Mineralica 2025-4

On the trail of red beryl: A collector's adventure in the Thomas Mountains

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David Evans (2025): On the trail of red beryl: A collector's adventure in the Thomas Mountains. Mineralica 2025-4, pp. 6–11.

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David Evans (2025): On the trail of red beryl: A collector's adventure in the Thomas Mountains. Mineralica online, December 2025. https://mineralica.com/a/d9w2z9 (accessed October 13, 2026)

In the deserts of Utah, David Evans saw a collector's dream come true: on a dig near Delta he found red beryl, one of the rarest gemstones in the world – amid blazing heat, hard rhyolite and topaz.

Red beryl with bixbyite and topaz on pseudomorph garnet. Searle Canyon Red Beryl Mine, Juab County, Utah. Approx. 18 × 10 × 8 mm. László Kupi photo.

In August of this year, I was given a rare opportunity: to join a collecting and digging tour with Gem Tours outside of Delta, Utah, in search of the legendary red beryl, one of the rarest gemstones on Earth. Among mineral collectors, this name borders on mythical. Only a few localities worldwide have ever produced crystals of this mineral, and the Thomas Range in western Utah ranks among the most important of them.

I’ve been an avid collector of crystals, gemstones, and even gold since childhood, but Utah was entirely new territory for me. After a long drive from Denver, I spent the night in Delta before meeting my guide, Christian, early the next morning.

Red beryl on rhyolite matrix, Searle Canyon Red Beryl Mine, Juab County, Utah. Approx. 19 × 14 × 11 mm. TheGemTours.com photo.

From Delta, we followed a short off-road trail that wound its way into the rugged foothills of the mountains. The landscape was barren and sunburnt, both harsh and fascinating. Christian, who had scouted the site the day before, handed me a small handful of gleaming topaz crystals he had collected. It was my first encounter with Utah topaz. It is gleaming in warm champagne tones, soft pinks, and clear whites, so different from the cool blues I knew from Colorado.

After a quick safety briefing, we descended into one of the main pits which are part of a network of excavations that have been worked regularly since the early 1980s. By mid-morning, the temperature had already climbed close to 100°F (40°C), and the pale rhyolite walls reflected the heat relentlessly. With hammer and chisel, we worked our way through the tough volcanic rock—layer by layer, strike by strike.

In Mineralica 2025-4

This article runs on pages 6–11. The first 2 pages are free to browse.

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