Javier de Marcos

TL;DR: In this paper, the authors presented cosmogenic 36 Cl surface exposure dates of four closely spaced lateral moraine ridges within the area of maximum advance of the ancient glacier, 8 km from the headwall; and two glacially polished bedrock thresholds 3 and 5 km from a headwall.

TL;DR: In this article, the authors investigated the glacial evolution on the east face of Pico de Penalara (40°51′N, 3°57′W; 2428m), the highest elevation of Sierra de Guadarrama in the center of the Iberian Peninsula, and selected 18 samples for dating with cosmogenic isotope 36Cl from moraine formations in four well-differentiated phases, as well as from a preglacial periglacial blockfield and a glacial threshold near the headwall.

TL;DR: In this article, surface exposure ages based on the in situ accumulation of 36 Cl were obtained from six moraine boulders and from three bedrock outcrops to investigate the timing of both the last local glacial maximum and the deglaciation.

TL;DR: The results of a lichenometrical and geomorphological study of one of the few remaining active snow hollows in the central region of the Iberian Peninsula are discussed in this article.

TL;DR: In this article, a model of slope dynamics for glaciated areas in the Iberian peninsula has been proposed to analyze the geomorphologic history of the Gredos Cirque.