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Series Names
 Soils that are shallow to bedrock

- bedrock occurs within 150 cm of surface
- a surface mantle of loamy hillslope or erosion surface sediments may be present
- pre-Wisconsinan paleosols may be present
- bedrock may be overlain by residuum from the insitu weathering of bedrock

 ISPAID MLRA ISPAID Parent Material ISPAID Landscape Position

 
SeriesSurface Material
ALLAMAKEEshallow to bedrock
ASHDALEshallow to bedrock
ATKINSONshallow to bedrock
AUREOLAshallow to bedrock
BACKBONEshallow to bedrock
BAUERshallow to bedrock
BERTRAMshallow to bedrock
BOONEshallow to bedrock
BUCKLICKshallow to bedrock
CALAMINEshallow to bedrock
CALMARshallow to bedrock
CLANTONshallow to bedrock
COPASTONshallow to bedrock
DARWINshallow to bedrock
DODGEVILLEshallow to bedrock
DUBUQUEshallow to bedrock
DUNBARTONshallow to bedrock
EMELINEshallow to bedrock
FAXONshallow to bedrock
FRANKVILLEshallow to bedrock
GALEshallow to bedrock
GASCONADEshallow to bedrock
GOSPORTshallow to bedrock
GOSSshallow to bedrock
HESCHshallow to bedrock
HIXTONshallow to bedrock
JACWINshallow to bedrock
KENSETTshallow to bedrock
LACRESCENTshallow to bedrock
LIMECREEKshallow to bedrock
LUANAshallow to bedrock
MARLEANshallow to bedrock
MASSBACHshallow to bedrock
MONTIETHshallow to bedrock
MOTTLANDshallow to bedrock
NASSETshallow to bedrock
NEWGLARUSshallow to bedrock
NORDNESSshallow to bedrock
NORVILLEshallow to bedrock
PAINTCREEKshallow to bedrock
PALSGROVEshallow to bedrock
RIPONshallow to bedrock
ROCKSANshallow to bedrock
ROCKTONshallow to bedrock
ROLLINGSTONEshallow to bedrock
ROSSFIELDshallow to bedrock
SCHAPVILLEshallow to bedrock
SHULLSBURGshallow to bedrock
SOGNshallow to bedrock
VANMETERshallow to bedrock
VILLAGEshallow to bedrock
WAUCOMAshallow to bedrock
WHALANshallow to bedrock
WINNESHIEKshallow to bedrock

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