"above follows, Medina sandstone in district then say its acting somewhat irregular upon the Cataract, Upon Cataract shale about 4 feet instead of 10 as in the gulech. Then 3 ft. of their redded and magnesian- green siliceous limestone abounding in Helfhorn. Late down that no such development in the gulech and 1/2 mile to the west. Then the brown green shales, I see them lying to back to the gulech I see these same lie at the level of the gulech so that they are at the top of the section. There appears there's little a little difference in dip between the two sets of strata thus:- Medina then redded sandstone. 4 ft. shale upon limestone 3 feet Tunnel above 10 feet of shale (middle shales) green then agillucino limestone 2 feet 7 feet of shale thin shales Basal sandstone about 20 feet. Queenstown. The tunnel is on some than 1/2 mile over of western line of Leviston. dip exaggerated some."