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Updated: July 29, 2026
M. Boussingault, in a memoir which he has recently addressed to me, calls the rock of the Morros a problematic calcariferous gneiss. This expression seems to prove that the plates of mica take in some parts a uniform direction, as in the greenish dolomite of Val Toccia. This cement, where it abounds, has a conchoidal fracture and passes to jasper.
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