Today's structure comes from the Wilkins Peak Member of the Eocene Green River Fm, in SW Wyoming (click on the picture and it will get larger!):
Interference Ripple Formsets! These little bastards form where there are two dominant paleoflow directions, and reflect the complexity that many flows exhibit as they move sediment around. It also serves as a good example as to why ripples are, for the most part, the most useless of the sed structures; they are commonly subject to extremely local whims of turbulent flow. Oh well!
1 comment:
Hi nice reading your ppost
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