Hydrated normal phosphate, monoclinic paramorph of orthorhombic scholzite
Specific gravity: 3.12 measured, 3.10 calculated
Colour: Colourless to white
Parascholzite is a secondary mineral produced by
alteration of primary phosphates in complex
At the type locality, the Hagendorf South Pegmatite, Hagendorf, Waidhaus, Neustadt an der Waldnaab District, Upper Palatinate, Bavaria, Germany, parascholzite was discovered on pegmatite specimens, where it occurs as well-developed crystals less than 1.0 mm in size associated with vivianite, phosphophyllite and strengite.
Parascholzite was first identified on a specimen in the Smithsonian collection. Subsequently it appeared that parascholzite also occurs, in some form, at all known scholzite locations (AM 66.843-851). Associated minerals include scholzite, vivianite, phosphophyllite and strengite (HOM).
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