QUOTE (Bill Harris @ Sep 30 2022, 02:01 PM)
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Note the coarse, conglomeratic, truncated unit below.
Adding onto Bill's observation, I think I see a fining-upward unit below the truncation, and a fining-upward succession with large-scale cross-stratification that has flattening-upward bedding.
My interpretation of these observations, in the context of the position of the outcrop, distal to the more proximal part of the delta, would be that these are the deposits of supercritical bedforms, likely cyclic steps (the lower coarse unit) and long wavelength antidunes in the distal delta front and toe-of-clinothem lobe element and feeder channel to lobe element transition zone.