Tibetan Quartz

Tibetan quartz is not a distinct mineral but a trade name for clear to smoky quartz (SiO₂), often carbon-included and double-terminated, collected from the Himalayan region. Tibetan quartz refers to quartz crystals hand-collected at extreme altitudes in the Himalayan region - typically 4,000-5,000+ meters elevation in Tibet, Nepal, and northern India. The crystals formed in alpine fissures and cavities within metamorphic and igneous rocks as part of the ongoing Himalayan mountain-building process.

Many Tibetan quartz crystals contain distinctive black carbon or hematite inclusions that give them a unique 'dirty' or speckled appearance unlike the clean crystals from lowland Brazilian or Arkansas deposits. Some are doubly terminated (pointed at both ends), having grown freely in open fissures. The extreme altitude means collection is physically demanding - miners work at elevations that cause altitude sickness in most people, often reaching crystal pockets through hand-dug tunnels in harsh terrain.

The provenance is the primary value driver. Mineralogically, Tibetan quartz is the same SiO₂ as quartz from anywhere else. What makes it special is the collection context: crystals gathered by hand from the highest mountains on Earth, in a region deeply associated with spiritual practice.

Tibetan quartz is identified as quartz with characteristic black carbon or hematite inclusions, often with a natural surface texture from high-altitude weathering. Many specimens are doubly terminated. At hardness 7, it's standard quartz.

Distinguish from regular included quartz from other localities (provenance is the distinction, not mineralogy), from Herkimer diamonds (New York origin, exceptionally clear), and from Himalayan quartz without inclusions (sold under the same name). There is no mineralogical test that confirms Tibetan origin - provenance relies on supply chain trust.