] SECTIONS NEAR MILFORD. 33 
Fauna of No. 1476 Dl. 
Modiomorptia my tiloirtes ( Con. ) Hall (rr) 
( ?) Glossites cf. subteimis Hall (rr) 
Nnculites triqueter (Con.) Hall (rr) 
Tellinopsis subemarginata (Con.) Hall (rr) 
Paracyclas lirata (Con.) Hall (r) 
Orthis vanuxeini Hall . (rr) 
Rhynchonella cf. congregata (Con.) Hall (r) 
Chonetes setigera Hall (rr) 
Tropidoleptus carinatus (Con.) Hall (rr) 
One specimen is a young shell. 
Coleolus tenuicinctum Hall (rr) 
Macrodon hamiltoni;e Hall (?) (rr) 
Nucula corbuliformis Hall (rr) 
Modiomorpha cf. small specimens of M. alta (Con.) Hall, possibly young 
shells of M. mytiloides ( Con. ) Hall (rr) 
Orthoceras crotalum Hall ... (rr) 
Actinopteria boydi (Con.) Hall (c) 
(?) Grammysia sp., possibly young of G. constricta Hall (rr) 
Pleurotomaria sp (rr) 
SECTIONS NEAR MILFORD, PIKE COUNTY, PA. 
Iii the bed of Kaymondskill Creek, 3 miles southwest of Milford, 
above the "Bridal Veil Falls" and below the High Falls, are coarse 
arenaceous Hamilton shales, some layers of which approach thin 
sandstones. The rocks have a dip of 10°, 20°, to 25° west of north 
and a cleavage of 45° to 50° to the southeast. The coral bed, "Tully 
limestone horizon," is stated- to occur at the head of Raymondskill 
Falls, 1 but it seems to me that it must be farther up the creek, for the 
coarse, arenaceous shales and thin sandstones continue up the creek 
some distance above the falls, and in other localities the "coral bed" 
is near their top. The steep walls of the canyon and the high water 
did not permit a sufficiently careful examination to determine this 
point. 
After crossing the bridge one-fourth of a mile above the "High 
Falls," at the summit of the first rise is an exposure of more argilla- 
ceous shales, resembling the Genesee shale of Prof. White. The dix> is 
16°+ about 25° west of north. 
At the next small rise in the road, going west, No. 147G Go, is an 
outcrop of rather coarse arenaceous shale in which was a beautiful 
specimen of Spirophyton velum (Van.) Hall. This locality is near the 
Lareaux house and old brewery, and not far east of the Lareaux 
schoolhouse mentioned by Prof. White. 2 
No. 1476 Gl. — On the Ghucktownroad, about 3 miles from the Dela- 
ware River and just west of the house of Mrs. D. M. Case, is a rather 
prominent ledge of greenish gray coarse grained sandstone. This is 
stated by Prof. White to be "the base of the Gatskill " (probably 
i G 6 , p. 109. 2 G ,; , p. 202. 
Bull. 120 3 
