this thickening can be explained in a perfectly natural way due W | E donna agreed to self his and say the subsurface minerals all appear to come from the W. Miller later told me that the Cret. foramen in the Miocene (2 ray characteristic forms) are from the Austin-Taylor formations to the EAST. Pratt confirmed Hunter that the Cengric thicken to the E, but drew no conclusion. The next day R.F Baker told me that the Congric in the E. he believed to be at least 20,000 feet thick, and that the surface outcrops of the Congric to the N. of Balcoston are around 10,000 feet thick. I made the point that the Inner Dalv Dome, got their salt out of the Comanchian. In the Pine b. land field E to Bellevue field the Comanchian is in red beds and there is here at least 75 feet of only diate to me gone. Furthermore the Trinity and Fredericks- key them not against Llanoia and that was part of the Warkita geocam. Warkite Fredniastri