Glaciers Landscapes during the Pleistocene in Trevinca Massif (Northwest Iberian Peninsula)
Augusto Pérez-Alberti and
Alejandro Gómez-Pazo ()
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Augusto Pérez-Alberti: Departament of Soil Science and Agricultural Chemistry, Faculty of Biology, Campus Vida, University of Santiago de Compostela, 15782 Santiago de Compostela, Spain
Alejandro Gómez-Pazo: Departament of Geography, Faculty of Geography and History, University of Santiago de Compostela, 15782 Santiago de Compostela, Spain
Land, 2023, vol. 12, issue 3, 1-21
Abstract:
The Trevinca Massif is in the northwestern Iberian Peninsula, on the border between Galicia and Castilla-León. Its highest elevation is 2124 m at the Trevinca peak. During the Pleistocene, an extensive icefield developed in this area, occupying the flattened surfaces in the high massif zones, and generating several glacier valleys. In the occidental sector, the identified paleoglaciers reached 187 km 2 , and glacier tongues up to 30 km in the Bibei valley, where the ice thickness came to 527 m. The glacial forms and deposits were mapped and analyzed in the entire Trevinca massif, whereas the paleoglacial reconstruction was carried out in the occidental sector (previous works analyzed the oriental sector). The reconstruction was performed by using high-resolution orthophotography, digital elevation models with a spatial resolution of 2 m, and fieldwork surveys to identify the primary forms and estimate the ice cover in the past through the GlaRe methodology. Moreover, the paleo-ELA was estimated for this sector, and the values of the ice thickness, the ELA position, and the moraines were related to other nearest sectors to analyze their similarities and differences. Three main paleoglaciers were identified in the occidental Trevinca massif (Xares, Canda, and Bibei-Barxacova). Bibei showed the highest ice thickness and ice extension, occupying more than 140 km 2 and with a thickness above 500 m some areas. Concerning the ELA, the values varied between the minimum at Xares with 1427 m and the maximum at Bibei-Barxacova with 1839 m. Four groups were identifying based on moraine ridges and were related to the different climatic phases in that sector.
Keywords: glacier reconstruction; GlaRe; ELA; Trevinca; Galicia (search for similar items in EconPapers)
JEL-codes: Q15 Q2 Q24 Q28 Q5 R14 R52 (search for similar items in EconPapers)
Date: 2023
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Persistent link: https://EconPapers.repec.org/RePEc:gam:jlands:v:12:y:2023:i:3:p:530-:d:1076817
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