USA – Gem Origins Overview

US gem deposits – Montana sapphire, Utah red beryl, Arizona peridot, California and Maine tourmaline; geologically diverse patchwork provinces.

By gemmology.dev editors Last updated
usa montana utah arizona california sapphire red-beryl peridot origin/usa

Introduction

The United States hosts geologically diverse gem deposits with no single dominant
orogenic province. Major deposits include: Montana sapphire (lamprophyre and
alluvial), Utah red beryl (rhyolitic volcanic), Arizona peridot (basaltic xenocyrst),
and California/Maine tourmaline (LCT pegmatite). Each deposit reflects a distinct
geological setting; no common chemical or inclusion fingerprint links them.

Major US Gem Deposits

State Deposit Host Rock Gems
Montana Yogo Gulch, Rock Creek, Missouri River Lamprophyre dike + alluvial placers Sapphire
Utah Wah Wah Mountains Topaz rhyolite (Eocene) Red beryl
Arizona San Carlos Apache Reservation Quaternary alkali basalt (xenocryst) Peridot
California Pala District, San Diego County Cretaceous LCT pegmatite Elbaite tourmaline
Maine Oxford County pegmatites LCT granite pegmatite Elbaite tourmaline (blue/green)

Montana Sapphire – Brief Overview

  • Three deposit types: Yogo Gulch (lamprophyre), Rock Creek (alluvial), Missouri River
  • Yogo: steely blue, rarely >2 ct, no heat treatment needed; low Fe; lamprophyre host
  • Rock Creek / Missouri River: pastel multicolour; mostly heat-treated for commercial blue
  • See dedicated file: origin/usa/montana-sapphire

Utah Red Beryl – Brief Overview

  • Wah Wah Mountains, Beaver County – the world's only commercial red beryl source
  • Hosted in Eocene topaz rhyolite; Mn³⁺ chromophore; typically <0.5 ct
  • See dedicated file: origin/usa/utah-red-beryl

Arizona Peridot – San Carlos

San Carlos Apache Reservation (Gila County) produces an estimated 80–95% of
commercial peridot by volume:

  • Host: Quaternary alkali basalt; peridot is a mantle xenocryst
  • Composition: Mg₂SiO₄–Fe₂SiO₄ (olivine); San Carlos material ~Fo₈₆–Fo₉₂
  • Properties: RI 1.654–1.712 (α–γ); biaxial positive; birefringence 0.035–0.038
    (strong facet doubling at 10×); SG 3.28–3.48; Hardness 6.5–7
  • Colour: Yellow-green to lime-green (Fe²⁺ chromophore)
  • Absorption: Three-banded iron spectrum: 493, 473, 453 nm (Foundation examination requirement)
  • Key inclusions: Chromite (spinel) with lily-pad tension fracture halos (Diploma
    requirement); ludwigite platelets; biotite; fluid inclusions
  • Origin discrimination: Not practical at bench level; San Carlos vs Hawaiian or
    Chinese peridot requires quantitative microprobe analysis

US Tourmaline (Brief)

California (Pala District) and Maine (Oxford County) tourmaline:

  • Both produce elbaite (Na(Li,Al)₃Al₆(Si₆O₁₈)(BO₃)₃(OH)₄) from LCT-type pegmatites
  • Colour range: pink/red rubellite, blue indicolite, bicolour, watermelon, parti
  • RI: 1.614–1.679 (uniaxial negative); SG: 3.01–3.06; birefringence: 0.014–0.021
  • California: historical Qing Dynasty export; Maine: first commercial North American tourmaline
  • Discrimination between California and Maine deposits, and between US and other
    tourmaline origins, is a laboratory-level task requiring trace element chemistry

US Tourmaline and Arkansas Diamond – Notes