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Series Names
 Shallow to pre-Wisconsinan Till
- pre-Illinoian till occurs within 150 cm of the surface under a surface mantle of hillslope or erosion surface sediments
- soils of these series form in pre-Wisconsinan hillslope and alluvial sediments on uplands.
- NRCS Map Units for these series are on uplands and upland drainageways

 ISPAID MLRA ISPAID Parent Material ISPAID Landscape Position

 
SeriesSurface Material
AFTONshallow to till
ANSGARshallow to till
ARBORshallow to till
AREDALEshallow to till
BASSETTshallow to till
BURCHARDshallow to till
CLYDEshallow to till
COGGONshallow to till
CRESCOshallow to till
CRESKENshallow to till
DELFTshallow to till
DINSDALEshallow to till
EGANshallow to till
EVERLYshallow to till
FARRARshallow to till
FLOYDshallow to till
FRANKLINshallow to till
GARAshallow to till
GORINshallow to till
HAVANAshallow to till
JAMESTONshallow to till
KENYONshallow to till
KLINGERshallow to till
LETRIshallow to till
LINDLEYshallow to till
LISCOMBshallow to till
LOURDESshallow to till
MAXFIELDshallow to till
NORTHBOROshallow to till
OLINshallow to till
ORANshallow to till
OSTRANDERshallow to till
PINICONshallow to till
PROTIVINshallow to till
RACINEshallow to till
RANSOMshallow to till
READLYNshallow to till
RENOVAshallow to till
RICEVILLEshallow to till
RUSSELLshallow to till
SACshallow to till
SCHLEYshallow to till
SHELBYshallow to till
STEINAUERshallow to till
TRIPOLIshallow to till
WAUBEEKshallow to till
WILMONTONshallow to till

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