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Rock glaciers are considered reliable indicators of permafrost occurrence, developed in environments with average temperatures below -2oC. Relict rock glaciers and protalus lobes are well preserved landforms which per- mit us to deduce the environment in which they were active. This article analyzes the distribution and characteristics of 32 rock glaciers and 9 protalus lobes in the central part of Cordillera Cantabrica. Based on the shape, orientation, altitude and morphostratigraphy of rock glaciers we have established 5 different phases of rock glacier formation. Finally a chronological hypothesis is purposed, and a palaeoclimatic inference is suggested for each phase.

Glaciares rocosos del sector central de la Montaña Cantábrica : indicadores paleoambientales