westward from Toroweap Valley. In this section several features illustrating the early stages of canyon cutting and of local vulcanism will be concealed. Also covered will be remnants of lavas that flowed down the river channel and sediments, in two places, formed in ancient lakes or reservoirs behind natural lava dams. A detailed account of these remnants of lava flows and other features of local vulcanism appears in a paper by McKee and Schank titled "The Lower Canyon Lavas and Related Features of Toroweap in Grand Canyon," published in the Journal of Geomorphology, Volume 5, Number 4, pages 243-273 (1942). d. Recreation The most obvious change in recreational use of the canyon brought about by the Bridge Canyon Project would be the li...