Knik Glacier dominates the southeastern portion of this glacial valley landscape, serving as the source for several significant alpine waterways. The drainage network is clearly defined by the Glacier Fork Knik River and the Lake Fork Knik River, which converge and flow toward the broader Knik River. A distinctive topographical narrowing known as The Gorge marks a transition point along the water's path through the high-elevation terrain. This 2013 survey illustrates the intricate relationship between the ice field and the resulting river systems, including smaller tributaries like Fall Cr and Metal Cr that feed into the primary basins. The map also delineates the administrative boundary between Matanuska-Susitna and Anchorage, showing how these jurisdictions meet amidst the peaks and glacial outflows.
14 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.
1951 · Anchorage
USGS Topo · 1:250,000
1951 · Anchorage C-5
USGS Topo · 1:63,360
1952 · Anchorage C-5
USGS Topo · 1:63,360
1960 · Anchorage C-5
USGS Topo · 1:63,360
1960 · Anchorage B-5
USGS Topo · 1:63,360
1960 · Anchorage B-4
USGS Topo · 1:63,360
1960 · Anchorage C-4
USGS Topo · 1:63,360
1962 · Anchorage
USGS Topo · 1:250,000
1979 · Anchorage
USGS Topo · 1:250,000
1994 · Anchorage B-4
USGS Topo · 1:63,360