29 
,,0F DENISON UNIVERSITY. 
fragilis occur both here and in Licking County, while Cyrtinia aciitir- 
ostris, which is found at Lodi, Medina County, rarely occurs here. 
Coarse sandstone, - - - - - lo ft. III2. 
Conglomerate II, - - - - - 5 ft. 
Sandstone, - - - - - - 12 ft. II. i 
Four and one-half miles northwest of Wooster, the above section 
was obtained in a quarry, No fossils which could with certainty be re- 
ferred to the strata farther south, were found here, but it is hardly pos- 
sible that the conglomerate exposed can be conglomerate I, as the strat- 
um below it is a solid freestone, containing Choneies^ while that be- 
low conglomerate I is usually a shale and no specimens belonging to 
the genus just referred to have ever been found immediately under 
conglomerate 1 . We should hardly expect conglomerate II to be so 
much thicker here than at Wooster; it must therefore be a local de- 
velopment, as it thins entirely out farther north. A few plants were 
found in it which is a new feature. The strata underlying the con- 
glomerate show premonitory symptoms of the decline farther north 
Freestone, _ . _ . _ 20 ft. II i. 
Conglomerate I, - - - - - 3 ft. 
Blue shale, - - - - - - 30 ft. I5. 
In this section which is exposed in Funk’s Hollow, five miles north- 
west of Wooster, conglomerate II is not represented, the top of divis- 
ion II having been removed by erosion; in II i Syrmgotheris carteri^ 
Sanguinolites aeolus ?, and Phaethonides occidentalis were found. These 
in Licking County are confined to division two. Conglomerate I is 
underlaid by thirty feet of blue shale which is entirely unlike its equiv- 
alent farther south. The nodule layer is not exposed. 
Sandstone and shales, - - , - - 60 ft. III2. 
Conglomerate II, - - - - - 
Losely bedded sandstone and shales, - - 15 ft. II. 
This section is revealed on the east and west banks of the Kill- 
buck, eleven miles north of Wooster. The sixty feet of strata form- 
ing the top of the section, consist of alterating shales and beds of 
white sandstone, which are quarried in places. No fossils were found 
in this part of the section. Underlying this is about fifteen feet of 
sandstone and differs lithologically from its equivalent at Wooster. It 
contains poorly preserved casts of Rynchonellae. The position of 
