
Summer Lake and Lake Abert dominate this high-desert landscape in south-central Oregon, illustrating a complex hydrological system of endorheic basins. The Chewaucan River flows through the extensive wetlands of the Upper Chewaucan Marsh and Lower Chewaucan Marsh before reaching the hypersaline waters of Lake Abert. The dramatic verticality of the region is defined by massive fault scarps, most notably the Abert Rim and Winter Ridge, which rise sharply above the basin floor.
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1889 · Klamath
USGS Topo · 1:250,000
1894 · Klamath
USGS Topo · 1:250,000
1955 · Crescent
USGS Topo · 1:250,000
1955 · Klamath Falls
USGS Topo · 1:250,000
1955 · Burns
USGS Topo · 1:250,000
1955 · Adel
USGS Topo · 1:250,000
1957 · Adel
USGS Topo · 1:250,000
1957 · Crescent
USGS Topo · 1:250,000
1958 · Crescent
USGS Topo · 1:250,000
1958 · Klamath Falls
USGS Topo · 1:250,000