Certain features of the report by George D. Morgan on the geology of the Stonewall quadrangle should be brought to the attention of those interested in the stratigraphy of Oklahoma, especially as these features in no way detract from the accuracy in mapping or description of the beds outcropping in the Stonewall quadrangle. In the correlation table, Plate XXVII, page 157, the Boggy to Wetumka is made the approximate equivalent of the Marmaton; the Wewoka, of the Kansas City; Holdenville, of the Lansing; Seminole, of the Douglas; Francis to Vanoss, of the Shawnee and Wabaunsee; and the higher beds, of...
You do not have access to this content, please speak to your institutional administrator if you feel you should have access.