
The East Branch Delaware River carves a central path through the high peaks of the western Catskills, anchoring a network of narrow mountain valleys. In the early 20th century, the Delaware and Ulster Railroad served as the vital artery for this region, connecting the valley settlements of Arkville, Fleischmanns, and Halcottsville. The map reveals a landscape defined by its hollows—such as Weaver Hollow and Canada Hollow—where small farming communities and timber interests concentrated. Near the confluence of the river and the Bush Kill, the village of Margaretville emerges as a principal hub of activity. Further south, the terrain becomes increasingly steep and remote, marked by the prominent Dry Brook Ridge and the heights of Balsam Roundtop. This period represents the era before the large-scale reservoir projects transformed the Delaware watershed, showing original riverine settlements like Arena and Dunraven in their earlier topographical context.
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7 editions found
1900 · Phoenicia
USGS Topo · 1:62,500
1901 · Margaretville
USGS Topo · 1:62,500
1901 · Gilboa
USGS Topo · 1:62,500
1903 · Gilboa
USGS Topo · 1:62,500
1903 · Phoenicia
USGS Topo · 1:62,500
1903 · Slide Mountain
USGS Topo · 1:62,500
1904 · Hobart
USGS Topo · 1:62,500
1904 · Margaretville
USGS Topo · 1:62,500
1905 · Slide Mountain
USGS Topo · 1:62,500
1909 · Delhi
USGS Topo · 1:62,500