In 2015 I began studying subglacial environments on Mount Rainier, WA. I compared discharge, sediment concentration, and anions within the meltwater around the mountain, focusing on South Tahoma, Nisqually, Emmons, Winthrop and Carbon glaciers. These data provided insight about subglacial channels and hydrothermal activity in the volcano.
Mendenhall Glacier and Lake (2023)
Here, we focus on Mendenhall Glacier and Lake to assess proglacial lake characteristics. Mendenhall Glacier has been the cause of large hazardous Glacial Lake Outburst Floods (GLOFs) stemming from K’óox Ḵaadí Basin (commenly known as Suicide Basin) in 2023, 2024, and 2025. You can learn more about it on the Juneau Glacial Flood Dashboard.
Benson, V., Sutherland, D., Hood, E., Connor, C., Amundson, J. (2023), Exploring Subaqueous Glacial Environments: Water Temperature Influences on Lake-Terminating Glaciers at Mendenhall Lake, AK, Geological Society of America Abstracts,
Measuring temperature and turbidity with CTD casts on Gilkey Lake (2025)
This is a NSF funded project with Billy Armstrong (Appalachian State) and Irina Overeem (CU Boulder) focusing on three lake-terminating glaciers in the Juneau Icefield. Check out our 10 day field campaign timelapse at Gilkey Glacier.
Here we ask the questions: What are the glaciological, limnological, and sedimentary processes at ice-contact proglacial lakes? Can we quantify frontal ablation of lake-terminating glaciers?
Shake Glacier stems from the Stikine Icefield in SE Alaska. We are working with the Wrangell High School Shakes Glacier Survey Team.
We track the retreat of Shakes Glacier. We also measure the bathymetry, temperature, and turbidity of Shakes Lake.
Benson V., Sutherland, D. (2024), A Deep Dive into Hydrographic Observations of Proglacial Lakes in Southeast Alaska, AGU Fall Meeting Abstracts 2024, C51B-04.