correct with the datings of [illegible], Maine, all are therefore of the same age. These strata in western Maine are cubal metamorphosed by granites that were of Post Pennsylvanian time. Then, there were no known Carls, strata across southern Maine until about St. John's River B. The "Late Devon" plant beds of Perry Maine and in are probably of [illegible] time. The strata on either side of the Green Mounts have the schistosity dip through the Mounts, towards the east on the Lake Champlain side, and towards the west on the Connecticut Valley side. The Leyden schists of supposed Devonian time go north from Bennington to Littleton N.H. Hampshire. They are also at Lake Memphremagog.