| Mammothite | |
| Category: | Sulfates |
| Formula: | Pb6Cu4AlSb5+O2(OH)16Cl4(SO4)2 |
| Imasymbol: | Mm[1] |
| Strunz: | 8th Edition, 6/B.10-50 |
| System: | Monoclinic |
| Class: | 2-Sphenoidal |
| Symmetry: | C2 |
| Unit Cell: | a = 18.93(3) Å, b = 7.33(1) Å c = 11.35(2) Å; β=112.44(10)°, Z = 2 |
| Color: | Cerulean blue, blue-green, pale blue |
| Habit: | Tabular to prismatic and acicular crystals, radial aggregates |
| Cleavage: | Distinct on, Good |
| Fracture: | Irregular, Uneven |
| Tenacity: | Brittle |
| Mohs: | 3 |
| Luster: | Sub-Vitreous, Resinous |
| Refractive: | nα= 1.868 nβ= 1.892 nγ= 1.928 |
| Opticalprop: | biaxial positive |
| Birefringence: | δ=0.060 |
| Dispersion: | r > v |
| Pleochroism: | Visible |
| Streak: | Pale blue |
| Density: | 5.25 g/cm3 |
| Diaphaneity: | Transparent |
| References: | [2] [3] [4] [5] |
Mammothite is a mineral found in the Mammoth mine in Tiger, Arizona and also in Laurium, Attika, Greece. This mineral was named in 1985 by Donald R. Peacor, Pete J. Dunn, G. Schnorrer-Köhler, and Richard A. Bideaux, for the Mammoth vein (one of the two main veins in the mine) and the town of Mammoth, Arizona, which was named for the mine. The mammothite that is found in Arizona exist as euhedral crystals imbedded in micro granular, white colored anglesite with a saccharoidal texture. The associated minerals include phosgenite, wulfenite, leadhillite and caledonite. In Greece, the mammothite exists as small euhedral crystals and also as microscopic rock cavities lined with projecting crystals within the slags. The associated minerals here are cerussite, phosgenite and matlockite. The ideal chemical formula for mammothite is Pb6Cu4AlSb5+O2(OH)16Cl4(SO4)2.
Mammothite is associated with various minerals but different minerals at different locations. In the Mammoth mine in Tiger, Arizona this mineral is associated with phosgenite, wulfenite, leadhillite and caledonite. There are roughly 100 different kinds of mineral species in the Mammoth mine and about 25 of these are considered to be a part of an anomalous oxidized sequence. These minerals will grow in close quarters with each other but other minerals containing Pb, Cu, Fe, and Zn are also present. The minerals contained in this abnormal sequence contain Pb, Cu, SO4, and CO3 and they may occur in the same minerals. The element Antimony is a very rare element that is exhibited in mammothite but also in the mineral tetrahedrite, which is seen having small crystals that are attached to pyrite crystals. In Laurium, Attika, Greece, the mammothite exists as small euhedral crystals and also as microscopic rock cavities lined with projecting crystals within the slags. The associated minerals here are cerussite, phosgenite and matlockite.
Mammothite is a cerulean blue to pale blue, transparent mineral with a resinous or subvitreous luster. It exhibits a hardness of 3 on the Mohs hardness scale. Mammothite occur as tabular to acicular crystals that exhibit radial aggregates. In Arizona, mammothite is mostly tabular but several samples are elongated on the [001] axis. In Tiger, Arizona, crystals are less than 1.0 mm in size. The density was difficult to be measured due to the small size and an abundance of other minerals attached to it. By using heavy liquid techniques, it was determined to be greater than 4.2g/cm3 but the idealized end member was calculated to be 5.25g/cm3. In Laurium, Greece, this mineral is different in appearance. The color of the samples may range from pale blue to white. The crystals in Greece are very small and can exhibit two habits. These habits include being prismatic and bladed; or being very prismatic and elongated on the [001] axis. Mammothite is brittle and shows distinct cleavage along the plane. The measured density is 5.25 g/cm3.
Mammothite is biaxial positive, which means it will refract light along two axes. It exhibits a 2V(measured)=80°, strong dispersion with r>v, and displays visible pleochroism with varying colors of shades of pale blue. The indices of refraction are α=1.868, β=1.892, γ=1.928. Mammothite is also transparent and does not respond to ultraviolet radiation.
The chemical formula for mammothite is Pb6Cu4AlSb5+O2(OH)16Cl4(SO4)2. Mammothite is one of the few minerals that has an Sb atom in the pentavalent state.
| Oxide | wt% | |
|---|---|---|
| Al2O3 | 2.3 | |
| CuO | 14.9 | |
| PbO | 57.6 | |
| Sb2O3 | 8.48 | |
| SO3 | 7.7 | |
| Cl | 5.7 | |
| H2O | 7.0 | |
| O=Cl | 1.3 | |
| Total | 100.00 |
Mammothite is in the monoclinic crystal system, with space group C2. The unit cell dimensions are a=18.93(3) Å, b=7.33(1) Å, c=11.35(2) Å, β=112.44(10)°. These values were obtained through powder diffraction that was found by using a 114.6 mm diameter Gandolfi camera, CuKα X-radiation, polycrystalline sample and a silicon sample as an internal standard.