Lab Notes
Gems & Gemology, Fall 2015, Vol. 51, No. 3

Color Zoned Emerald

Jonathan Muyal, Nathan Renfro, and Amy Cooper
Different views show the color zoning in this emerald.
Figure 1. Left: When table-down, the stone is mainly colorless, showing some partially green overgrowth. Right: Face-up, the faceted stone displays an even and attractive dark green emerald color. Photos by Jonathan Muyal.

Cutting style and orientation are important considerations when cutting natural crystals with strong color zoning. Careful placement of these zones can distribute color by reflection, creating a uniformly colored finished stone when viewed face-up.

Recently, the Carlsbad laboratory received a 33.73 ct green octagonal step cut showing strong color zoning  (figure 1). The gem cutter skillfully placed a thin green color zone in this emerald along the pavilion facets so that the stone would appear uniformly green when in a face-up position. Standard gemological testing revealed a refractive index (RI) of 1.571–1.578 and a specific gravity (SG) of 2.72. Chromium-related features were observed in the red end of the spectrum when examined with a handheld spectroscope. All of these properties were consistent with emerald. During microscopic examination, minute jagged fluid inclusions and growth tubes were observed, proving the stone was of natural origin (figure 2).

Irregular green color zoning and inclusions.
Figure 2. When viewed from the side, irregular green color zoning is observed along with
minute jagged fluid inclusions. Photomicrograph by Jonathan Muyal; field of view 14.52 mm. 

Interestingly, the stone showed a strong green color zone very close to some of the pavilion facets, as well as hexagonal columnar-like growth and irregular zoning (figure 3). This type of zoning represents a late-stage influx of chromium and vanadium into the genetic environment, which were then incorporated into the crystal lattice of the beryl. Energy-dispersive X-ray fluorescence (EDXRF) revealed high levels of Cr and V in the green color zone, which was consistent with the observed color. Although similar zoning has been observed in emerald previously (E.J. Gübelin and J.I. Koivula, Photoatlas of Inclusions in Gemstones, Volume 3, Opinio Verlag, Basel, Switzerland, 2008, pp. 433–434), the zoning in this specimen was quite distinct.

White beryl is overgrown by green emerald.
Figure 3. The colorless spots indicate parallel columnar growth of white beryl overgrown
by green emerald. Photomicrograph by Jonathan Muyal; field of view 19.27 mm. 

This emerald demonstrates the significance of proper orientation and cutting style in fashioning high-quality gem materials.

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