66 PENNSYLVANIA AND NEW YORK DEVONIAN. [bull. 120. 
quite similar to this specimen, but the base is entirely different from 
the Lanesville specimen since it has a broad root with several stalks 
rising from it. Nathorst has figured and described somewhat similar 
markings as the trails of worms. 1 
No. 1058 El.— The North quarry, H miles up the Hollow Tree 
Branch, north of Lanesville, is on the western side of the creek, and 
shows mainly pink sandstone with a little red shale and gray sandstone 
on top. No fossils were found, and the quarry is some 300 feet above 
the railroad, or, approximately, 1,050 feet A. T. About 150 feet higher 
on the mountain side is another small quarry of pink sandstone with a 
little bluish shale. 
No. 1491 Al. — Simpson quarry, just above Edgewood, is mainly the 
pink sandstone. This quarry is 3 miles northeast of Lanesville, about 
470 feet higher, or with an approximate elevation of 1,820 feet. In the 
bed of Stony Clove Creek, just above Edgewood railroad station, is a 
fine exposure of the red shale. 
No, 1494 B. — In the " notch" on the eastern side of the railroad, about 
one-fourth of a mile south of the Stony Clove station, is the Eldredge 
quarry. In the upper part is very dark bluish-gray sandstone, and in 
the lower, the pink sandstone. The sandstone is coarse grained, very 
compact, and contains no fossils. Loose blocks of conglomerate with 
quartz pebbles are present. This quarry is on the western side of 
Plateau Mountain, and nearly 130 feet higher than the Stony Clove 
switch, which is 2,071 feet A. T., 2 making the approximate altitude of 
the quarry 2,200 feet A. T. 
No. 1495 A.— HAINES FALLS, GREENE COUNTY. 
In Twilight Park, near the foot of Bound Top Mountain, on the west- 
ern side of Kaater skill Creek and Haines Falls, is a prominent ledge 
of conglomerate (1495 A2). Some.of the pebbles are very large and the 
stratum forms a conspicuous feature of the mountain side, being called 
locally the " pudding stone." This massive conglomerate is well up in 
the Catskill stage, and is lithologically about the same as the conglom- 
erate noted by Mather on South Mountain, between Hotel Kaaterskill 
and the Catskill Mountain House, 3 which he referred to the " lower 
grits of the Coal formation, n evidently regarding them as above the 
Catskill division. This ledge is by the barometer 110 feet above 
Haines Falls which, according to Guyot, are 1,890 feet, A. T., 1 making 
its elevation approximately 2,000 feet A. T. 
In the creek, under the bridge above the Haines Falls (1495 Al), are 
red sandstones. Below, at the brink of the falls and in the side of the 
'See Om nagra form. Vaxtfoss.. PI. 18, fig. 11, 12, in Ofversigt af Kongl. Vetenskaps-Akad. Fork., 
Stockholm, 1873. 
- Van Loan's Catskill Mountain Guide, 1890, p. 78. Guyot seems to have been in error in assigning 
this locality an elevation of 1,700 feet. (Am. Jour, Sci., 3d ser., Vol. XIX, p. 435). 
3 Geol. X. Y., Ft. i, 1843, p. 303. 
4 Am. Jour. Sci., 3d. ser.,Vol. XIX, p. 449. 
