Utahite | |
Category: | Tellurate minerals |
Formula: | Cu5Zn3(Te6+O4)4(OH)8·7H2O |
Imasymbol: | Uta[1] |
Molweight: | 1,542.46 g/mol |
Strunz: | 7.DE.25 |
System: | Triclinic Unknown space group |
Unit Cell: | a = 8.794 Å, b = 9.996 Å c = 5.66 Å; α = 104.1° β = 90.066°, γ = 96.3333°; Z = 1 |
Color: | Pale blue, greenish blue |
Habit: | Prismatic thin tabular to bladed crystals; as sheaves and bow tielike clusters |
Cleavage: | none |
Fracture: | Brittle – uneven |
Mohs: | 4–5 |
Luster: | Vitreous to pearly |
Streak: | Pale blue |
Diaphaneity: | Translucent |
Gravity: | 5.33 |
Opticalprop: | Biaxial |
Refractive: | nα = 1.830 – 1.840 nβ = 1.830 – 1.900 nγ = 1.880 – 1.900 |
Birefringence: | δ = 0.050 – 0.060 |
Dispersion: | Strong |
References: | [2] [3] [4] |
Utahite is an extremely rare secondary copper zinc tellurate mineral found as a product of oxidation. Its chemical formula is Cu5Zn3(Te6+O4)4(OH)8·7H2O.
It was first described in 1997 for an occurrence in the Centennial Eureka mine, one mile southeast of Eureka, Tintic District, Juab County, Utah, US (type locality). The discovery site was a mine dump of a hydrothermal ore deposit where it occurs with cesbronite and quartz.[4] It has also been reported from the Empire Mine in the Tombstone District of Cochise County, Arizona.[3]