
P21/n

via Wikipedia infobox

Wikidata facts

Image
Kolbeckite-215064.jpg
Show 6 more facts
Commons category
Kolbeckite
chemical formula
ScPO₄·2H₂O
Nickel-Strunz '10th ed', review of (9th ed/ 2009 update)
8.CD.05
Nickel-Strunz 9th edition (updated 2009)
8.CD.05
IMA Mineral Symbol
Kbe
Strunz 8th edition (series ID, updated)
VII/C.05a

via Wikidata · CC0

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Encyclopedic overview

2 sections
Contents
  • See also
  • References

Kolbeckite (scandium phosphate dihydrate) is a mineral with formula: ScPO4·2H2O. It was discovered originally at Schmiedeberg, Saxony, Germany in 1926 and is named after Friedrich L. W. Kolbeck, a German mineralogist. Kolbeckite is usually found as small clusters of crystals associated with other phosphate minerals.

==See also== List of minerals List of minerals named after people

Excerpted from Wikipedia’s “kolbeckite” article, available under the CC BY-SA 4.0 licence.

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