The Chugach Mountains dominate this high-latitude Alaskan terrain, providing the source for the Wernicke Glacier which feeds into the braided channels of the Wernicke River. This landscape is defined by the intersection of massive federal land tracts, where the southern boundary of Wrangell-Saint Elias National Park meets the northern reaches of the Chugach National Forest. The absence of any roads, settlements, or infrastructure reflects the extreme nature of the Cordoba D-1 region, where natural glacial flow and topography dictate the environment. Geologists and researchers can use this survey to examine the 21st-century extent of glacial ice and the drainage patterns that characterize this segment of the Unorganized Borough.
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This is the sole edition of this map. No revisions or reprints were ever made.
1948 · Cordova
USGS Topo · 1:250,000
1951 · Cordova
USGS Topo · 1:250,000
1959 · Cordova C-2
USGS Topo · 1:63,360
1959 · Cordova D-1
USGS Topo · 1:63,360
1959 · Cordova D-2
USGS Topo · 1:63,360
1959 · Cordova C-1
USGS Topo · 1:63,360
1959 · Cordova
USGS Topo · 1:250,000
1994 · Cordova D-2
USGS Topo · 1:63,360
2014 · Cordova C-2 NE
USGS Topo · 1:25,000
2014 · Cordova D-1 SE
USGS Topo · 1:25,000