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Formulae:
There are three piemontite minerals:
piemontite: Ca2(Al2Mn3+)[Si2O7]{SiO4]O(OH)
Piemontite-(Pb): CaPb(Al2Mn3+)[Si2O7]{SiO4]O(OH)
Piemontite-(Sr): CaSr(Al2Mn3+)[Si2O7]{SiO4]O(OH)
This page refers to piemontite.
Sorosilicate (Si2O7 groups), manganese-bearing
mineral,
epidote group
Crystal System: Monoclinic
Specific gravity: 3.46 to 3.54 measured, 3.45 calculated
Hardness: 6 to 6½
Streak: Reddish
Colour: Red, red-violet, red-brown to reddish black
Common impurities: Fe,Ti,Na,K,H2O
Environments:
Metamorphic environments
Hydrothermal environments
Piemontite is the manganese analogue of
clinozoisite, with Mn3+ substituting for Al. Piemontite
is not found in many manganese-rich deposits where it might be expected. This
is because piemontite can form only where there is sufficient manganese
and the conditions are sufficiently oxidising to create Mn3+
(R&M 86.5.449-455).
Piemontite occurs in regionally metamorphosed rocks of the
greenschist to
amphibolite facies, in metasomatized
manganese deposits and in low-temperature hydrothermal veins in altered
rhyolite, andesite and
diorite. Associated minerals include
epidote, tremolite,
glaucophane, orthoclase,
quartz and calcite
(HOM).
Localities
At the type locality, the Prabornaz Mine, Saint-Marcel, Aosta Valley, Italy, piemontite forms dark red, bladed
crystals and masses in the upper zone of a metamorphic manganese ore deposit
(R&M 86.5.449-455).
At the Cassagna Mine, Ne, Genoa, Liguria, Italy, piemontite is found as well formed crystals to 3 mm in size with
pyrolusite and quartz
(R&M 86.5.449-455).
In Japan, piemontite schist is found in the Sonoki and Sangun
metamorphic zones
(R&M 86.5.449-455).
At the Tone mine, Kinkai-Tone-machi, Nagasaki City, Nagasaki Prefecture, Japan, piemontite occurs as crystals
associated with braunite
(R&M 86.5.449-455).
At the Otakiyama manganese deposit, Bizan, Tokushima City, Tokushima prefecture, Shikoku Island, Japan, piemontite
is found as 3-cm acicular crystals
(R&M 86.5.449-455).
At the Messina Mine, Musina, Musina Local Municipality, Vhembe District Municipality, Limpopo, South Africa, translucent
to transparent crystals of piemontite to 6 mm in size are found with colourless
quartz
(R&M 86.5.449-455).
At Shadow Lake, Minarets District, Ritter Range, Madera county, California, USA, specimens containing well crystallised
piemontite were taken from a shear zone in schistose volcanic rocks
about three hundred yards east of the outlet of Shadow Lake. The usual mineral association is piemontite,
tremolite and vein quartz, which were
deposited in that order. In addition some cavities in the rock are lined with small, orange-coloured crystals of a
manganese-bearing garnet. In thin
section tremolite, itself enclosed in later
quartz, can be seen replacing piemontite
(AM 18.493-500).
At the Pilar Cliffs, Taos county, New Mexico, USA, rough, dark red crystals of piemontite have been found
(R&M 86.5.449-455).
At Culp Ridge, Glatfelter Farm, Hamiltonban Township, Adams county, Pennsylvania, USA, piemontite has been found
as dense veins of radiating acicular crystals
(R&M 86.5.449-455).
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