Simple oxide, rutile group, manganese mineral
Specific gravity: 4.9 to 5.1
Colour: Silver-grey to flat black
Solubility: Moderately soluble in hydrochloric acid; insoluble in nitric acid
Sedimentary environments (commonest)
Pyrolusite is one of the commonest manganese minerals, formed under oxidising conditions and high pH
as an alteration product of manganese minerals such as rhodochrosite,
and also as a chemical precipitate in lakes.
Nodular deposits of pyrolusite are found in bogs, on
lake bottoms, and on the floors of seas and oceans. Beds of manganese ores are found enclosed in residual
clay, derived from the decay of manganiferous
limestone. Pyrolusite is also found in the oxidation zone of
epithermal (low temperature) hydrothermal veins with
quartz and various metallic
At Burdell Gill, Coombe Height, Caldbeck, Allerdale, Cumbria, England, UK, pyrolusite is a supergene mineral associated with romanèchite in a goethite, cryptomelane and pyrolusite impregnated quartz vein. It may contain quartz inclusions, and is often covered by crusts of cryptomelane. There are possibly pseudomorphs of pyrolusite after manganite. (JRS 8(1).1-9).
At the Clargillhead vein, Garrigill, Alston Moor, Eden, Cumbria, England, UK, pyrolusite occurs as rare fibrous aggregates up to 60 microns in diameter in the quartz-fluorite gangue (JRS 23.51).
At Croft Quarry, Croft, Blaby, Leicestershire, England, UK, pyrolusite is associated with palygorskite and dolomite (JRS 20.24).
At the Peldar Tor quarry, Spring Hill, Whitwick, Leicestershire, England, UK, pyrolusite occurs on quartz (RES p201).
In the Mendip Hills, Somerset, England, UK, pyrolusite occurs in mineralised cavities in manganese pods and veins. (JRS 13.15).
In the geodes at Las Choyas, Chihuahua, Mexico, pyrolusite formed on the surface of a chalcedony variety agate band, and was then covered by more chalcedony. (R&M 85.2.112).
In the Tombstone Mining District, Arizona, USA pyrolusite occurs as inclusions in calcite, and associated with quartz, bromian chlorargyrite, chlorargyrite and cerussite. Where cerussite and pyromorphite dominate, there is a strong goethite-muscovite variety illite-pyrolusite alteration. (R&M 90.4.345).
At the Manganese Mine, Keweenaw County, Michigan, USA, pyrolusite occurs in calcite vugs pyrolusite replaces braunite and macfallite. The paragenetic sequence is calcite, orientite, macfallite, braunite and manganite. Pyrolusite is a late-stage mineral, but there is much overlapping. (R&M 89.6.510).
At the Apex Mine, Lander County, Nevada, USA, pyrolusite forms a substrate for autunite on monzonite (R&M 87.3.270-276).
pyrolusite and quartz to braunite and O2
7Mn4+O2 + SiO2 ⇌ Mn2+Mn3+6O8(SiO4) + 2O2
Increasing temperature favours the forward reaction (AM80.571).
rhodochrosite and O2 to pyrolusite and CO2
2MnCO3 + O2 ⇌ 2Mn4+O2 + 2CO2
Increasing temperature favours the reverse reaction (AM80.571).
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