WEST VIRGINIA GEOLOGICAL SURVEY. 623 



Section, ascending, hand-level, west bank of Glady Creek, 

 1.1 miles north of Bablin, Collins Settlement District, 1085' B., 

 Locality 106: 



Feet. 

 Stream level 



1. Sandstone, thin-bedded, hard, limestone con- 

 cretions, weathering shaly, with some thick 

 beds 13 



2. Shale, yellow, slightly sandy 4 



3. Shale, black, stained yellow, weathers gray. . . 



4. Coal 0' 4" 



Shale and bone 8 



5. Sandstone, hard, black, micaceous and calcare- 

 ous, weathers shaly and crumbles, plant and 

 marine invertebrate fossils abundant, Kana- 

 wha Black Flint 1 



6. Shale, weathers clayey, containing limestone 

 concretions in layers and bands w r hich are fos- 

 siliferous, both marine and plant fossils, Ka- 

 nawha Black Blint 11 



7. Concealed 17 



8. Sandstone, thick and thin beds, visible 20 



THE FAUNAS. 

 Conemaugh Series. 



Orlando Limestone. This fauna has not been studied in 

 the laboratory. From notes made in the field while collect- 

 ing, the following general description may.be given. Fish 

 teeth and scales are abundant and striking. They are of small 

 size and frequently fragmentary. Naiadites el on gat a Dawson 

 is found in association with pelecypoda suggestive of Edmondia, 

 which latter have been examined only superficially. Os- 

 tracoda and plant remains complete an association of forms 

 which strongly suggests a non-marine origin. The Edmondia- 

 like pelecypoda may be marine types, and if so have probably 

 been brought in by currents to a non-marine locality, or the 

 inland forms have been carried out toward the sea. 



