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 …
R Cruz, A Martínez-Graña, JL Goy, N Nogueira - Geoheritage, 2021 - Springer
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 …
V Turu, RM Carrasco, J Pedraza, X Ros… - Quaternary …, 2018 - Elsevier
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 …
RM Carrasco, J Pedraza… - … Annaler: Series A …, 2013 - Taylor & Francis
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 …