
Claryville sits at the confluence where the West Branch Neversink River and East Branch Neversink River join to form the main stem of the Neversink River. This remote section of the Catskills is defined by high peaks and narrow hollows, straddling the border of Ulster and Sullivan counties. Significant engineering for New York City's water supply is visible underground through the paths of the West Delaware Aqueduct and East Delaware Aqueduct, which tunnel through the deep bedrock beneath the mountains.
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1900 · Phoenicia
USGS Topo · 1:62,500
1901 · Margaretville
USGS Topo · 1:62,500
1903 · Phoenicia
USGS Topo · 1:62,500
1903 · Slide Mountain
USGS Topo · 1:62,500
1904 · Margaretville
USGS Topo · 1:62,500
1905 · Slide Mountain
USGS Topo · 1:62,500
1910 · Neversink
USGS Topo · 1:62,500
1942 · Neversink
USGS Topo · 1:62,500
1942 · Lackawack
USGS Topo · 1:24,000
1943 · Peekamoose Mountain
USGS Topo · 1:31,680