Mosesite is a very raremineral found in few locations. It is a mercury mineral found as an accessory in deposits of mercury, often in conjunction with limestone. It is known to be found in the U.S. states of Texas and Nevada, and the Mexican states of Guerrero and Querétaro. It was named after Professor Alfred J. Moses for his contributions to the field of mineralogy in discovering several minerals found alongside mosesite. The mineral itself is various shades of yellow and a high occurrence of spinel twinning. It becomes isotropic when heated to.
Composition
Mosesite contains 16 Hg, 3 Cl, 1½ SO4, ½ CO3, ½ MoO4, 16 H, and 8 N with a volume of 8.4777x10−1 nm³ and calculated density of 7.53 g/cm³. The accepted formula for mosesite is Hg2N•H20.
Geologic occurrence
Discovered in a mercury mine in Terlingua, Texas, mosesite has also been seen in Nevada and Mexico. Mosesite is a secondary mineral formed at low temperature in hydrothermal mercury deposits. The mercury ore at the mine in Huahuaxtla is aligned with ribs of brecciated limestone that formed along shallow angle fault plane. In the Huahuaxtla mine, this is due to the evidence of oxidized minerals. The portion of the mine in which the mosesite was found is thought to be a solution cavity in a zone of fractured limestone. Mosesite is never found in abundance in any of the known locations of its origin. Mineral associations include montroydite, calcite, gypsum, and at some localities native mercury.
Structure
twinning is a common occurrence in mosesite. Mosesite was found to have a unit cell with diamond typespace lattice and the measured unit cube of Mosesite was approximately 9.44 nmx10−1 with additional forms,,,, and. In Mexico, the mosesite was most usually found as octahedral crystals which were usually intergrown. Single crystals are rare. Mosesite has a similar structure to Millon’s base. Mosesite consists of a three-dimensional framework of Hg2N+ groups. The mercury atoms form linear sp bonds, while the nitrogen forms tetrahedral sp3 bonds, in a face-centered cubic lattice. The space group of mosesite is F*43m.
Physical properties
Mosesite is a minute yellow crystal with imperfect cleavage along and uneven fracture. It is brittle with a hardness of 3.5. Long exposure, a month or more, to light will change Mosesite to a light olive green color. The powdered form retains its color streaking a light yellow. The mineral exhibits no pleochroism and displays uneven birefringence in polarized light. Heat has a notable effect on Mosesite for when heated above the mineral becomes isotropic. This corresponds optically with the observed crystal form only at this higher temperature. It is considered weakly anisotropic. The index of refraction is n = 2.065±0.01. It has an adamantine luster officially ranges in color from lemon yellow to canary yellow. Mosesite reacts chemically with HCl leaving a residue of HgCl.
