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[[encircled]] 7 [[encircled]]

Remarks on March 19, 67 - The vertical massive beds tipped up along the mountain front suggest Sullivan Peak. The beds are so dolomitized that we could not find any fossils in it. I was unable to find diagnostic brachiopods in the ammonite beds although we saw what looked like Peniculauris and Torynechus, a fragment. This suggests Bed 3 of King. The tipped up beds on the front might be bed 2 which has some biohermal material in it.

On the way up the Mountain we found a loose [[underlined]] Institella [[/underlined]] as float under the big sandstone but we could not find it in any of the limestones. I think the upper limestone is probably Wedin but can't be sure. [[underlined]] Edriosteges [[/underlined]] was common in biohermal limestone and [[underlined]] Coscinophora [[/underlined]] occurred just under or in the Cretaceous. The uppermost beds under the Cretaceous may be a basal conglomerate, certainly there was a variety of pebbles in the conglomerate.