Almandine Garnet in Volcanic Rhyolite (Garnet Hill, Ely, NV)
A sharp, glassy deep crimson almandine crystal nestled inside a natural quartz cavity within pale volcanic stone from Garnet Hill in White Pine County, Nevada.
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 (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.
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.
A sharp, glassy deep crimson almandine crystal nestled inside a natural quartz cavity within pale volcanic stone from Garnet Hill in White Pine County, Nevada.
Bright, symmetrical trapezohedral crystal faces reflect incoming light cleanly across crisp isometric edges.
Two high luster garnet crystals formed side by side inside a weathered volcanic rhyolite cavity.
Deep dark garnet facets set against warm Great Basin golden stone from the Garnet Hill collecting slopes.
Looking across the pinkish volcanic slopes, juniper woodland, and Great Basin mountain horizon outside Ely, Nevada.