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Witherite is a mineral, 3, in the group. Witherite crystallizes in the system and virtually always is . The mineral is colorless, milky-white, grey, pale-yellow, green, to pale-brown. The is 4.3, which is high for a translucent mineral. It light blue under both long- and short-wave light, and is under short-wave UV light.

Witherite forms in low-temperature environments. It is commonly associated with , celestine, , , , and . Witherite occurrences include: Cave-in-Rock, Illinois, US; Pigeon Roost Mine, Glenwood, Arkansas, US; Settlingstones Mine ; , ; , and ,Ashburn, J.H., Mining Witherite in North-West Durham, Colliery Guardian, August 1963 (at Durham Mining Museum web-site) , ; area, , , , and (Tarnowskie Góry and Tajno at Suwałki Region).

Witherite was named after William Withering (1741–1799) an physician and naturalist who in 1784 published his research on the new mineral. He could show that barite and the new mineral were two different minerals.


Discovery
In 1789 the German geologist Abraham Gottlob Werner named the mineral witherite in honour of William Withering. The mineral collection of Birmingham Museum and Art Gallery may contain one of the earliest known specimens of witherite. A label in Boulton's handwriting, records: "No.2 Terra Ponderosa Aerata, given me by Dr. Withering".


Risk to human health
The 18th-century naturalist Dr. Leigh recorded its effects after the death of a farmer's wife and child. James Watt Jnr. experimented with the mineral on animals and he recorded the same lethal properties. Until the 18th century farmers at used the mineral as rat poison.The Mining Magazine, March 1963, Vol 108, pages 133–139


Industrial use
An experiment conducted by , led to it being used in his ''; the mineral had previously been considered as worthless. Witherite has been used for hardening steel, and for making cement, glass, enamelware, soap, dye and explosives.'Looking Back' p10 Hexham Courant 10 January 2014 featuring a photograph of Settlingstones miners in 1905

Witherite crystallizes in the system. The are invariably twinned together in groups of three, giving rise to pseudo-hexagonal forms somewhat resembling bipyramidal crystals of , the faces are usually rough and striated horizontally. It transforms into an hexagonal phase at 1084 K that changes into a cubic phase at 1254 K. The mineral is named after William Withering, who in 1784 recognized it to be chemically distinct from . It occurs in veins of at in , Alston in , , near in and a few other localities. Witherite is readily altered to barium by the action of water containing in solution and crystals are therefore frequently encrusted with . It is the chief source of barium salts and is mined in considerable amounts in Northumberland. It is used for the preparation of rat poison, in the manufacture of and , and formerly for refining . It is also used for controlling the chromate to ratio in baths.

Witherite-216507.jpg|Two sharp pseudohexagonal crystals of witherite on calcite from Hardin County, Illinois (size: 6.4 × 5.4 × 3.4 cm) Witherite-65711.jpg|Witherite crystal from the Cave-in-Rock Sub-District, Illinois – Kentucky Fluorspar District, Hardin County, Illinois


See also
  • List of minerals
  • List of minerals named after people


External links
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