Jacquet River, Monday July 15=1929 (cont.) Nearly everywhere the upended Silurian is unmem- formatively retained by the Bromavertine implements. It always overlies directly half the Silurian. It does not in any one case than 1/2 miles, and its thickness is not great. At the west end of the section it runs north to the Silurian but hits against a vertical cliff of it. Allrock is displaced or grames physiographically from if the Bromavertine was not laid down in Cretaceous time. He thinks he who has some support in the Foraminifera found by Clarke and determined by Chapman. This evidence is almost worthless. To me all of it is best called Pennsylvanian and certainly isn't older than Drinker = dip Mississippian.