Searlesite

Searlesite is a rare silicate mineral that is rarely available faceted due to its soft and fibrous nature. It is not an attractive gem but one that is for collectors of the very unusual. Searlesite is a Piezoelectric mineral, meaning that it has the ability to generate a voltage in response to applied mechanical stress. Relatively large crystals are usually flat and fibrous and occur along bedding planes. Tiny transparent prismatic crystals are much too small for faceting.

Searlesite can be found in the USA, at Searles Lake, San Bernardino County, in the Kramer borate deposit, Kern County, and at Lake Tecopa, Inyo County, California; widespread in the Green River Formation of Utah and Wyoming; from Cave Springs Wash, Silver Peak Range, Esmeralda County, Nevada; and at Point of Rocks, Colfax County, New Mexico. In Canada, at Mont Saint-Hilaire, Quebec. From Kremna, near Tito Uzice; Lopare; and near Bela Stena, Yugoslavia.

Category: Phyllosilicate
Chemical Formula: NaBSi2O5(OH)2
Sodium Boron Silicate Hydroxide
Molecular Weight: 203.98 gm
Composition: Sodium 11.27 % Na 15.19 % Na2O
Silicon 27.54 % Si 58.91 % SiO2
Boron 5.30 % B 17.06 % B2O3
Hydrogen 0.99 % H 8.83 % H2O
Oxygen 54.90 % O
  100.00 % 100.00 % = TOTAL OXIDE

 

Crystallography: Monoclinic – Sphenoidal
Crystal Habit: Flat crystals, to 17 cm, occur along bedding planes. Commonly as spherulitic aggregates of radiating acicular to prismatic crystals; as massive granular aggregates.
Twinning: None

 

Cleavage: Perfect on {100}; imperfect on {102}, {010}
Fracture: Fibrous
Tenacity: Brittle, Fibrous
Moh’s Hardness: 1.0 – 2.0
Density: 2.44 – 2.46 (g/cm3)
Luminescence: Fluorescent; SW UV = blue green or green, LW UV = orange
Radioactivity: Not Radioactive
Other: Piezoelectric

 

Color: Colorless, White, light Brown
Transparency: Translucent to Transparent
Luster: Vitreous, slightly pearly on cleavage surfaces
Refractive Index: 1.515 – 1.535  Biaxial ( – )
Birefringence: 0.0110 – 0.0200
Dispersion: None
Pleochroism: None