Diaspore is geologically common — it occurs in every major bauxite deposit on Earth. Gem-quality color-change diaspore is not, because the simultaneous geological conditions required (slow metamorphic crystallization plus the specific iron-to-chromium trace ratio plus crystal size large enough to facet) appear to be unique to the İlbir Mountains. Other bauxite localities produce diaspore in microcrystalline form, opaque masses, or without the trace-element profile needed for the alexandrite effect.

The verified facts

This entry is part of the Zultpedia editorial archive on color-change diaspore from the İlbir Mountains of southwestern Türkiye. Mineral species: diaspore (α-AlO(OH)). Hardness: 6.5–7 Mohs. Refractive index: 1.682–1.752. Specific gravity: 3.30–3.39. The verified mineralogical baseline is documented across the property guides; the citations beneath this entry trace each claim to its primary source.

Editorial framing

Zultpedia treats color-change diaspore as a single-source mineral species first and a trade-name commodity second. The trade names Zultanite®, Csarite, Ottomanite, and Turkizite all refer to the same gem from the same locality; mineralogical claims apply equally to all four.

Cross-references

See also the related entries listed beneath this article and the property guides for verified physical and optical values.