Hydrological and Geomorphological Significance of Rock Glaciers in the Dry Andes, Chile (278 grados–338 gradosS)

Abstract

The latitudinal-altitudinal distribution of rock glaciers in the dry Chilean Andes between 278 and 338S was analysed and their hydrological and geomorphological significance evaluated. Statistical estimation techniques were used based on digital elevation models and air photo interpretation, and sediment budget models were applied to assess surfacelowering rates. The estimated specific density of rock glaciers in the study area is 1.4 per cent, which corresponds to 147.5 km2 and a water equivalent of 2.37 km3. A comparison with glacier water equivalents derived from revised glacier inventory data shows that rock glaciers are more significant stores of frozen water than glaciers between 298 and 328S. The latitudinal-altitudinal distribution of rock glacier limits roughly follows the mean annual air 08C isotherm, but in the southern part of the study area it extends into elevations where modern regional mean annual air temperatures exceed 08C. High Andean surface-lowering rates inferred from rock glacier sediment budget models are in the order of 0.6–0.7mmyr 1, which is comparable to previous results from the dry Chilean Andes, but lower than in the more humid Andes further south.