| Summary: | The rock glaciers of the Andes of Santiago de Chile are unsuspicious, but important water resources and play a key role within the debris transport system of this semiarid high mountain area. The significance of these bodies of debris and ice within the geomorphologic and hydrologic system is shown in the case of the Casa de Piedra valley. This subcatchment of the Yeso river is situated very close to the El Yeso reservoir, which is of outstanding importance for the drinking water supply to Santiago. In the Casa de Piedra valley, recent sporadic permafrost in the form of active rock glaciers reaches down to 3000 m a.s.l. Between 3500 and 3800 m a.s.l., active rock glaciers occupy even 16% of the total debris-covered area and represent the predominant landform. Therefore discontinuous mountain permafrost has to be assumed above 3500 m a.s.l. In the study area, debris rock glaciers are observed as well as morrainic rock glaciers, the latter in lower altitudes in the neighborhood of dead ice bodies and the corresponding end morraines. The transition to the nival zone takes place around 3800 m a.s.l. at the recent equilibrium line of glaciers. In the Casa de Piedra valley, more frozen water is stored in active rock glaciers than in “true” glaciers. This situation may be assumed to be representative of many of the small catchments in the Andes of Santiago with elevations below approx. 5000 m a.s.l. Los glaciares de escombros (glaciares de roca, glaciares rocosos) de la Cordillera de Santiago constituyen un insospechado, pero importante recurso hídrico y juegan un papel clave en el sistema de transporte de sedimento de la alta montaña semiárida. Se señala la importancia de estos cuerpos de detrito y hielo en los sistemas geomorfológico e hidrológico tomando el Cajón de la Casa de Piedra como ejemplo. Esta subcuenca del río Yeso se ubica cerca del embalse El Yeso, que es de gran importancia para el abastecimiento de agua para Santiago. El permafrost insular del Cajón de la Casa de Piedra empieza a los 3000 m.s.n.m. en ...
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