Kentbrooksite

Kentbrooksite can be a mineral that is extremely uncommon is a manganese and fluorine rich member associated with the Eudialyte team of minerals with the formula (Na, REE)15(Ca, REE)6Mn3Zr3NbSi25O74F2·2H2O and crystal habit are Anhedral to subhedral aggregates to 2cm. The characteristic options of kentbrooksite, that create it totally different from eudialyte are (1) dominancy of F (2) dominancy of Mn, and (3) dominancy of Nb. It really is primarily available at Mt Saint-Hilaire, Quebec, Canada; Kangerlugssuaq Firth, Greenland; Telemark, Norway; Kola Peninsula, Russia; and Tien Shan Mts, Tajikistan. Gem quality crystals are excessively small and rare. Kentbrooksite contains Rare that is several worlds (REE) such as Lanthanum (La), Cerium (Ce), Praeseodymium (Pr), Neodymium (Nd) and Samarium (Sm) and for that reason is weakly radioactive as defined in 49 CFR 173.403 (greater than 70 Bq/gram).

Category: Silicate mineral, Cyclosilicate
Chemical Formula: (Na,REE)15(Ca,REE)6Mn3Zr3NbSi25O74F2·2H2O
Crystallography: Trigonal – Ditrigonal Pyramidal
Crystal Habit: Anhedral to subhedral aggregates to 2cm
Twinning: None

 

Cleavage: None
Fracture: Uneven
Tenacity: Brittle
Hardness (Mohs): 5.0 – 6.0
Density: 3.07 – 3.10 (g/cm3)
Luminescence: None
Radioactivity: Weak; GRapi = 29,710.44

 

Color: Yellowish Brown
Transparency: Transparent, Translucent
Luster: Vitreous
Refractive Index: 1.623 – 1.628  Uniaxial ( – )
Birefringence: 0.005
Dispersion: Weak
Pleochroism: None