Rock Glaciers Emerge as Critical Water Havens in Warming American Mountains
Rock glaciers in the Teton Range and other high peaks across Colorado and Utah are proving more resilient to rising temperatures than traditional exposed glaciers and snowfields. A research team, including experts from the University of Wyoming, found that these ice-filled rock formations provide a more sustained cold-water streamflow, acting as critical climate havens as iconic mountain ice fades. These hidden ice reserves are becoming essential for maintaining local ecosystems during periods of warming. While traditional glaciers are rapidly disappearing, the protective layer of rock debris helps preserve the ice beneath, ensuring a steady water supply for downstream environments that would otherwise face severe shortages.
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UW Researcher Part of Team That Finds Ice in Tetons’ Rock Glaciers Persisting Better Than on Exposed Glaciers, Snowfields
A University of Wyoming researcher was part of a team that determined ice found in rock glaciers in the Teton Range persists in a warming climate, providing a sustained cold-water streamflow, as ...
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