File:Old chromite mine (Beartooth Plateau, Montana, USA) 2.jpg

English: The Red Lodge Mining District is located near the southeastern termination of the Beartooth Mountains, southwest of the town of Red Lodge in southern Montana, USA. Active mining took place during the 1940s. Most of the old, small mines occur on the high plateaus or just below the eroded plateau edges.

Mines in the Red Lodge District targeted chromium ores in the form of black-colored chromitite rocks hosted in serpentinite and bastite (= serpentinized pyroxene). In this area, lenses, or pods, or fault-chopped stratiform bodies of serpentinite occur among high-grade metamorphic rocks such as quartzites, gneisses, migmatites, amphibolites, etc. Chromitite is a coarsely-crystalline textured, intrusive igneous rock that is rich in the mineral chromite (FeCr2O4 - iron chromium oxide).

The rocks in the Beartooth Mountains are very old. They are principally Archean in age (2.5+ billion years old). The chromite-bearing serpentinite bodies of the Red Lodge District were originally chromite-bearing peridotites (dunites) of early Neoarchean age, or older. Granulite-grade to upper amphibolite-grade regional metamorphism at about 2.75 Ga altered the original dunites to serpentinites. The rocks of the area were also altered by greenschist-grade metamorphism between 1.6 to 1.8 billion years ago, during the late Paleoproterozoic.

Locality: old chromite mine, near the eroded edge of the Beartooth Plateau, southeastern side of Rock Creek Canyon, southwest of the town of Red Lodge, Red Lodge Chromite District (Red Lodge Mining District), Beartooth Mountains, southern Montana, USA (45° 02' 04.36" North latitude, 109° 24' 35.11" West longitude)