"Showed samples of the big conglomerate, and the slate beneath it to Rawson, he did not know what to make of it but said it could be either the equivalent of the basal Cambrian conglomerate seen in the Metacoma Mts., or another conglomerate that is undulain by slate and quartzite which Rawson calls Barnes cong. above, but which Dauten refers to the Pretergne. I rather think Rawson is correct... In any event we intend to return to the Pepper-sauce canyon with Rawson and sort the thing out. Jan 30 - Feb 4, 1924, Worked most of the time on the text-book.