slate that have the Linnarsonia faecica and Acritheli gotten in previous trips, Hydra still the follows the true Milton. In this general re- gion Keith holds that the Milton is not far from 8 or far thick, and that the Mallett has a like thickness. This is a remarkable similarity why the Milton arises to the south of Redbridge, there is from 30 to 20 feet of Milton followed by some dendules of far of St. Alban's slate. We then entered about four miles to the northwest through lots of Mallett to the Jave monument, a large boulder of obsolite. It is an erratic for Canada and is smoothed almost to polish by the glacial. It is one of the most faulted masses I have ever seen and must have taken place under eroding pressure, and then are recremental. It is one of the most of monuments at my appropriate for the places. The entered O.W and found large guanis in the marble of the early Beedmantown. The same one seen at Phillipstown.