Broken Hills anchors the southern portion of this high-desert Nevada landscape, situated within a basin defined by complex topographic shifts. The terrain is characterized by the arid drainages of Gabbs Wash and the presence of Mud Spring, a critical water source in an otherwise dry expanse. The elevation rises toward the northeast with the East Gate Range, where the map documents steep contours and prominent landforms like Grayback and Iron Rock. This area, surveyed during the early 21st century, reflects the persistent geographic isolation of Churchill County. The lack of major modern infrastructure on this 2014 sheet suggests a landscape largely unchanged in its fundamental layout, where natural features and township boundaries dictate the human understanding of the territory. Researchers can trace the drainage patterns that define the region's seasonal water movement across this part of the Great Basin.
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This is the sole edition of this map. No revisions or reprints were ever made.
1908 · Carson Sink
USGS Topo · 1:250,000
1910 · Carson Sink
USGS Topo · 1:250,000
1955 · Millett
USGS Topo · 1:250,000
1957 · Reno
USGS Topo · 1:250,000
1959 · Reno
USGS Topo · 1:250,000
1959 · Millett
USGS Topo · 1:250,000
1960 · Reno
USGS Topo · 1:250,000
1969 · Quartz Mtn
USGS Topo · 1:24,000
1969 · Quartzite Mtn NW
USGS Topo · 1:24,000
1969 · Desatoya Peak
USGS Topo · 1:24,000