Oolitic calcarenite and micritic calclutite contact. Helena fm., grinnel glacier cirque, Montana. Example of soft sediment deformation. This looks like a loading structure – soft sediment deformation due to a density inversion – perhaps when some high-energy event (a storm?) dumped a bunch of relatively coarse ooids atop some squishy micrite mud. The upper oolitic layer glooped down into the micritic lower layer, creating this convoluted contact. #ScienzeGeologichePage