Tilleyite

Tilleyite is a rare calcium silicate carbonate mineral that is rarely (if ever) transparent but may occassionally be found as small white translucent crystals that can make attractive gems for collectors of the unusual. It is always white by itself but may appear pale bluish-white when associated with blue Calcite at the type locality of Crestmore, Riverside County, California. The best location for gem quality crystals is from Redcap Creek, Queensland, Australia.

Locations for Tilleyite include the type locality of Crestmore, Riverside County, California; North Peak, Iron Mountains, Sierra County, New Mexico; and near Helena, Lewis and Clark County, Montana, USA. In Ireland, at Barnavave, near Carlingford, County Louth. From near Kilchoan, Ardnamurchan, Argyllshire, and Camas Mòr, Isle of Muck, also on the Isles of Skye and Rhum, Scotland. From the Güneyce-Ikizdere area, Trabzon Province, Turkey. In Russia, from near Anakit Creek, at the mouth of the Lower Tunguska River, central Siberia, and several other less-well-defined localities. At Kushiro, Hiroshima Prefecture, and the Akagané mine, Iwate Prefecture, Japan; and from Redcap Creek, Queensland, Australia.

Chemical Formula: Ca5Si2O7(CO3)2
Calcium Silicate Carbonate
Molecular Weight: 488.58 gm
Composition: Calcium 41.02 % Ca 57.39 % CaO
Silicon 11.50 % Si 24.60 % SiO2
Carbon 4.92 % C 18.02 % CO2
Oxygen 42.57 % O
  100.00 % 100.00 % = TOTAL OXIDE

 

Crystallography: Monoclinic – Prismatic
Crystal Habit: As subhedral crystals, rounded grains, and irregular plates.
Twinning: On {100}, simple; rarely, lamellar

 

Cleavage: Perfect on {201}; poor on {100} and {010}; very poor on {001}
Fracture: No data
Tenacity: Brittle
Moh’s Hardness: No data
Density: 2.82 – 2.84 (g/cm3)
Luminescence: None
Radioactivity: Not Radioactive

 

Color: White, Colorless in thin section
Transparency: Translucent to Transparent
Luster: Vitreous, Dull
Refractive Index: 1.612 – 1.654  Biaxial (+)
Birefringence: 0.0370 – 0.0400
Dispersion: Perceptible; r < v
Pleochroism: None