• Source: Hanksite

Hanksite is a sulfate mineral, distinguished as one of only a handful that contain both carbonate and sulfate ions (a sulfate carbonate). It has the chemical formula Na22K(SO4)9(CO3)2Cl.




Occurrence


It was first described in 1888 for an occurrence in Searles Lake, California, and named for American geologist Henry Garber Hanks. Hanksite is normally found in crystal form as evaporite deposits. Hanksite crystals are large but not complex in structure. It is often found in Searles Lake, Soda Lake, Mono Lake, and in Death Valley. At its deposits in San Bernardino County, California hanksite is commonly found beneath the surface embedded in mud or in drill cores (Palache et al., 1960). It is associated with halite, borax, trona, and aphthitalite at the Searles Lake locality. It is also associated with borax mining in the Soda Lake area.




Physical characteristics


Hanksite can be colorless, white, gray, green, or yellow, and is transparent or translucent. The mineral's hardness is approximately 3 to 3.5. The specific gravity is approximately 2.5 (slightly below average). It is salty to the taste and sometimes glows pale yellow in ultraviolet light. Typical growth habits are hexagonal prisms or tabular with pyramidal terminations. The streak of Hanksite is white. It can contain inclusions of clay that the crystal formed around while developing.




Similar minerals



Borax
Halite
Nahcolite
Tincalconite
Trona




References






Bibliography


Palache, P.; Berman H.; Frondel, C. (1960). "Dana's System of Mineralogy, Volume II: Halides, Nitrates, Borates, Carbonates, Sulfates, Phosphates, Arsenates, Tungstates, Molybdates, Etc. (Seventh Edition)" John Wiley and Sons, Inc., New York, pp. 628-629.

Kata Kunci Pencarian:

• Segi enam
• Hanksite
• Hexagon
• Evaporite
• List of gemstones by species
• Sulfate mineral
• Mineralogy
• List of minerals
• Searles Lake
• Crystal habit
• Crystal system