Till, Ground 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 smooth, rolling terrain. Composite thickness of all Upper Wisconsin till may be up to 300 ft (91 m).
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). Faulted and contorted supraglacial sediment with hummocky topography.
Till, Stagnation 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 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).
Till, End 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 with hummocky terrain locally at former ice sheet margins. Composite thicknessof all Upper Wisconsin till may be up to 300 ft (91 m).
Eolian Deposits(Phanerozoic | Cenozoic | Quaternary)at surface, covers < 0.1 % 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).
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.
Dark, obscurely bedded clay and silt (overbank sediment); generally overlying cross-bedded sand (channel sediment); as thick as ten meters (30 feet); on flood plains of modern streams.
Outwash, Undifferentiated(Phanerozoic | Cenozoic | Quaternary | Pleistocene [Upper Wisconsin])at surface, covers < 0.1 % of this area
Heterogeneous sand and gravel, with minor clay and silt. Deposits of glaciofluvial orgin including outwash plains, kame terraces, and other undifferentiated deposits. Thickness up to 30 ft (9m).
Well-sorted, medium sand with obscure bedding; poorly developed palesols common; as thick as 10 meters (30 feet); knobby topography consisting of inactive transverses or longitudinal dunes nearly obliterated by more recent blowouts.
Outwash, Collapsed(Phanerozoic | Cenozoic | Quaternary | Pleistocene [Upper Wisconsin])at surface, covers < 0.1 % 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).
Laminated silt and clay of glacier-dammed lakes; as thick as 60 meters (200 feet). Flat-bedded sediment elevated above surrounding area or floded sediment with hummocky topography.
Lacustrine Sediments(Phanerozoic | Cenozoic | Quaternary | Pleistocene [Upper Wisconsin])at surface, covers < 0.1 % 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).