Coburn serves as a focal point in this central Pennsylvania landscape, where the waters of Elk Creek and Pine Creek converge into the winding Penns Creek. The terrain is defined by a series of parallel ridges and valleys, including Second Mountain and Strong Mountain, which have historically constrained travel to gaps like Greenbrier Gap and McNitt Gap. Toward the center of the sheet, the recreational infrastructure around Poe Lake and Poe Dam within Poe Valley State Park highlights the transition of this area from industrial timber or mountain farming toward conservation and public use. The presence of a CCC Camp in the south and various named hollows such as Stillhouse Hollow and Rupp Hollow point to a history of local mountain life and government-led landscape development. Numerous runs, including Swift Run and Weikert Run, drain the high ridges of Pitchpine Ridge and Spruce Mountain, creating a complex hydrological network.
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This is the sole edition of this map. No revisions or reprints were ever made.
1924 · Centre Hall
USGS Topo · 1:62,500
1924 · Lewistown
USGS Topo · 1:62,500
1925 · Mifflintown
USGS Topo · 1:48,000
1927 · Lewisburg
USGS Topo · 1:62,500
1929 · Centre Hall
USGS Topo · 1:62,500
1934 · Mifflintown
USGS Topo · 1:62,500
1937 · Mifflintown
USGS Topo · 1:62,500
1937 · Millheim
USGS Topo · 1:48,000
1941 · Millheim
USGS Topo · 1:62,500
1943 · Lewistown
USGS Topo · 1:125,000