TB,
quote:
Originally posted by Tranquility Base:
So no comment on the fact that the facies sorted hydrodynamically from each other are about 300 feet thick each?
Why, then, can I see multiple
coarse flat bedded conglomerates within a foot of each other?
"
Close up of the Tapeats at the same Verde River outcrop, showing crossbedding from underwater marine dunes that are interbedded with coarse flat bedded conglomerates from shore line wave deposits."
Mark
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Occam's razor is not for shaving with.