Spring Gulch descends from the high ridges of the Pine Nut Mountains in this modern topographic study of eastern Douglas and western Lyon counties. The terrain is characterized by steep, undeveloped drainage systems where seasonal flows like Otts Cr carve through the high-elevation basin. This map highlights the intersection of public land survey systems and county boundaries in a landscape largely defined by its natural hydrology and high-desert relief. The lack of named settlements emphasizes the area's role as a buffer between the fertile valley bottoms and the surrounding mountain ranges, preserving the original watercourses and geographical landmarks used by early surveyors.
2 named features on this map. Tap any name to fly to it.
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This is the sole edition of this map. No revisions or reprints were ever made.
1889 · Markleeville
USGS Topo · 1:125,000
1891 · Carson
USGS Topo · 1:125,000
1891 · Markleeville
USGS Topo · 1:125,000
1891 · Wabuska
USGS Topo · 1:125,000
1891 · Wellington
USGS Topo · 1:125,000
1893 · Carson
USGS Topo · 1:125,000
1893 · Markleeville
USGS Topo · 1:125,000
1893 · Wellington
USGS Topo · 1:125,000
1894 · Wabuska
USGS Topo · 1:125,000
1948 · Walker Lake
USGS Topo · 1:250,000