Chalk Bank Landing sits at the edge of a highly modified hydrologic landscape along the California-Oregon border. This area is defined by the remnants of Lower Klamath Lake, which is crisscrossed by an extensive network of reclamation infrastructure, most notably the Klamath Strait Drain. The map reveals the intricate grid of agricultural land and water management that has reshaped the basin, including White Lake and Fairchild Island. To the south, the terrain rises into the Modoc National Forest, where the flat reclaimed beds give way to features like Big Tableland and Sardine Flat. Coyote Point and Glaser Lakes mark the western transition from the basin floor toward higher ground, while Willow Creek provides a natural contrast to the engineered drainage canals that dominate the northern flats.
20 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.
1886 · Modoc Lava Bed
USGS Topo · 1:250,000
1889 · Klamath
USGS Topo · 1:250,000
1892 · Modoc Lava-Bed
USGS Topo · 1:250,000
1894 · Klamath
USGS Topo · 1:250,000
1950 · Mt. Dome
USGS Topo · 1:62,500
1950 · Dorris
USGS Topo · 1:62,500
1954 · Alturas
USGS Topo · 1:250,000
1955 · Klamath Falls
USGS Topo · 1:250,000
1957 · Merrill
USGS Topo · 1:62,500
1957 · Klamath Falls
USGS Topo · 1:62,500