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Topography glacial. At mouth of Marvine Creek we found red sandstones which continued their exposures for 10 or 12 miles up river on south bank. Reached dense pine forests on south side of river about one or two miles below Hines' place, but quaking aspens etc. principal trees on north side. The last three miles or so we have seen no more sandstone and the glacial debris is all lava as in Marvine Creek. Reached Hines' place at 4:05 p.m. about 15 miles above Fitzgerald's, it is said. Dense pine timber comes down to south side of canyon to the bottom of the slope and ends abruptly. Scant tree growth on north side. Vegetation indicates about
