comes to the surface, either rising in sharp local folds or is pushed through the shifgate into the general level of the Devonian conglomerate. The Milton here is the usual sandy clc with small hard chert, and is often with intraformational conglomerates or is actually broken up into a dilomite sand. from there onse. Evidently to the west to Parker Quarry Brown's or Middle Cambrian. To the east of the Devonian conglomerate are other folded plates, and these go to the carly Georgia Center. Their age is unknown. For the structure of this region see the appended sheet. Bralert in this area completely mistrusts the schis- tosity for bedding. Everywhere in the shifgate the bedding is scarce seen because of the decided folding. As for his faults and repetition of the sections he is mistaken because of the assumed great thickness, his limestone level that he calls an intrafor. continental conglomerate is our Devonian overlying conglomerate, Bralert completely missed the structural relations, and through the stratigraphic