Some pictures from Buckskin Gulch 2017.
The water was cold. The muck sometimes wanted to keep our shoes. It reached our shorts but not all the way up to our butts.
A curious little sedimentary study: Walls are Navajo Sandstone which have been incised by the intermittent creek/river. In the bottom of the canyon is evidence of continued cutting along with examples of more recent deposition and even more recent cutting. The light colored layers are slack water deposits, placed and cut away in turn. The reddish “powder” is Navajo Sandstone which was eroded back into sand grains up on the high ground outside this canyon. This sand was then rolled, skipped, and lifted by wind and dropped into the canyon when the leap across the top was too far. It filtered down the hundred fifty feet and landed on the “windward” side of the canyon.