Page Hill The west shore of Wilson Stream opposite the cor along 153.7-8, performed of a flow shalyite which gives in its upper portion and a duller red colour. The strike is N. 75° W dip 38° NE, the shalyite becomes an agglomerate - 153.8 [illegible] below the lower 50 feet and at the base as exposed a few feet for make dull red muds. These seem as the point in 153.8 and are splintered N 40° E in which direction (approximately) indicate a fault plane since the red muds plant against an acid porphyry tuff which forms the joint. This porphyry tuff is also greatly sheared [N 38° E] for over 50 feet S.E. of the contact. The porphyry with contours & the top of Knibley's Point and is of a prevailing light color. Red more than dark red not occur at all. No usual colors are various shades of a light gray with blue fragment occasionally pink. Strike N 12°-15° W dip 32° E. for near 100 yds S.E. of fault, and strike N. 32° W dip 28° NE. Between here the Point