Quartz after Calcite

specimen number:
2312240

location:
Droujba mine, Laki, Plovdiv, Bulgaria

description:
A sparkling thin shell of crystallized quartz, this forming a hollow cast after now gone scalenohedral calcite. The hollow nature of the specimen is evident in the video. This is complete all around and in great condition.

The Droujba Mine, situated within the prominent Laki ore district of the Plovdiv Province in southern Bulgaria, is part of a historic mining region with roots stretching back to ancient Thracian and Roman times. Modern industrial scale operations in the area developed primarily during the 20th century as part of Bulgaria's organized state-led mining sector for lead and zinc extraction. Geologically, the deposit is set within the complex metamorphic and igneous terrain of the Rhodope Massif. It is characterized by hydrothermal vein systems formed through Tertiary magmatic activity, producing rich polymetallic mineralizations consisting chiefly of galena, sphalerite, and pyrite, alongside well-crystallized gangue minerals like calcite and quartz.

Pseudomorphs occur when one mineral replaces another while preserving the original crystal form of the parent mineral. A classic example is quartz after calcite, where silica-rich fluids gradually dissolve the original calcium carbonate crystal and replace it with quartz. During this replacement process, the external crystal geometry of the calcite is perfectly maintained, resulting in a hollow or solid quartz replica with an exterior shape it never could have formed on its own.

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