(14) the place for the current Milltn fauna collected he par Ountur was ont one. Keith looked at the Miltin districts tells them then redded basal Upper Miltm limestone, and since they had Haddell Check said that they are of the true Milltm. It is a series of intrformational flat pettle sandy conglomerates. If this is true then we have here a division, formative contact of the Lower or true Millim followed out by the M.C. slate, but by the Upper Miltm Then Redded limestone series. The strata of the Lown Milltm is 30 degrees differ from that of the Upper Drielm. I proposed to call the Upper Miltm, the Missiguri limestone. The Middle Cambria slate or they be called the St. Albans slate. The Trenton conglomerate name will be retained as a member of the Mississouri. The Carlin Ledge conglomerate at the base of the Georgia one will once the Carlin conglomerate.