Can recommend Mr. P. Le Bon tell us as (Correspondent) a place to stop. Mr. Beard says a better and cheaper place to stop in Mr and Mrs. Lempere Scott and Jersey people. Mr. Beard also said he would keep us. Has a daughter May. In coming along the Murailles this morning one sees how the Cape Barre beds some swing around and stand vertical as in Pierce Rock. Towards the Grand Coupe appear the Mt. Joli beds and then a fault which dips in the same Ordovician beds as those the other side of Mt. Joli. I do not see more than this one fault. Continuing from that out Charlie's fault between Cape Adams over to Pierce Rock is due to turning and dipping at an angle. Collected a few fossils from the very bed against which the Ordovician beds rest. Between them lies a fayer and angular unconformity. The upturned Pierce rocks were more deeply along the Murailles eroded before the Bonaventure formation was laid upon them than in the case at Pierce Rock. The Bonaventure conglomerate comes down as Red Tof to within 20 to 30 feet of the beach. The Trentonian fauna here is widely different in that of the U. S. Of brachiopods there are