
Slide Mt and the surrounding high peaks of the southern Catskills dominate this mid-century topographic study, which highlights a landscape of steep elevation and remote river valleys. The Neversink River and its various branches, including the West Branch Neversink River, carve through the terrain, providing the primary corridors for small mountain settlements like Denning and Sundown. These communities are shown at a time when local education was still decentralized, as evidenced by several one-room schoolhouses like Denning School and Red Hill School scattered across the valley floors.
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3 editions found
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 · West Shokan
USGS Topo · 1:24,000
1942 · Neversink
USGS Topo · 1:62,500
1942 · Lackawack
USGS Topo · 1:24,000