Fort Union formation(Phanerozoic | Cenozoic | Tertiary Cretaceous-Late | Paleocene)at surface, covers 67 % of this area
Fort Union formation: Clay shale, siltstone, and sandstone; local lenses of impure limestone, and numerous lignitic beds; contains Tertiary plant and animal fossils but no dinosaurs; base generally placed at the lowest of the succession of lignite beds within it; includes the Tongue River member, Lebo shale member, and Tullock member.
Alluvium(Phanerozoic | Cenozoic | Quaternary)at surface, covers 5 % of this area
Alluvium: mainly valley fill consisting of silt, sand, and gravel; includes some terrace deposits and glacial drift of Pleistocene age in some areas; locally includes hot spring tufa. The older part of the alluvium, where present, is probably of Pliocene age.
Ludlow Formation(Phanerozoic | Cenozoic | Tertiary | Paleocene )at surface, covers < 0.1 % of this area
White, tan, yellow, and gray, cross-bedded, fine- to medium-grained,silty sandstone interbedded with locally bentonitic, gray siltstone, claystone, and sandy to silty claystone. Characterized by uranium-bearing lignite beds and "clinker" beds fromed by burning coalseams. Thickness up to 420 ft (128 m).
Hell Creek Formation(Phanerozoic | Mesozoic | Cretaceous-Late)at surface, covers < 0.1 % of this area
Tan to brown, light- to dark-gray, "somber beds" of shale. Interbedded with brown to red carbonaceous shale, gray and brown bentonitic silty shale, and gray, brown and yellow siltstone, sandstone, and claystone-pebble conglomerate. Thickness 260-600 ft (79-183 m).
Fox Hill sandstone(Phanerozoic | Mesozoic | Cretaceous-Late)at surface, covers 4 % of this area
Fox Hills sandstone: Typically shaly sandstone grading upward into massive brownish sandstone with white sandstone of the Colgate member locally at top.
Hell Creek formation(Phanerozoic | Mesozoic Cenozoic | Cretaceous-Late Tertiary | Paleocene)at surface, covers 13 % of this area
Hell Creek formation: somber-gray sandstone and greenish shaly clay and mudstone containing dinosaur bones; a few thin lignite and subbituminous coal beds.