(It is not known that Laura Seton is meagres here) In the Ilitario the Tesnus is also present and folded with the same general style (S.W.) as in the Slam Out. Porus also got Liliurian here. In the Haftun Repim Udder gives a thickness of 1430 fut = Cit-Clr series. Since Blanchard days that deposition is continuous here. Supposed Pennosilranian goes unbroken into the Permian. Only lithologic proof for Pennosilranian; basal Haad shales with their beds of quartzite that look like Tesnus. No folding here, only domal uplift; due in the area the folding is thought to have died out. Blanchard has seen but one erinoid columnal in the Dimple li. No other forms other than sponge opicules are known in the Dimple. Harmond is not regarded as Tesnus. Baker at first [only interpreting how ignotable] and therefore this formation is to be disregarded. Blanchard says Nuevo lies below the Dela- ware li, that has "Chaturkaron", partly some Penn. and the Permian. Delaware - Dried. Cepitan = Vidrea, and the Lipton beds = William and Toney