Walter 155 Stafford 923 200 200 1/4 X 8 {100} {80} {200} 385 farenheit = Reckman form - Joffin Clandrian 1/348 385 Tft / 1733 ft. 27 Below the sandstone come [illegible] laminated blue cloud dolomites, that are fine over-excavated (very smooth grains), ruffled, with some of interstratified some crystalline or limestone. One is edgewise englement. No joints of any kind, has except for Going back to the line of separation between the sandstone and the laminated dolomites are on just sum exactly sometimes 3 ft but with the cross from 1 to 2 miles across and filled in down to a depth of 3 to 5 inches. One two feet below occur Cyl/togyra, five feet below in a thinned bed of Cyl/togyra. The laminated beds are interbedded with the same fine grains smaller sandstone as different. Ruffling is constant and there are thick beds of crystalline limestone. Never occur the latter better developed anywhere the reason why one can so little own seeing in that the thin plates 1 limestone are washed away to from the edgewise engl. We estimate this beds to be at least 65 feet thick. We are near the end of an accessible section in Mary of San Core about 2 1/2 to 3 miles for the grains. Going a mile or more to the west we go down again the core has the same tendencies as is on the shale at Felipe's Core, where the dip reverses itself and goes up to the west in the next mile, at least 20 feet more of layer than reddish (weathered) sandstone reflect with shirty smooth surfaces that have furries, ruffled and some-circling. We see here [see me specimen] about four faults one duplicating about 100 feet of strata and another that brings up at least 40 feet older strata when the section again crosses on our way to the west. These are in place