Occurs as a secondary mineral on specimens from a mine dump (Neubulach, Germany).
IMA Status:
Approved IMA 1981
Locality:
From Neubulach, and in the Clara mine, near Oberwolfach, Black Forest, Germany. At the Centennial Eureka mine, Tintic district, Juab Co., Utah, USA. Link to MinDat.org Location Data.
Name Origin:
For "arsenic" in the composition, and relation to "crandallite."
Conchoidal - Fractures developed in brittle materials characterized by smoothly curving surfaces, (e.g. quartz).
Hardness:
5.5 - Knife Blade
Luster:
Vitreous (Glassy)
Streak:
white
Optical Properties of Arsenocrandallite
Gladstone-Dale:
CI meas= 0.086 (Poor) - where the CI = (1-KPDmeas/KC) CI calc= 0.249 (Poor) - where the CI = (1-KPDcalc/KC)
KPDcalc= 0.1578,KPDmeas= 0.1923,KC= 0.2103 Ncalc = 1.68 - 1.83
Optical Data:
Uniaxial (?), a=1.625, b=1.625, bire=0.0000.
Calculated Properties of Arsenocrandallite
Electron Density:
Bulk Density (Electron Density)=3.15 gm/cc note: Specific Gravity of Arsenocrandallite =3.25 gm/cc.
Fermion Index:
Fermion Index = 0.0081080124 Boson Index = 0.9918919876
Photoelectric:
PEArsenocrandallite = 27.09 barns/electron U=PEArsenocrandallite x rElectron Density= 85.28 barns/cc.
Radioactivity:
GRapi = 0 (Gamma Ray American Petroleum Institute Units) Arsenocrandallite is Not Radioactive
Arsenocrandallite Classification
Dana Class:
42.07.04.01(42)Hydrated Phosphates, etc., Containing Hydroxyl or Halogen