34 PENNSYLVANIA AND NEW YOKE DEVONIAN. [bull. 120. 
Starucca sandstone, which was later called Upper Chemung), "and a 
few feet below it the bluish-gray fossiliferous shales and sandstones of 
the Chemung make their appearance." 1 
No. 1476 Grl\ — The bluish, arenaceous shales below the coarse sand- 
stone contain a moderate fauna, and specimens were collected from 
small ledges on the low hill north of Mrs. Case's, as well as from a similar 
hill on the opposite side of the road, southeast of the house. No con- 
siderable number of fossils were obtained, but several specimeus of a 
few species such as were usually seen just before the driving out of the 
fauna by the invasion of the gray sandstones and later red shale. A 
few good specimens were obtained from some riprap in the road, the exact 
locality of which was not learned, except that they came from one of 
the fields in that vicinity. 
Fauna of No. 1476 G2. 
Orthonota ( ?) parvula Hall (aa) 
Many of the specimens are quite small, as well as those of other species, 
showing that the conditions were becoming unfavorable for marine life. 
This species is very abundant on one slab from this locality. 
Nuculitcs oblongatns Con (c) 
Paheoneilo emarginata (Con.) Hall .. (rr) 
Nuculitcs cuneiformis Con (c) 
Nucula corbuliformis Hall (aa) 
Modiomorpha subalata (Con.) Hall var. chemungensis Hall (?) (rr) 
Actinopteria boydi (Con.) Hall (r) 
Leptodesma rogersi Hall or L. sociale Hall ( rr) 
Specimen broken and these two species are apparently closely related. 
Rhynchouella sp (rr) 
Specimen broken, but apparently of the R. eximia Hall type. 
Spirifera sp ( rr) 
Section of the Sawkill Creek, Between Milfohd and Dingman Townships, 
Neah Milford. 
No. 1476 Fl.— Bridal Yeil Cascades in Sawkill Creek below the rustic 
bridge. The exposures consist of bluish, argillaceous, and coarse arena- 
ceous shales, running into thin sandstones, in which specimens of 
Tropidoleptus camiatus (Con.) Hall are abundant. The dip at the foot 
of the Bridal Veil, and also on the creek below the bridge, is about 14°. 
Fauna of No. 1476 Fl. 
Tropidoleptus carinatus (Con.) Hall (a) 
Paheoneilo emarginata (Con.) Hall ( ?) (rr) 
Nuculitcs triqueter Con (rr) 
Phacops rana (Green) Hall ( rr ) 
No. 147G F2.— Above the Sawkill Fails and at nearly the last bed 
rock in the creek are bluish, rather coarse argillaceous shales, which 
contain many small Lamellibranchs of the Hamilton fauna. On the 
western side of the creek is a slight excavation, evidently the begin- 
ning of a quarry, in which some bluish sandstone appears, with bluish 
shales below. Tbe locality is about one-fourth of a mile below the pike 
' (l fi , p. 204. In reference to tlie correlation of the Starucca sandstone see Prosser in Am. Jour. 
Sci., Ctl acr., Vol. XLIV, pp. 218, 219. 
