gme at Bellefont, Pa., above which there is about 2000 feet of later Bell mountain but that shortly abortates in use of the Chazy. We then motored 17 miles out to Canajoharie by the change I the same game to see the section described in this same paper by Parson and Cremins (p. 638). Here the (<Tritic livid) Bellmountain is at the tip undulatory shortly due to folding or rather due to warping previous to the Trenton. The tip layers are also creathed out into shallow pockets and in places fats are plucked out. Into these hollows and undulations the Trenton fits but at the very base and flat one up to eight inch agency. thus are pettles mainly then rounded by the Bell- mantins. It is here 30 feet below the top that Reggmeal from the Fnt Shenter found bed. Then comes in at once the Trenton in thin lebs reflect with sands. Thickness 17 feet. None where there's no Lenville on any Bluel or Amoth dam. Aim. The Trenton limit me has just riffs near the hollows and near the top, with the crust