Römerite

romerite

copiapite

melanterite

voltaite

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Formula: Fe2+Fe3+2(SO4)4.14H2O
Hydrated normal sulphate
Specific gravity: 2.174
Hardness: 3 to 3½
Streak: White
Colour: Brown, yellow, violet-brown; yellow-brown in transmitted light
Solubility: Soluble in cold water
Environments

Hydrothermal environments
Volcanic sublimate uncommon

Römerite occurs as an early alteration product of oxidising pyrite or pyrrhotite, and uncommonly as a volcanic sublimate. Associated minerals include copiapite, melanterite, voltaite, halotrichite, szomolnokite, kornelite, rozenite, siderotil and alunite (HOM).

Localities

At the Sunny Corner Mine, Sunny Corner, Roxburgh county, New South Wales, Australia, römerite occurs with other sulphate minerals that can be formed only under very acidc conditions. It occurs in an overhang in blue-green coloured material that is a mixture of chalcanthite, melanterite, siderotil and römerite. Close by there is a paler material that is a mixture of major alunogen and minor jurbanite and felsobanyaite. Other minerals present in the vicinity include hydroniumjarosite, copiapite, ferricopiapite, cuprocopiapite and zincocopiapite (AJM 17.1.45-51).

At the Siglo Veinte Mine, Llallagua, Rafael Bustillo Province, Potosí, Bolivia, römerite has been reported as crusts of rust-brown crystals in old workings, associated with chalcanthite, melanterite and pickeringite (Minrec 37.2.151).

At the Zagh Mine, Haji Abad, Bandar Abbas, Bandar Abbas County, Hormozgan Province, Iran, römerite has been found associated with with voltaite (Dana).

At the type locality, the Rammelsberg mine, Rammelsberg, Goslar, Goslar District, Lower Saxony, Germany, römerite has been found associated with copiapite (Dana).

At the United Verde mine, Jerome, Verde Mining District, Black Hills, Yavapai county, Arizona, USA, römerite is amongst the minerals resulting from a fire that burnt in the mine for many years. The first fire started in 1894, probably due to spontaneous combustion. Subsequent stripping operations with steam shovels exposed the still hot rocks impregnated with these minerals.
The relatively rare römerite occurs as a thin crust, a few millimeters in thickness, coating massive, granular pyrite and associated with small, yellow flakes of copiapite; the römerite, however, was formed later than the copiapite. The römerite is pale chestnut brown in the thicker crusts, and colourless in thin slivers (AM 13.203-229 as louderbackite).

At the Island Mountain mine, Moose Peak, Island Mountain, Coastal Range, Trinity county, California, USA, römerite occurs as one of the interesting sulphates developed by the alteration of pyrrhotite. It is cinnamon-brown or chestnut-brown in colour, and occurs in stocky to tabular crystals up to 5 mm in length, and 2 or 3 mm in width and thickness. It is commonly associated with a yellowish earthy oxide like coquimbite (AM 12.279-282).

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