from the base to the very tip. They are charrned of shale beds are depicted in the conglomerate intregration all. The series consists probably about 85% of coarse dark green quartzitic conglomerates in all of the pebbles average from 1/4 to 3/8 inch in dia. The sandstones may as a rule be said to be then bedded and very rare and then appear thin zones of black or greenish slakes that range from 0 to These shale are not often seen as those of the Dalong series. Two or more feet. A bit is the bottom fourth of Ottes. Vello over again but darker in color and with the shale pebbles here of black shale, layer thin and once abundant. The reason why there are coarse grains seems to be due to grains of thin beds that break up into smaller pieces and or come to cover the Grand. Comparing the two sides of the Delaware River though letting things But one sees that the coarse grains are not the same in places and then the New Jersey side shows no shale in the coarse areas.