(66) 8/22/57 - (Dillinger, Trout & Co. noted) 8/22/57/1 - from Here Coule, near Gapland area. - Pebble is an Concremitry Coule series. N of the point Highway passes through "E Caplak 1s. 8/22/57/2 - Barite runs 200m on plain, 45-30 miles Ee, "Hill Allen", Tex. The conglomerate is a large coarse high extending nearly SSW across the intervening Ranch just S of their Ranch. Inside and outside of this canyon 1 1/2 to 2 miles WSW for Brooks Ranch (see). The thinning of the clastic interval in the canyon and the gradual increasing dip of older rocks on the Here Ranch suggest there was an active high during upper Pliocene time through western Texas. It seems to have had little effect on the Here Ranch itself but did it. On Gapland conglomerate there is, excepts in a sandy facies on the south. (15) 8/23/57 [See p. 104 & 126] Sections 37 - 1/2 mile NE of Here Ranch Nourse - Level sheet dip 100 1) Agamous inclusion, rhythmic like. 2) Covered, 5' 3) Calcareudite, E-5.5 foudders, quantity to clc. pebble up to 1" creamy orange brown sand matrix. 4' beds; 25' 4) Covered, 35', probably conglomerate #3. 5) Calcarudite; pebbles & cobbleys bl., well rounded, light yellow sand matrix. Stone chert & quartzite (up to 25%). 8/23/57/1 base 8/23/57/2 40' np. total - 49' 6) Limestone, calcareous, some limestone pebbles but most pebbles are 1/2" chert. This is gradational with # below in the last 15' of that (15') unit. This unit (#6) become progressively less conglomeratic upwards. 1'-3' beds 8/23/57/3; 11' above base. 8/23/57/4; 32' above base- total 32'