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directly on an uneven eroded surface of rotten, deep red granite, contact showing for100 ft., conglomerate dipping 10˚ bearing about E. The center of the plain for some distance back is covered with a thin remnant of Fountain conglomerate thus showing approximately the ancient sea bottom. Another inlet (sic) of the Fountain, including the upper beds extends far west of Livermore. It is a syncline> At Livermore dip is only about 20 to 40 bearing NE. Camped at Owl canyon at 6 p.m.
Owl Canyon, Friday June 14/07
Dodds and I started up canyon on foot in morning and in narrow part, west of bridge, in limestone at top of next to top limestone bench found brachiopods of carboniferous type. In a much lower horizon where
