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Geologic units in Roosevelt county, Montana

[Additional scientific data in this geographic area]

Flaxville gravel (Phanerozoic | Cenozoic | Tertiary) at surface, covers 12 % of this area
Flaxville gravel: Brown, yellow, and gray gravel, sand, and silt with marl and volcanic ash locally.
Lithology: coarse-grained mixed clastic; silt; volcanic ash
Hell Creek formation (Phanerozoic | Mesozoic Cenozoic | Cretaceous-Late Tertiary | Paleocene) at surface, covers 14 % 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.
Lithology: sandstone; mudstone; coal
Fox Hill sandstone (Phanerozoic | Mesozoic | Cretaceous-Late) at surface, covers 5 % 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.
Lithology: sandstone; mudstone
Glacial Sediment- Collapsed Glacial Sediment (Phanerozoic | Cenozoic | Quaternary | Pleistocene Holocene) at surface, covers < 0.1 % of this area
Unbedded, unsorted mixture of clay, silt, sand, and pebbles, and a few cobbles and boulders; as thick as 30 meters (100 feet)
Lithology: clay or mud; silt; sand; gravel
Bearpaw shale (Phanerozoic | Mesozoic | Cretaceous-Late) at surface, covers 10 % of this area
Bearpaw shale: Dark-gray and brownish clay shale; thick units of nonfissile bentonitic shale; calcareous and ferruginous concretions throughout; contains some thick bentonite beds.
Lithology: shale; sandstone; bentonite
Coleharbor Formation- River Sediment- Uncollapsed River Sediment (Phanerozoic | Cenozoic | Quaternary | Pleistocene Holocene) at surface, covers < 0.1 % of this area
Moderately well sorted cross-bedded sand and plane-bedded gravel, including sediment of melt-water and other rivers; as thick as 30 meters (100 feet). Flat-bedded sediment of gently sloping plains and terraces, commonly with braided-channel scars.
Lithology: sand; gravel
Fort Union formation (Phanerozoic | Cenozoic | Tertiary Cretaceous-Late | Paleocene) at surface, covers 45 % 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.
Lithology: shale; siltstone; sandstone; coal; limestone
playa (Phanerozoic | Cenozoic | Quaternary) at surface, covers 0.2 % of this area
playa
Lithology: playa
Alluvium (Phanerozoic | Cenozoic | Quaternary) at surface, covers 12 % 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.
Lithology: alluvium; glacial drift; carbonate

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