Wattersite | |
Category: | Chromate mineral |
Formula: | Hg+14Hg+2Cr+6O6 |
Imasymbol: | Wte[1] |
Strunz: | 7.FB.15 |
Dana: | 35.4.2.1 |
System: | Monoclinic |
Class: | 2/m |
Symmetry: | C2/c (number 15) |
Unit Cell: | 859.81 ų |
Color: | Dark red-brown to black |
Habit: | Prismatic, aggregates, massive |
Twinning: | [001], contact twins on |
Cleavage: | None |
Fracture: | Conchoidal |
Tenacity: | Brittle |
Mohs: | 4.5 |
Luster: | Sub-Metallic |
Streak: | Brick red |
Diaphaneity: | Opaque |
Gravity: | 8.91 |
Opticalprop: | Biaxial |
Refractive: | nα = 2.440 - 2.520 nγ = 2.700 - 2.860 |
Birefringence: | δ = 0.260 - 0.340 |
Pleochroism: | Visible |
Dispersion: | r > v strong |
References: | [2] |
Wattersite is a rare mercury chromate mineral with the formula Hg+14Hg+2Cr+6O6.[3] It occurs in association with native mercury and cinnabar in a hydrothermally altered serpentinite.[4] It was first described from Clear Creek claim, San Benito County, California, USA in 1961.[5] It was named to honor Californian mineral collector Lucius "Lu" Watters.[4]