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Formula: Mn4+O2
Simple oxide, rutile group,
manganese-bearing mineral
Polianite is a name for pyrolusite pseudomorphs after
pseudoorthorombic manganite crystals (actually
manganite has monoclinic structure)
(Mindat).
Crystal System: Tetragonal
Specific gravity: 5.04 to 5.08 measured, 5.189 calculated
Hardness: 6
Streak: Black
Colour: Silver-grey to flat black
Solubility: Moderately soluble in hydrochloric acid; insoluble in nitric acid
Environments:
Sedimentary environments (commonest)
Hydrothermal environments
Pyrolusite is one of the commonest manganese minerals, formed under oxidising conditions and high pH
(highly alkaline),
(Dana)
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
minerals.
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).
Alteration
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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