Tuesday August 29 - 1933. Wea. SAT. OCT. 2, 1909 Ther. Am came the surprising thing of the day. My new place of last year at "Mid. Cambrian" turns out to be wrong. There is no M. C. here and the Highgate directly makes a decidedly emyl. dol. This I called the Ruff Brook but which must be the Parker dol, seem to be 5 some thicker. The facts are as follows: My "Ruff Brook" dol. emyl. is basal to High-gate dipping E. at a low angle. If this angle is pro-jected W of the N.-S. and it is seen to make Parker slate considerably distorted and folded. It makes the surface of the hill owing to the W., and may be as thicker than the mean mak-ing Parkers Cattle 30' - thick. On my "Ruff Brook dol" box is a covered area and to the E. in the little lies of erof folded slate having the trilobite, for though to be of St. Albans age and which partly are of earlier Highgate Time. In the quarry stuff above me I found the horn- like fossil and it also occurs in the quarry when I get the trilobite. See the one found here and a trilobite head. Hornels place forms is on north side and here he got lam experiments, lotites (name) food and my ne