Below the Corlin clay, has but little foreign material, and it is are [illegible] small becoming to differentiate there. Hidden smears bottles of these are introduced and try to come from once above out and lay them through the top. The stratified Corlin clay. appears to merge into the stratified material but this is primarily due to the bitterns having moved out the stratified beds during the caenic orogeny. The fossil beds are near from the growth end of the stratified beds about half way of its thickness. Is about 15-20 feet. Just one few transitions, for though I cannot get to a bay face. This stratified material begins with the Corlin clay, has to affect the center after the transition in the 15 [illegible]