Abstract The Cuerpo de Hombre paleoglacier occupies the upper sector of the Cuerpo de
Hombre river basin, located on the northwest slope of the Sierra de Béjar Mountains (Iberian …

Abstract The Iberian Central System (ICS) is a clue region to reveal Mediterranean/Atlantic
inferences over Iberia. We present a multidisciplinary study from western Spain conducted in …

This article identifies, describes, and characterizes, based on the analysis of 20 geosites, the
geological heritage of the Béjar and El Barco massifs. Using 22 characteristics, and …

The study of the Peña Negra paleoglacier during the Last Glacial Maximum reveals its
sensitivity to paleoclimatic variations. The evolutionary phases of the paleoglacier are …

A paleoglacier reconstruction during the Last Glacial Maximum (LGM) is presented for a
high mountain area of La Covacha massif in Sierra de Gredos (Iberian Central System) in …

Glaciers in mountainous landscapes reshape the topography by forming wide-open valleys.
Besides valley excavation, the amount of available glaciogenic sediment stored after …

The Navamuño peatbog (Sierra de Béjar, western Spain) is a∼ 14 ha pseudo-endorheic
depression with boundaries defined by a lateral moraine of the Cuerpo de Hombre …

During the deglaciation stages of the last glacial period a rock avalanche took place on the
glacier that occupied the upper sector of the uerpo de ombre alley (ierra de éjar). The …

It is well known that glacial erosion modifies the topography by increasing the local relief,
producing cirques and U-shaped valleys. During the Last Glacial Maximum (LGM) the …

Descripción: Se trata de una de las zonas más visitada por la población en general, ya que
la laguna de Peñalara es un lugar emblemático y muy accesible desde Madrid. Desde el …