Till, End Moraine (SDQlte;0)

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).

State	South Dakota
Name	Till, End Moraine
Geologic age	Phanerozoic \| Cenozoic \| Quaternary \| Pleistocene [Upper Wisconsin]
Original map label	Qlte
Primary rock type	clay or mud
Secondary rock type	silt
Other rock types	sand; gravel
Lithologic constituents	Major Unconsolidated > Coarse-detrital > Boulders (Glacial, till) Unconsolidated > Coarse-detrital > Gravel (Glacial, till) Unconsolidated > Coarse-detrital > Sand (Glacial, till) Unconsolidated > Fine-detrital > Silt (Glacial, till) Unconsolidated > Fine-detrital > Clay (Glacial, till)
Map references	Martin, J. E., Sawyer, J. F., Fahrenbach, M. D., Tomhave, D. W., and Schulz, L. D., 2004, Geologic Map of South Dakota: South Dakota Geological Survey
Unit references	Martin, J. E., Sawyer, J. F., Fahrenbach, M. D., Tomhave, D. W., and Schulz, L. D., 2004, Geologic Map of South Dakota: South Dakota Geological Survey
Geographic coverage	Aurora - Bon Homme - Brookings - Campbell - Clark - Clay - Codington - Davison - Day - Deuel - Douglas - Edmunds - Faulk - Grant - Hamlin - Hand - Hughes - Hutchinson - Hyde - Jerauld - Kingsbury - Lake - Lincoln - McCook - McPherson - Marshall - Miner - Minnehaha - Moody - Potter - Roberts - Sully - Turner - Union - Walworth - Yankton