nature & planetanalysisEos
Scientists Mapped a Hidden Glacier Using Gravity
Timpanogos Rock Glacier in Utah's mountains is buried under a layer of loose rock, and its ice is hidden inside it. Researchers mapped it using a gravimeter, which detects tiny differences in gravity caused by changes in underground density, since ice is less dense than rock. Taking 232 measurements over six trips, they used Bayesian inversion to compare thousands of simulated ice distributions with the data. The glacier holds about 1,550,000 cubic meters of ice, enough to fill Egypt's largest pyramid. Rock glaciers are an overlooked water source because they release meltwater year-round, including late in summer when other sources run low.
Ice is less dense than rock, so a column of ice exerts slightly less gravitational pull than the same column of rock. A sensitive gravimeter detects these small differences across the surface, and models of the buried ice are tested against the readings to estimate thickness.
Ground-penetrating radar often cannot see through the rock layer, so many rock glaciers have had their ice content guessed rather than measured. A gravity-based method offers a second way to measure them, and rock glaciers are not yet included in Utah's hydrological models.
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) ↗Eos (AGU) · CC BY-NC-ND 3.0
Illustrative photo · Jerzas, CC BY-SA 3.0, via Wikimedia Commons
