Montana Governor and First Lady
's Math and Science Initiative
Black Gold

Mile Post 6.6 on Secondary 308, near Bearcreek
About sixty million years ago, this area was part of a vast
subtropical coastal plain with major rivers flowing
eastward into an inland seaway. Between these major
river systems great thicknesses of plant material accumulated
that was converted to peat and eventually buried under sand,
mud, and other sediments. Over millions of years, the increased
pressure and temperature from burial compressed and baked
the peat into medium grade sub-bituminous coal. Between
about 70 to 55 million years ago, tectonic forces caused
dramatic deformation of the region and culminated in the
formation of mountain ranges like the Beartooth, Pryor, and
Big Horn Mountains. This deformation tilted the sedimentary
layers and associated coal seams in this area downward to the
east. The coal in the Bear Creek field is part of the immense
Fort Union Formation, which is estimated to contain over 200
billion tons of coal in eastern and central Montana.
Black Gold
A Brief History
“Yankee Jim” George discovered the Bear Creek coal field in 1866, but it would not be commercially mined for another forty years with the arrival of the Yellowstone Park Railway. Five companies operated coal mines in this narrow valley by 1910. Two towns, Bearcreek and Washoe, provided living quarters and services to the multi-ethnic miners and their families. The field contains about a dozen workable coal beds, with some seams as thick as 11 feet. Underground coal mining peaked in the early 1920s, when Bear Creek coal powered railroad locomotives, fueled the Anaconda Copper Company’s smelter in Anaconda, and heated homes throughout Montana. Production gradually diminished as the railroads converted to diesel-powered locomotives and private homes began using natural gas. Commercial coal mining in the Bear Creek field ended in 1953 when the Smith Mine closed. Small privately operated companies provided coal to area residents for years afterwards.
