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Series Names
cf. Gunder or Corrington Members
No Series or Map Unit is linked to the Corrington Member.
- The following series occur in NRCS Map Units on footslopes and alluvial fans where the Corrington Member is typically found.
- On such landforms, if a buried soil is present, the sediments are Corrington; if absent, the sediments are Gunder Member.
- NRCS Map Units for some of these series also occur in upland drainageways and stream terraces.
Corrington Member (usually early-middle Holocene in age)
- The unit consists of vertically stacked, fining upward sediment packages.
- At least one buried soil is present, typically at the top of fining upward sequencies.
- Unit is found beneath alluvial fans and colluvial slopes along the margins of large- and moderate-sized valleys.
- Deposited between about 9000 and 2500 years before present.

 ISPAID MLRA ISPAID Parent Material ISPAID Landscape Position

 
SeriesSurface Material
CANTRILGunder or Corrington
CASTANAGunder or Corrington
ELYGunder or Corrington
JUDSONGunder or Corrington
MARTINSBURGGunder or Corrington
MOINGONAGunder or Corrington
NAPIERGunder or Corrington
OLMITZGunder or Corrington
TERRILGunder or Corrington
WORTHENGunder or Corrington

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