Therefore this conglomerate may make the = of the Swantum and if it is then the Swantum does not lie immediately beneath the Georgia slate - Mohawkian. The question also arises in this giant cmpl. at the base of the M.C. and is or in the midst of the M.C. shale. The forms in the li. petter are M.C. and therefore therefore there must be M.C. li. below the cmpl. The cmpl. cannot be intraformational once it has various kinds of li. petter, the white marble kind as large as 5 or 6 full acres. Then maybe out of the Otobester. The entire section between St. Althaus Bay and St. Althaus needs to be restudied. Just east of St. Althaus Bay occurs the L.C. sequence See my map for the loc. of Chesterian forms. A little further east and to the south of the road is a cmpl. hard to see. What is the age of this cmpl. and now what does it lie? Further east and on the north side of road is the Odamus faster cmpl. above described. It maybe that all the slate hereabouts in M.C., and not at all Georgia as Keith defines it.