Formed by interaction of phosphate solutions derived from quano with micacous and chloritic minerals in soil under a penguin rookery.
IMA Status:
Approved IMA 1986
Locality:
On Elephant Island, South Shetland Islands, about 800 km southeast of Cape Horn, British Antarctic Territory, Antartica. Link to MinDat.org Location Data.
Name Origin:
Named for "Sphenisciformes," the Latin order name or penguins.
Name Pronunciation:
Spheniscidite + Pronunciation
Synonym:
ICSD 75229
PDF 41-593
Spheniscidite Crystallography
Axial Ratios:
a:b:c =1.0124:1:1.0072
Cell Dimensions:
a = 9.75, b = 9.63, c = 9.7, Z = 4; beta = 102.567° V = 888.94 Den(Calc)= 3.09
Selvage - As a reaction rim, surrounding the host mineral.
Hardness:
1-1.5 - Talc or a little harder
Luster:
Earthy (Dull)
Streak:
white
Optical Properties of Spheniscidite
Gladstone-Dale:
CI meas= -0.053 (Good) - where the CI = (1-KPDmeas/KC) CI calc= 0.077 (Fair) - where the CI = (1-KPDcalc/KC)
KPDcalc= 0.2265,KPDmeas= 0.2583,KC= 0.2453 Ncalc = 1.66 - 1.76
Optical Data:
Biaxial (?), b=1.7
Calculated Properties of Spheniscidite
Electron Density:
Bulk Density (Electron Density)=2.71 gm/cc note: Specific Gravity of Spheniscidite =2.71 gm/cc.
Fermion Index:
Fermion Index = 0.02 Boson Index = 0.98
Photoelectric:
PESpheniscidite = 7.99 barns/electron U=PESpheniscidite x relectron= 21.63 barns/cc.
Radioactivity:
GRapi = 54.53 (Gamma Ray American Petroleum Institute Units)
Concentration of Spheniscidite per GRapi unit = 1.83 (%)
Estimated Radioactivity from Spheniscidite - barely detectable
Spheniscidite Classification
Dana Class:
42.11.06.03(42)Hydrated Phosphates, etc., Containing Hydroxyl or Halogen