nature & planetanalysisThe Conversation
You’ve never heard of these glaciers, but they’re becoming critical climate havens as America’s iconic mountain glaciers and their water fade
Rock glaciers are slow-moving masses of ice and rock debris that flow downhill like glaciers, but a thick layer of boulders covers the ice and insulates it. In the Teton Range of Wyoming, the white glaciers thinned by about 0.84 meters a year between 2014 and 2022, roughly seven times faster than in the previous half century, while rock glaciers lost only about 0.05 meters a year. The debris acts like a shade, keeping the ice colder, much as reflective blankets slow melting on ski slopes. As a result, streams fed by rock glaciers warmed about 0.6 degrees Celsius over the decade, compared with 3.4 degrees for streams fed by snowpack. There are at least 1,500 active rock glaciers across the western United States, holding roughly 2.5 cubic kilometres of water, about a fifth of the amount in mountain glaciers.
As mountain glaciers disappear, rock glaciers may become the last reliable source of cold meltwater for streams and the wildlife that depends on them, such as the meltwater stonefly. They are not a full replacement, though, and many are projected to become ice-free by the end of the century under current warming.
background
Rock glaciers are glaciers shielded from melting by a layer of non-icy rocks, allowing them to stay frozen in locations where they would otherwise melt. They consist either of angular rock debris frozen in interstitial ice, former "true" glaciers overlain by a layer of talus, or something in between. Rock glaciers are normally found at high latitudes and/or elevations, and may extend outward and downslope from talus cones, glaciers or terminal moraines of glaciers. The early textbook 'Characteristics of Existing Glaciers' refers to the varied, sometimes confusing, names given to these features; 'stone rivers', 'rock flows', 'rock streams' and 'rock glaciers', and includes a map and two photographs of 'rock streams' from the Silverton area of Colorado from the US Geological Surveyors Ernest Howe and W Cross. About the same time, Stephen Capps was surveying in the Wrangell Mountains, Alaska and reported similar landforms in the McCarthy area. Although a variety of names seemed to have been used in the USGS at this time, it is 'rock glacier' that is now generally used.
From Wikipedia: Rock glacier (CC BY-SA 4.0) ↗Illustrative photo · Jerzas, CC BY-SA 3.0, via Wikimedia Commons
