Page:Field Notes of Junius Henderson, Notebook 2.pdf/116

 ward the Fountain rests on red granite. Along road just before leaving the creek and again on the hill just south of are small outcrops of Fountain conglomerate dipping E into the gneissic mt. They are only a few square feet in area. Could not determine whether they are left in such positions by fault or fold. On W side of, which reached at 11:a.m., the granite contains large bodies of white quartz. The mt. On W side is gneiss. The Fountain occupies E side of park, dipping inward from all sides. Killed a just S of, in. Left Park at 2 p.m. Strata badly twisted where enters  and below there for some distance. Reached Hotel at 6:15, very tired and sore. Here as elsewhere, Lyons is sharply differentiated from Fountain in both color and texture, in the escarpment. Fountain contains