
Cheney serves as the primary hub in this mid-1960s Kansas landscape, situated along the tracks of the Atchison Topeka and Santa Fe railroad. The northern portion of the map is dominated by the newly formed Cheney Reservoir, with its normal pool elevation of 1422 feet flooding the valley where the North Fork Ninnescah River once wound freely. This transformation of the terrain reflects a period of significant water management and infrastructure development in the region.
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