"Farther east along the over southern ridge one sees another in pea green shale quarry and here about one-half of the material marked in above the limiters. My often the shales and the li, have about the same general dip as the shales on both sides of the li, employments [illegible] and in a case of li and shales in the form marked into one another during the deformation. It's the separate sheets of a rock slide that's marked together during the time of deformation. The li rocks have been marked into the shales or that the latter may crop around the li. From the top really bottom of the li ridge is larger than 200 feet. That's all theory of this rock slide across the li fault of the ridge it may be 100 feet a or better. I did not go across it to see, The over northern area also appears to have rock of Upper Cambrian li. It is at least 75 feet long and 40 feet thick. I am in it second large gap and once they that look like Caulerops. Shales dip to the S.W. at 50 to 60 degrees. There's another ridge & line on it to the west which is somewhat longer with a somewhat irregular strike these angle ridges"