1951 Map of Bering Glacier A-2

About this map

Guyot Glacier dominates this landscape in the early 1950s, its massive icy expanse flowing toward the waters of Icy Bay. The terrain is defined by the high elevations of the Robinson Mountains and the Guyot Hills, where the ice begins to break into distinct lobes and smaller glaciers. Based on aerial photography from 1948, the topography reveals a dynamic environment where water and ice meet, seen in the movement of the Beare Glacier and the drainage of the Big River.