Sunday August 21 - 1937 Wea. TUES. JUNE 22, 1909 Ther. To the E. of the Fremont Central R.R. one sees more of the Grindshi. The latter must lie nearly horizontal or that the Ordalite does not come to the surface until some place east of the Fremton pile. What underlies this marble area and east of the Fremont road cannot be told, but when the whole area is mapped over only forma- tion boundaries could be seen on the map. Sort back to the hotel in good shape, for the first time not tired out.