Wea. SAT. NOV. 6, 1909 Ther. Either this drl. is repeated Mallet or it is the older type Cambrian. In other words it is more Lower Cense and equivalent to the Milton. I doubt if its thickness is fudten from 20 ft. All of it dips E. and flumps, N. The dip flats out from 20° on the E., to 15° or even 10° on the W. The drl. first appears half way up the hill and to the top adds but little. Someone seems to have slipped. The dip is true when that reddish drl. is around 10° - 15° E. These beds are often from the overlying drl.