Santaclaraite

santaclaraite

howieite

rhodochrosite

kutnohorite

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Formula: CaMn2+4Si5O14(OH)2.H2O
Inosilicate (chain silicate), manganese-bearing mineral
Crystal System: Triclinic
Specific gravity: 3.31 measured, 3.379 calculated
Hardness: 6½
Streak: Very pale pink
Colour: Pink to reddish orange, brown
Solubility: Insoluble or only very slightly soluble in hot concentrated acids
Common impurities: Al,Fe,Ni,Co,Mg,Na
Environments

Chert

Santaclaraite dehydrates to bustamite at about 550oC in air (AM 69.200-206).

Localities

The type locality, the Pennsylvania mine, Sugarloaf Mountain, Black Wonder Mining District, Santa Clara county, California, USA, is one of about fifty abandoned manganese mines located in Santa Clara that occur in chert. The paragenesis of the specimens is noteworthy in that the more common manganese minerals are scarce or absent and the manganese silicates so far found are all unusual in some respects. Santaclaraite occurs both as cross-fibre veins (the largest measures 1 cm in width by more than 9 cm in length) and irregular masses (10 cm in maximum dimension) in manganese oxide stained chert and quartz. Santaclaraite is the most abundant manganese silicate at this locality. Manganese-rich howieite is associated with santaclaraite as yellow-brown fibrous veinlets, masses and small spherules. Fine-grained rhodochrosite is subordinate to the manganese silicates but is widely disseminated throughout them and the quartz matrix. Kutnohorite and calcium-bearing rhodochrosite were found in a single occurrence as small scalenohedra to 0.6 mm.
The manganese mineral that was mined at this locality appears to have been braunite, which occurs as masses and veins, up to 6 cm across. Other associated minerals are calcite (some manganoan), baryte, rare harmotome, chalcopyrite and native copper. Some of the quartz is coloured dark greyish blue by inclusions of asbestiform riebeckite (AM 69.200-206).

At the Buckeye mine, Mount Oso, Ladd-Buckeye Mining District, Stanislaus county, California, USA, santaclaraite occurs sparsely as pink prismatic crystals up to 3 mm long in quartz veins in tan chert, associated with rhodochrosite, a friedelite-like mineral, braunite, and very minor chalcopyrite (AM 69.200-206).

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