The Halls Mills Covered Bridge anchors the southern portion of this landscape, where the Neversink River begins its journey through the Catskills. This 2019 survey captures the convergence of the West Branch Neversink River and the East Branch Neversink River at the hamlet of Claryville. The terrain is defined by high peaks such as Blue Hill and Denman Mtn, which separate narrow valleys where settlements like Ladleton and Frost Valley are situated along winding mountain roads. A complex network of drainage basins is visible, including Willowemoc Cr in the west and Sugarloaf Brook in the southeast. These waterways and the historic road network, including Co Rd 47 and Peekamose Hollow Rd, illustrate the long-standing geographic isolation and specialized mountain economy of the Ulster and Sullivan county border region.
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This is the sole edition of this map. No revisions or reprints were ever made.
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