Saturday Oct. 25 [1851] "...Left camp
"desertion" where Indians without cause have left us we
entered the canyon. Perpendicular bluffs 4 or 5 hundred feet high
hemmed us in on both sides. But by threading the stream, crossing
and recrossing probably a hundred times through quick sands and bogs
& over precipices and barrancas, we proceeded about 8 miles where we
encamped on good grass...Rock of red feldspar predominates. A
mountain of magnetic iron ore was passed today...The banks were covered
with a conglomeration of trap porphiry [sic], pudding stone, sand, and
boulders often approaching granite. The rocks are of plutonic and
metamorphic origin. The following is a sketch from camp."
-Whipple
Collection, Oklahoma Historical Society