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Series Names
 cf. Camp Creek Member:
Stratified Sediments (Usually Historic Age)
- The sediments are layered in beds that vary in thickness.
- In the upper 25 cm of the unit, stratification may be disrupted by plant rooting and animal burrowing.
- Often contains artifacts dating to the historic period (tin cans, fence wire, glass, crockery.
- Modification of the sediments by soil formation is minimal
- Is thickest in areas adjacent to the modern channel.
- Usually buries the presettlement soil.
- Dates from 400 years before present to modern times.
- NRCS Map Units with these series are on floodplains, concave terrace/floodplain depressions, footslopes, alluvial fans, upland drainageways.
- Coarse textured, stratified 2C and 3C horizons in some series may represent presettlement fluvial sediments.

 ISPAID MLRA ISPAID Parent Material ISPAID Landscape Position

 
SeriesSurface Material
ALBATONCamp Cr > 150
BLAKECamp Cr > 150
CARRCamp Cr > 150
CHASEBURGCamp Cr > 150
DOCKERYCamp Cr > 150
ELONCamp Cr > 150
FLORISCamp Cr > 150
GRABLECamp Cr > 150
HAYNIECamp Cr > 150
KLUMCamp Cr > 150
LOSSINGCamp Cr > 150
MCPAULCamp Cr > 150
MODALECamp Cr > 150
MORCONICKCamp Cr > 150
NODAWAYCamp Cr > 150
OMADICamp Cr > 150
ONAWACamp Cr > 150
PERCIVALCamp Cr > 150
PERKSCamp Cr > 150
REEDSCREEKCamp Cr > 150
SARPYCamp Cr > 150
SCROLLCamp Cr > 150
TICONICCamp Cr > 150
VORECamp Cr > 150

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