Garnet Hill, Ely, Nevada • White Pine County • 7,050 ft

Almandine garnet & the Garnet Hill rhyolite fields

Named after the deep crimson Almandine garnet crystals found embedded in ancient volcanic rock atop Garnet Hill in Ely, White Pine County, Nevada. Explore the geological story and interactive specimen photographs that inspired the name and visual design of Almandine OS.

◆ Almandine Mineralogy & Crystal Geometry

Almandine (Fe₃Al₂(SiO₄)₃) is a deep crimson iron aluminum garnet mineral forged under intense heat and pressure inside the Earth's crust. Valued for its Mohs 7.0 to 7.5 hardness, high refractive index, and sharp 24 facet trapezohedral geometry, the crystal embodies durability and clean symmetry.

Its deep wine red facets and glassy vitreous luster inspired the obsidian, crimson garnet, warm desert gold, and crisp quartz white palette used across Almandine OS.

Mineral Species Almandine Garnet
Crystal Habit 24 Facet Isometric
Mohs Hardness 7.0 to 7.5
Refractive Index n = 1.810 (Vitreous)

▲ Garnet Hill, Ely, Nevada (White Pine County)

Rising to 7,050 feet just northwest of Ely, Nevada, Garnet Hill overlooks Robinson Canyon and the rugged Egan Range in the Great Basin high desert. Millions of years ago, Tertiary volcanic eruptions left behind pale pinkish gray rhyolite lava flows riddled with vapor phase cavities.

Inside those volcanic cavities, dark crimson almandine garnets crystallized directly on quartz and rhyolite walls, weathering naturally onto the mountain slopes today as one of Nevada's classic mineral landmarks.

Landmark Garnet Hill, Ely, NV
Elevation 7,050 ft (2,149 m)
Host Rock Tertiary Volcanic Rhyolite
Region Egan Range • Great Basin