Coal geology of the Bowman-Gascoyne area, Adams, Billings, Bowman, Golden Valley, and Slope Counties, North Dakota

Open-File Report 79-1698
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Abstract

The Bowrnan-Gascoyne area is located in southwestern North Dakota. It is situated on the southwestern edge of the Williston structural basin and the northeastern flank of the Cedar Creek anticline. Strata of the Fort Union Formation (Paleocene), consisting of nonmarine claystone, sandstone, and lignite, dip to the northeast 25-50 ft/mi. Seven correlatable coal beds of varying thicknesses and areal dimensions occur in the area. The thickest and most persistent of these beds is the Harmon bed which attains a maximum thickness of 38 ft in T. 134 N., Rs. 101 and 102 W. Analyses show a heating value of 5,915-6,680 Btu/lb and a sulfur content of 0.6-1.4 percent. Two areas of high-coal-development potential are located near Gascoyne and Amidon. The Harmon bed in these two areas contains a total of 740,000,000 and 650,000,000 tons, respectively, and is under less than 150 ft of overburden.

Study Area

Publication type Report
Publication Subtype USGS Numbered Series
Title Coal geology of the Bowman-Gascoyne area, Adams, Billings, Bowman, Golden Valley, and Slope Counties, North Dakota
Series title Open-File Report
Series number 79-1698
DOI 10.3133/ofr791698
Year Published 1979
Language English
Publisher U.S. Geological Survey
Description Report: ii, 35 p.; 11 Plates: 45.01 × 31.71 inches or smaller
Country United States
State North Dakota
County Adams County, Billings County, Bowman County, Golden Valley County, Slope County
Other Geospatial Bowman-Gascoyne area
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