Sectionally quartzite in northern edge of West Union, on Ogleby Fork road. Projection 19 5/8 2ft and Massive ferrimisch gravel. 2 ft. " which l., splitting into 2 layers; 1 ft 4in. massive black l. duller marl, 6 in thick l., breaking up into 2 marly layers, 11 ft 9 in. an massive cemented, central part chinnical) and above this a thin nodular layer, 4 ft 6 in. massive third gravel with surface as are- terial, upper surface was marked. 2 ft 10 in., ferrimisch ferrimisch crass l. 3 ft Same as above, but with cherty noduled layers, 1 ft 8 in. massive ferrimisch coarsely worn marled at top. Base of spath. odent quartzite. Black argillaceous Osgood shales almost directly be- neth; At Benterville, the Clinton forms the summit of the ridge. About half way between Benta- vil and West Union there is a small knoll which jurn- both carries the system shall part of the West Union cliff. Loc. 1. Five miles east of Flemingsburg, Staff Wallingford road. Black shale hill on property of Charles Blanchet. 1 ft Black slate, partly Sinking, 2.5 ft shaly sandstone, partly Berea and Bedford. 113 ft Ohio shale. 46 ft red clay, apparently in upper part of Oxford. At least two limited sue fragments visible in the clay, and hence not supposed to be West Union, 27 ft red clay with ferriminnous frag- mets of limestone common, 18 ft red clay with thin limestone fragments such as are common in upper part of Crab Orchard. 36 ft clay shale undated older of Crab Orchard age. Level 1, strike in front of home of John Parker. I think the density of Crab Orchard could be determined along future since Clinton's exposed eastward.