34 EIVEKBY 



stand up above all other peaks. It takes its name 

 from a landslide which occurred many years ago 

 down its steep northern side, or down the neck of 

 the grazing steed. The mane of spruce and balsam 

 fir was stripped away for many hundred feet, leav- 

 ing a long gray streak visible from afar. 



Slide Mountain is the centre and the chief of the 

 southern Catskills. Streams flow from its base, and 

 from the base of its subordinates, to all points of the 

 compass, — the Eondout and the Neversink to the 

 south; the Beaverkill to the west; the Esopus to 

 the north; and several lesser streams to the east. 

 With its summit as the centre, a radius of ten mUes 

 would include within the circle described but very 

 little cultivated land; only a few poor, wild farms 

 in some of the numerous valleys. The soil is poor, 

 a mixture of gravel and clay, and is subject to slides. 

 It lies in the vaUeys in ridges and small hillocks, 

 as if dumped there from a huge cart. The tops of 

 the southern Catskills are all capped with a kind 

 of conglomerate, or " pudden stone," — a rock of 

 cemented quartz pebbles which underlies the coal 

 measures. This rock disintegrates under the action 

 of the elements, and the sand and gravel which re- 

 sult are carried into the valleys and make up the 

 most of the soil. From the northern Catskills, so 

 far as I know them, this rock has been swept clean. 

 Low down in the valleys the old red sandstone crops 

 out, and, as you go west into Delaware County, in 

 many places it alone remains and makes up most of 

 the soil, all the superincumbent rock having been 

 carried away. 



