Pierre Shale(Phanerozoic | Mesozoic | Cretaceous-Late)at surface, covers 0.1 % 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).
Till, Ground Moraine(Phanerozoic | Cenozoic | Quaternary | Pleistocene [Upper Wisconsin])at surface, covers 26 % of this area
Heterogeneous, clay with silt to boulder-size clasts of glacial orgin. A geomorphic feature that is characterized by smooth, rolling terrain. 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 16 % 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).
Till, Stagnation Moraine(Phanerozoic | Cenozoic | Quaternary | Pleistocene [Upper Wisconsin])at surface, covers 45 % 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, Minor Moraine(Phanerozoic | Cenozoic | Quaternary | Pleistocene [Upper Wisconsin])at surface, covers < 0.1 % of this area
Heterogeneous, clay with silt to boulder-size clasts of glacial orgin. A geomorphic feature that is characterized by elevated linear ridges including minor, washboard, or recessional moraines. Composite thicknessof all Upper Wisconsin till may be up to 300 ft (91 m).
Outwash, Collapsed(Phanerozoic | Cenozoic | Quaternary | Pleistocene [Upper Wisconsin])at surface, covers 8 % 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).