gular tendency. In most cases the bands are \frac{1}{2} in thick but at times about 3\frac{1}{4} to \frac{1}{2} and thicker. Always a crumple and firm band in alternation. These are so regular and look so much like the Squawtown banded slate that they appeared to me to be of glacial origin. Their age, however, is probably not so young as Permian, rather Devonian or older. In places one also sees the crumpling and faulting of the banded Phyllite as at Squawtown and elsewhere. It in those phyllites that lay on the western side of the notch valley and as they dip into the valley they are found to hide down very low and then. They can be studied both along the road between one and two miles south of Cranford Notch. See the small samples taken along. Monday, Sep. 20 - 1920 Mt Willard Climbed Mt Willard at Cranford Notch. Started in at 1890 and at the top it is 2786 feet above sea. The day is clear with but little wind. I had a fine view of the Presidential