Late Holocene Activity of Sherman and Sheridan Glaciers, Prince William Sound, Alaska

• Published in: Quaternary Science Reviews
• Main Authors: Shugar, D.H., Clague, J.J., McSaveney, M.J.
• Format: Text
• Language: unknown
• Published: UW Tacoma Digital Commons 2018
• Subjects: Alaska; Climate change; Glacial geomorphology; Glaciation; Glacier-dammed lake; Holocene; Radiocarbon dating; Sedimentology; Sheridan Glacier; Sherman Glacier; Dammed Lake; Lower Lake; glacier; glaciers
• Online Access: https://digitalcommons.tacoma.uw.edu/ias_pub/903; https://doi.org/10.1016/j.quascirev.2018.07.016

Two adjacent glaciers in the Chugach Mountains of south-central Alaska have markedly different histories on decadal to perhaps centennial timescales. Sheridan Glacier has advanced and retreated hundreds of metres during the latest Holocene. Its recent fluctuations have markedly altered local base level of Sherman River, which drains Sherman Glacier and flows into Sheridan Lake. Sheridan Glacier advanced to its greatest extent during the Little Ice Age, raising base level of Sherman River and inducing aggradation there of up to 17 m of sediment. Retreat of Sheridan Glacier formed a series of lakes that have coalesced. As lower lake outlets have become available, base level of Sherman River has dropped, resulting in the evacuation of substantial volumes of sediment from Sherman River valley. In about 2000, the terminus of Sheridan Glacier began to disintegrate; retreat accelerated dramatically in 2010. By 2016, the glacier had retreated an average of 600 m from its 2010 terminus, although some areas retreated up to 1.9 km and others did not retreat at all. Meanwhile, Sherman Glacier continued a slow advance initiated by a rock avalanche that blanketed much of its ablation area in the 1964 Alaska earthquake. © 2018 Elsevier Ltd