
Porcupine Valley defines this section of Valley County during the late 1910s, revealing a landscape of winding drainages and complex coulees. This 1918 edition, based on earlier surveys by the General Land Office and R.C. Seitz, documents the natural hydrology of the Missouri River watershed before modern water management altered the plains. The confluence of Porcupine Creek and its East Fork forms a central spine through the terrain, flanked by notable geological features like Enright Coulee and Sargent Creek. For researchers, the map provides a precise record of the public land survey system lines and early topography in a region defined by its seasonal watercourses, including Cherry Creek and Cherry Coulee, which shaped the early paths of travel and homesteading in the Montana high plains.
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2 editions found
1914 · Nashua
USGS Topo · 1:62,500
1915 · Frazer
USGS Topo · 1:62,500
1915 · Spring Creek
USGS Topo · 1:62,500
1916 · Nashua
USGS Topo · 1:62,500
1919 · Boundary
USGS Topo · 1:125,000
1943 · Glasgow
USGS Topo · 1:125,000
1954 · Glasgow
USGS Topo · 1:250,000
1957 · Glasgow
USGS Topo · 1:250,000
1958 · Glasgow
USGS Topo · 1:250,000
1958 · Whately
USGS Topo · 1:24,000