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Formula: Na2(Si7Al2)O18.6H2O
Tectosilicate (framework silicate), stilbite subgroup,
zeolite group
Crystal System: Orthorhombic
Specific gravity: 2.3 measured, 2.08 calculated
Hardness: 3 to 4
Streak: White
Colour: White, pink
Common impurities: Ca,K,Fe,Mn,Mg,Sr,Ba
Environments
Localities
At the type locality, the Sant' Efisio Tower, Capo di Pula, Pula, Metropolitan City of Cagliari, Sardinia, Italy,
barrerite occurs as well-formed, laminar crystals to 5 mm, on the walls of large fractures in deeply
weathered andesitic and
rhyolitic lavas, associated with
heulandite
(HOM).
At Hound Island, Petersburg Borough, Alaska, USA, barrerite is very rare in the calcium-rich
Triassic (252-201 million years ago) breccias
(CM 35.691-698).
At Kuiu Island, Petersburg Borough, Alaska, USA, barrerite crystals up to several centimeters in length,
accompanied by microcrystalline quartz in characteristic stalactite-like
dendritic aggregates, line vugs as wide as several decimeters. Barrerite crystals and
quartz aggregates overgrow one another, probably as the result of several
sequences of altemating crystallisation
(CM 35.691-698).
Rocky Pass, Petersburg Borough, Alaska, USA, is a narrow and shallow area separating the islands of Kuiu and
Kupreano. It features pillow basalt having the characteristic texture
of lavas solidified under water or ice.
Zeolite-containing vugs have been exposed in the tidal area.
Barrerite is restricted to this tidal area, and is probably formed by crystallisation in the presence of
seawater
(CM 35.691-698).
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