Hemimorphite
| Hemimorphite | |
|---|---|
|
Hemimorphite from Mapimi, Durango, Mexico | |
| General | |
| Category | Sorosilicates |
| Formula (repeating unit) | Zn4Si2O7(OH)2·H2O |
| Strunz classification | 09.BD.10 |
| Crystal symmetry | Orthorhombic mm2 |
| Unit cell | a = 8.367(5) Å, b = 10.73Å, c = 5.155(3) Å; Z = 2 |
| Identification | |
| Color | White, blue, greenish |
| Crystal habit | Polar crystals, with different or hemimorphic ends. Also coxcomb masses, mammillary, stalactitic, or massive |
| Crystal system | Orthorhombic pyramidal |
| Twinning | Rare on {001} |
| Cleavage | Perfect on {110}, poor on {101}, {001} rare |
| Fracture | Uneven to conchoidal |
| Tenacity | Brittle |
| Mohs scale hardness | 4.5-5 |
| Luster | Vitreous, adamantine, rarely silky |
| Streak | White |
| Diaphaneity | Transparent to translucent |
| Specific gravity | 3.516 - 3.525 |
| Optical properties | Biaxial (+) |
| Refractive index | nα = 1.614 nβ = 1.617 nγ = 1.636 |
| Birefringence | δ = 0.022 |
| 2V angle | Measured: 46°, calculated: 44° |
| Solubility | Soluble in acid |
| References | [1][2][3] |
Hemimorphite, is Zn4(Si2O7)(OH)2·H2O, a component of calamine. It is a sorosilicate mineral which has been historically mined from the upper parts of zinc and lead ores, chiefly associated with smithsonite, ZnCO3. They were assumed to be the same mineral and both were classed under the same name of calamine. In the second half of the 18th century it was discovered that these two different minerals were both present in calamine. They closely resemble each other.
The silicate was the rarer of the two, and was named hemimorphite, because of the hemimorph development of its crystals. This unusual form, which is typical of only a few minerals, means that the crystals are terminated by dissimilar faces. Hemimorphite most commonly forms crystalline crusts and layers, also massive, granular, rounded and reniform aggregates, concentrically striated, or finely needle-shaped, fibrous or stalactitic, and rarely fan-shaped clusters of crystals.
Some specimens show strong green fluorescence in shortwave ultraviolet light (253.7 nm) and weak light pink fluorescence in longwave UV.
Occurrence
Hemimorphite most frequently occurs as the product of the oxidation of the upper parts of sphalerite bearing ore bodies, accompanied by other secondary minerals which form the so-called iron cap or gossan. Hemimorphite is an important ore of zinc and contains up to 54.2% of the metal, together with silicon, oxygen and hydrogen. The crystals are blunt at one end and sharp at the other.
The regions on the Belgian-German border are well known for their deposits of hemimorphite of metasomatic origin, especially Vieille Montagne in Belgium and Aachen in Germany. Other deposits are near Tarnovice in upper Silesia, Poland; near Phoenixville, Pennsylvania; the Missouri lead-zinc district; Elkhorn, Montana; Leadville, Colorado; and Organ Mountains, New Mexico in the United States; and in several localities in North Africa. Further hemimorphite occurrences are the Padaeng deposit near Mae Sod in western Thailand; Sardinia; Nerchinsk, Siberia; Cave del Predil, Italy; Bleiberg, Carinthia, Austria; Matlock, Derbyshire, England.
References
- Hurlbut, Cornelius S.; Klein, Cornelis, 1985, Manual of Mineralogy, 20th ed., ISBN 0-471-80580-7
- Boni, M., Gilg, H.A., Aversa, G., and Balassone, G., 2003, The "Calamine" of southwest Sardinia: Geology, mineralogy, and stable isotope geochemistry of supergene Zn mineralization: Economic Geology, v. 98, p. 731-748.
- Reynolds, N.A., Chisnall, T.W., Kaewsang, K., Keesaneyabutr, C., and Taksavasu, T., 2003, The Padaeng supergene nonsulfide zinc deposit, Mae Sod, Thailand: Economic Geology, v. 98, p. 773-785.
- Mineral galleries
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