Resource World Magazine

Resource World - June-July 2018 - Vol 16 Issue 4

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J U N E / J U L Y 2 0 1 8 www.resourceworld.com 49 MINING gem variety of the mineral cordierite. To further enhance the gemstone potential of the area, pegmatite dykes intrude the Passmore metamorphic complex and contain small blue aquamarine crystals, gorgeous deep red garnets, and smoky quartz. Pegmatites are particularly pro - spective for many gemstones because the coarse-grained igneous rock may contain small cavities that enable late-stage gem crystal growth. Star sapphires and other gems are also found in alluvial gravels in the Slocan River valley area. Further south, between Salmo and Creston, light blue to sky blue aquamarine crystals are found within later-stage quartz veins and pegmatites along the Shaw Creek Stock. Aquamarine is also found in peg - matites northwest of Cranbrook along the western margin of the White Creek batho- lith. Other places where aquamarines are found include McDame, Prince George and near Atlin, northern BC. Sherry-brown topaz crystals are commonly associated with aquamarine. What about emeralds in BC? Emeralds and aquamarine are both varieties of the mineral beryl. Beryl is an ore mineral for beryllium, which is used in the aerospace industry. The splendid verdant color of the emerald variety of beryl is caused by trace amounts of chromium and/or vanadium in the beryl crystal structure. Beryllium and chromium atoms are prac - tically incompatible in nature and only under extreme geological conditions can they combine to form an emerald crystal. Geologists have postulated where emer - alds may occur in BC. A single occurrence of deep green beryl is reported at Red Mountain near Stewart. There are several excellent papers describing "beryl belts" where the elusive combination of beryl - lium and chromium may be targeted within the province. One of the best target areas is where beryllium-bearing pegmatites or granites interact with ultramafic chromium- rich rocks. Other good targets are where granitic stocks cut through black shales. Emeralds are also found in mica-rich reaction zones that occur at the contact of pegmatites and quartz-tourmaline veins continued on page 61

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