Pierre Shale(Phanerozoic | Mesozoic | Cretaceous-Late)at surface, covers 7 % of this area
Blue-gray to dark-gray, fissile to blocky shale with persistent beds of bentonite, black organic shale, or light-brown chalky shale. Contains minor sandstone, conglomerate, and abundant carbonate and ferruginous concretions. Thickness 1,000-2,700 ft (305-823 m).
Fox Hills Sandstone(Phanerozoic | Mesozoic | Cretaceous-Late)at surface, covers 2 % of this area
Bluish-green to green, white to dark-gray, yellow to tan, carbonaceous and iron-stained, cross-bedded, very fine- to coarse-grained, glaconitic sandstone and siltstone. Interbedded with gray and green to brown shale and silty shale. Thickness 25-400 ft (8-122 m).
Oahe Formation- Windblown Silt(Phanerozoic | Cenozoic | Quaternary | Pleistocene Holocene)at surface, covers < 0.1 % of this area
Obscurely bedded silt with paleosols; as thick as 6 meters (20 feet) where mapped. As much as 2 meters (7 feet) of windblown silt is present, but not mapped, on many level uplands southwest of the Missouri River, and less than 1 meter (3 feet) occurs at the surface throughout the state.
Eolian Deposits(Phanerozoic | Cenozoic | Quaternary)at surface, covers 20 % of this area
(loess and sand dune) Silt to medium-grained sand. Deposited as sand sheets and barchan, linear, and dome-like dunes and as veneer on uplands. Thickness up to 300 ft (91m).
Till, Stagnation Moraine(Phanerozoic | Cenozoic | Quaternary | Pleistocene [Upper Wisconsin])at surface, covers 24 % of this area
Heterogeneous, clay with silt to boulder-size clasts of glacial orgin. A geomorphic feature that is characterized by hummocky terrain with abundant sloughs resulting from stagnation of ice sheets. Composite thickness of all Upper Wisconsin till may be up to 300 ft (91 m).
Till, End Moraine(Phanerozoic | Cenozoic | Quaternary | Pleistocene [Upper Wisconsin])at surface, covers 15 % of this area
Heterogeneous, clay with silt to boulder-size clasts of glacial orgin. A geomorphic feature that is characterized by elevated linear ridges with hummocky terrain locally at former ice sheet margins. Composite thicknessof all Upper Wisconsin till may be up to 300 ft (91 m).
Lacustrine Sediments(Phanerozoic | Cenozoic | Quaternary | Pleistocene [Upper Wisconsin])at surface, covers 0.5 % of this area
Glaciolacustrine clay and silt with minor sand and gravel. Forms flat, low-lying terrain. Includes deposits from Glacial Lake Dakota and Glacial Lake Agassiz. Thickness up to 60 ft (18m).
Outwash, Collapsed(Phanerozoic | Cenozoic | Quaternary | Pleistocene [Upper Wisconsin])at surface, covers 19 % of this area
Heterogeneous sand and gravel of glaciofluvial orgin. Deposited as outwash sediments that collapsed due to melting of buried ice. Thickness up to 90 ft (27m).