
The rolling prairies of Burke County are defined by a complex network of glacial depressions and drainage basins in the late 1940s. The northern reaches are shaped by the Great Northern railroad line, which cuts across a landscape dotted with significant water features like Rennie Lake, Black Slough, and the aptly named Shallow Lake. These basins suggest the seasonal water patterns of the region, where the East Branch Short Creek provides a primary channel through the terrain. Evidence of rural community organization is prominent through the placement of local education centers, including Scandia Sch and School No 1. The southern portion of the map transitions into the Foothills, showing a distinct change in elevation and topography compared to the flatter northern sections where early 20th-century agriculture and transit took hold.
12 named features on this map. Tap any name to fly to it.
Don’t see what you’re looking for? This feature index may not catch every label — zoom into the map to look around manually.
This is the sole edition of this map. No revisions or reprints were ever made.
1947 · Flaxton
USGS Topo · 1:24,000
1948 · Flaxton
USGS Topo · 1:24,000
1948 · Beaver Lake
USGS Topo · 1:24,000
1948 · Woburn
USGS Topo · 1:24,000
1948 · Stampede
USGS Topo · 1:24,000
1949 · Portal
USGS Topo · 1:24,000
1950 · Flaxton
USGS Topo · 1:62,500
1950 · Portal
USGS Topo · 1:62,500
1953 · Williston
USGS Topo · 1:250,000
1957 · Williston
USGS Topo · 1:250,000