living zones and intraformational pebbles of cement like rock. A shallow sea bottom torn up by the waves reworking the living mud layers. After seeing it down stream from the falls opposite the abandoned mill I see that it is thinner bedded, and more third down quite due to the rain are inclosing grains. Often and often in a breathend piece of this grit, atly where off shale lumps have been looked out. Without hearth and without marked transitional takes zone it goes into the Shifl Falls shale. The upper 10 fut may be called another braterlime but was or sandy or dirty as the very thin bedded. It area- thin yellow but inside in blue. Has ammonites. calcite gathering flat and concentric lumps of to bricks thick one or ten circular. Its mud our cracked and jassos imbedder into the Red Shifl Falls shales, interbedded with an occasional blue shale. Thicken about 30 fut. There beds in the upper fut have much intraformational beds, a whitest sand a green mud with red shale, square pebbles (clunee material). Some of these goes are also common (something disturbed out)