This specimen showcases a cluster of well-formed, white botryoids of franconite within a tight gap of a vug packed with grey weloganite. This is the type locality for both species. Collected by Dr. Tarassoff in 1970, franconite was officially recognized as a new mineral species in 1984. It occurs as white globules on weloganite crystals, and less commonly on calcite or quartz, in vugs within a dawsonite-bearing sill in the Francon limestone quarry. These globules consist of radiating bladed crystals with a vitreous lustre and white streak, collectively imparting a silky lustre to newly split surfaces. An elusive species!
Ref: The Canadian Mineralogist (1984) 22 (2): 239–243.
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