The Humboldt River terminates in this arid landscape of Churchill County, forming the distinctive hydrological terminal basin known as the Humboldt Sink. This 2011 survey documents a region where the waters of the Humboldt Lake fluctuate across a low-lying desert floor, creating an ever-shifting shoreline depending on seasonal inflow. The topography is dominated by the vast, sandy reaches of the Lahontan Basin, where the endorheic drainage system of northern Nevada finally concludes. Without any established towns or settlements on this quadrangle, the focus remains on the stark intersection of water and desert, showing the various braided channels and intermittent marshlands that define this terminal point of one of the West's most significant rivers.
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1908 · Carson Sink
USGS Topo · 1:250,000
1910 · Carson Sink
USGS Topo · 1:250,000
1931 · Lovelock
USGS Topo · 1:250,000
1935 · Lovelock
USGS Topo · 1:250,000
1951 · Carson Sink
USGS Topo · 1:62,500
1955 · Lovelock
USGS Topo · 1:250,000
1956 · Toulon
USGS Topo · 1:62,500
1956 · Lovelock
USGS Topo · 1:62,500
1957 · Reno
USGS Topo · 1:250,000
1959 · Lovelock
USGS Topo · 1:250,000