Micro-World Gems & Gemology, Fall 2025, Vol. 61, No. 3

Gersdorffite in Quartz


Figure 1. Octahedral gersdorffite inclusions in quartz appearing as triangles. Photomicrograph by Nathan Renfro; field of view 8.16 mm.
Figure 1. Octahedral gersdorffite inclusions in quartz appearing as triangles. Photomicrograph by Nathan Renfro; field of view 8.16 mm.

While examining a 59.32 ct transparent colorless freeform shield-shaped step cut from Kara-Oba in the Karagandy Province of Kazakhstan, the authors noticed something curious. Using optical microscopy, X-ray powder diffraction, and standard gemological testing, we identified the sample as transparent rock crystal quartz and its eye-visible inclusions as the isometric nickel arsenic sulfide, gersdorffite.

Figure 2. When viewed from the opposite side of the quartz host, the same gersdorffite inclusions display as hexagons. Photomicrograph by Nathan Renfro; field of view 8.11 mm.
Figure 2. When viewed from the opposite side of the quartz host, the same gersdorffite inclusions display as hexagons. Photomicrograph by Nathan Renfro; field of view 8.11 mm.

What made this quartz subject particularly interesting to study was the euhedral morphology of the opaque, silvery gray, highly reflective, cubically modified octahedral crystals of gersdorffite. From one side of the quartz host, the inclusions with octahedral faces reflected as triangles (figure 1). Through the opposite side of the host, the faces of the very same inclusions appeared as hexagons (figure 2). In this sample, the perceived shape of the inclusions—triangles or hexagons—depends entirely on viewing direction.

John I. Koivula is analytical microscopist, and Nathan Renfro is senior manager of colored stone identification, at GIA in Carlsbad, California.