Monday Sep. 10-1934 In the afternoon near (N.W.) 20 miles from Phillipsturg to Laerlle to see the string of dol, ls. freccia. It is made up with many layered dol. Beelmontian rocks (some joints seem) up to 11 feet deep, many small masses of chaggy with comminuted fossils, and one careful with smaller pieces of Trachyma ls. only Ammufella quincens, Dalmanella, small hand-lig byggram and good heads of Trigoneulus. In places the rocks are nearly all Beel-montian, with few chaggy masses. At other places the blocks of smaller Beelmontian are converted into chaggy masses. At that time nearly all the pieces are small chaggy and Trachyma pieces. From the central body of the Beelmontian and elsewhere around chaggy beds, but my exposed Trachym is known decadent to be. To one it seemed these early (striking N.E.-S.W.) once made the base of a submarine fault scarp. The chaggy here is 200' thick. The scarp may have stood too high with the extraordinarily shelling down, and the storm waves tearing down the scarp. After Trachym came into not there. Administering 25 and it very.