The U.S. Geological Survey conducted an assessment of the mineral and energy resources of the Ashland Division of the Custer National Forest. The Ashland Division comprises approximately 780 square miles (2,030 square kilometers) between the towns of Ashland and Broadus in southeastern Montana. All rocks exposed in this area are part of the Tongue River Member of the Paleocene Fort Union Formation, consisting mainly of shale, siltstone, sandstone, thick coal, clinker, and thin lenses of limestone. The study area lies in the north-central part of the Powder River Basin. The resource wealth of the Ashland Division lands abides in enormous reserves of lignite and subbituminous coal with low sulfur and low to moderate ash content. One estimate suggests that about 42 billion short tons of non-leased federal coal occur within 3,000 ft of the surface in the Ashland Division. The entire extent of the Ashland Division is underlain by coals of the Tongue River Member; about 20 coal beds have been correlated through the area to a depth of 2,000 ft. Single coal beds are as much as 65 ft thick. The thickest coal beds of the study area include the Anderson, Dietz (or the merged Anderson-Dietz), and Knobloch beds. At least one-third of the study area contains strippable coal deposits, defined as one or more coal bed(s) of 5 ft or greater in thickness overlain by less than 200 ft of overburden. The Ashland Division contains 16 strippable coal deposits, which include several areas where thick coal seams are covered by less than 100 ft of overburden. The largest tonnages of strippable coal occur in the Ashland coal deposit, where the Knobloch coal bed is 40-58 ft thick and the Sawyer bed is 7-16 ft thick. Thick widespread outcrops of clinker represent another abundant resource of the Ashland Division area. Clinker is a baked, fused or melted rock, usually reddish or lavender, formed by the natural burning of an underlying coal bed. Clinker in the Powder River Basin region is often mined, crushed and used locally for surfacing improved unpaved roads and as an aggregate material in paved roads. Clinker is abundant, accessible, and easy to excavate. The proximity to roads where it is needed is the primary factor in its usage. The Ashland Division area has no record of oil or gas production despite a moderate amount of oil and gas exploration. Five prospective petroleum plays have been identified beneath the Ashland Division; they involve Lower and Upper Cretaceous strata that host producing horizons elsewhere in the Powder River Basin. These plays remain hypothetical for the Ashland Division area, which appears to lack the prominent anticlines and domes typically favorable for oil and gas accumulation. The potential exists for undiscovered coal-bed methane, although this resource has yet to be proven or developed within the National Forest. Areas with Fort Union Formation coal beds deeper than 500 ft should have potential for coal-bed methane. Many areas of the Ashland Division meet this criteria. No potential for metallic mineral de...