Datolite

Datolite is a collector that is unusual gem not often observed in the treasury market. Faceted gems are very brilliant despite the fact that their dispersion (fire) is low. It is found in basalt vesicles along with Calcite and Zeolites and is often confused with certain Zeolites because of its lustre, color and associations.

Although sources are worldwide, many Datolite gems come from US material. US sources are Hampden County, Massachusettes; Hartford County, Connecticut; Essex County and Passaic County, New Jersey; Loudoun County, Virginia. Worldwide sources are Arendal, Norway (the locality that is typed; Harz Mountains, Germany; Italy; Habachtal, Austria; Iwato Copper Mine, Japan; Charcas, San Luis Potosi, Mexico and exceptional, pale yellow crystals from Dal’negorsk, Primorskiy Kray, Russia.

Datolite can be found in the Lake Superior region of Michigan. It’s linked with indigenous copper as of this location and is found in porcelain-like masses and nodules. The nodules are brown to off-white in colour and some are cut and polished as a stone that is ornamental.

Category: Nesosilicate
Chemical formula: CaBSiO4(OH)
Crystallography: Monoclinic – Prismatic
Crystal Habit: Crystals typically short prismatic to wedge shaoed tabular, to 12 cm with complex faceted terminations. Also in porcelain-like masses or nodules; botryoidal or globular, having columnar structure; granular to compact; cryptocrystalline.
Twinning: None

 

Cleavage: None
Fracture: Conchoidal to Irregular/Uneven
Tenacity: Brittle
Hardness (Mohs): 5.0 – 5.5
Density: 2.96 – 3.00 (g/cm3)
Luminescence: None
Radioactivity: Not Radioactive

 

Color: Colorless, White, Brown, Yellow, Light Green
Transparency: Transparent to Translucent, nearly Opaque
Luster: Vitreous, Resinous
Refractive Index: 1.626 – 1.670  Biaxial ( – )
Birefringence: 0.0440
Ultraviolet fluorescence: Fluoresces blue under SW UV
Dispersion: Very Weak to None; r > v
Pleochroism: X = Colorless, Y = Colorless, Z = Colorless