Climate sensitivity and geomorphological response of cirque glaciers from the late glacial to the Holocene
Résumé
Through a detailed geomorphological study, including thourough mapping of the geomorphic features as well as 10 Be Cosmic-Ray Exposure (CRE) dating, the geomorphological evolution of the Mulhacén cirque since the maximum ice extent of the last glacial cycle until nowadays was determined. This glacial cirque is shaped on the northern face of the Mulhacén peak (3479 m a. .l., 37 03 12 N / 3 18 41 W), Sierra Nevada, southern Spain. It includes several depositional and erosional glacial landforms
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Palacios et al QRS glacial cirques Sierra Nevada.pdf (1.92 Mo)
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