Wea. THUR. JULY 29, 1909 Ther. The manor drl. finally has at its western base a decidedly blue-black intraformational cgl. It is a fangled mass of breccia bound in a muddy blue- black dolomite paste. About 4' is exposed above low water and about 14' more can be seen in the water. Honey is still thickan. In any event it is the same cgl. seen on Thursday at the Road metal quarry NW of Highgate Center. This then establishes the conclusion that there is no Middle Cambrian here, and that the Milton here rests on the Parker Slate.