Garronite is a series with end members:
Garronite-Ca:
Ca3(Al6Si10O32).14H2O
Garronite-Na:
Na6(Al6Si10O32).8.5H2O
These minerals are tectosilicates (framework silicates),
zeolite group.
Garronite-Na was approved as a new mineral in 2015. Previously "garronite"
had been the species name of the mineral now renamed "Garronite-Ca".
Specific gravity: 2.13 to 2.18
Hardness: 4½ to 5
Streak: White
Colour: Colourless, white
Common impurities: Ca: Fe,Ba,K
Environments:
Garronite is most common in vesicles in basalt and other
mafic rocks, often overgrown by or associated with
phillipsite, and also as epitaxial overgrowths on
phillipsite
(Dana).
Localities
In Iceland garronite occurs at numerous localities in lavas rich in phenocrysts of anorthite variety
bytownite and in non-porphyritic
olivine basalt flows
(HOM).
In Russia, near Nevon, on the Angara River, 50km below the Ilim River, Siberia, garronite occurs in
dolerite porphyry
(HOM).
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