HOLOCENE ARROYO CUT AND FILL CYCLES, SOUTH CENTRAL WASHINGTON
The modern arroyo exposed evidence of at least one previous episode of arroyo incision to a depth of ~4 m between 3140±40 cal yr BP and 1000±40 cal yr BP. This paleo-arroyo cut through a tephra layer from Mt. Mazama (~7700 cal yr BP) at multiple locations. Filling of this paleo-arroyo with fine to coarse cross-bedded sand ceased between 520±60 cal yr BP and 110±40 cal yr BP. A distinct 0.5-1 m thick, finely-bedded silt unit caps the fill, which may have been deposited as Selah Creek spread onto the floodplain forming the shallow wide channel depicted in photographs taken prior to the dam ruptures.
Changes in sediment supply, paleoclimatic conditions, flooding characteristics, or a combination may have contributed to paleo-arroyo cycle(s) within the Selah Creek basin. Additional dating will allow further investigation into the possibilities of synchronous arroyo incision on multiple channels within the local region and initial indications of negative correlations with similar alluvial cycles in the southwestern United States.