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Cluster of prismatic quartz from Dalnegorsk. The lines are evidence of preferential dissolution of calcite that had formed simultaneously with the quartz. Contacted crystals off to lower edge of upper side and tiny chip on top of one crystal: main portion of display area is in excellent condition. Mined ca. early 2000's.
Russia
Dalnegorsk
14,0x9,9x9,8 cm
492.3g
