PROSSER.] 
NEVERSINK RIVER SECTION. 
45 
In a quarry south of Narrowsburg, N. Y.. 
hillside, is a good exposure of the greenish 
stone. A dip of 4° to 5°, 20° to 30° ^ 
west of south, is shown in the quarry. 
In an old quarry three-fourths of a 
mile south of Narrowsburg, and in 
ledges along the western slope of the 
hill, are numerous exposures of the 
greenish-gray sandstone, with argil- 
laceous shale partings. Some of the 
finer of these shales contain frag- 
ments of Arcluvopteris. At several 
places along the ledges are good ex- 
amples of current bedding. The dip 
on the floor of the quarry is about 5 
between 30° and 40° east of north. 
An outcrop of red shale occurs a few 
rods north of the quarry. 
The section along the line of the 
Delaware River was not examined 
west of Narrowsburg, and, with the 
exception of plants, no fossils were 
found above Saw Mill Rift. The zone 
above Henryville, on the Delaware, 
Lackawanna and Western Railroad 
was not detected along the Delaware 
River. 
NEVERSINK RIVER SECTION. 
After making the section along the 
Delaware River, the strike of the 
Middle and Upper Devonian was 
followed northeast from Port Jervis 
through Orange. Sullivan, Ulster 
and Greene counties, 1ST. Y. 
No. 1478 Al.— At Rose Point, on 
the Monticello and Port Jervis Rail- 
road, 8 miles northeast of Port Jervis, 
is a good exposure of arenaceous 
shales and sandstones by the railroad, 
at the base of the hill. In the gravel 
quarry at the southern end are thin, 
black, argillaceous shales alternating 
with thin sandstones. The base of 
some of the sandstone layers is 
pebbly. This horizon is apparently 
near the dividing line of the Marcellus and 
north, on the western side of the railroad, 
and one-half mile up the 
gray, coarse-grained flag- 
- East Stroudsburq 
4-03' 
1 T a i n ilton . A little farther 
is an excellent exposure of 
