Reversible glacial-periglacial transition in response to climate changes and paraglacial dynamics: A case study from Héðinsdalsjökull (northern Iceland)

• Published in: Geomorphology
• Main Authors: Palacios, David, Rodríguez-Mena, Manuel, Fernández-Fernández, José, Schimmelpfennig, Irene, Tanarro, Luis, Zamorano, José, Andrés, Nuria, Úbeda, Jose, Sæmundsson, Þorsteinn, Brynjólfsson, Skafti, Oliva, Marc, Aster, Team
• Other Authors: Universidad Complutense de Madrid = Complutense University of Madrid Madrid (UCM), Universidade de Lisboa = University of Lisbon (ULISBOA), Centre européen de recherche et d'enseignement des géosciences de l'environnement (CEREGE), Institut de Recherche pour le Développement (IRD)-Aix Marseille Université (AMU)-Collège de France (CdF (institution))-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE), Universidad Nacional Autónoma de México = National Autonomous University of Mexico (UNAM), University of Iceland Reykjavik, Icelandic Institute of Natural History, Universitat de Barcelona (UB), R108/20-20 (Santander Bank-UCM Projects), Nils Mobility Program (EEA GRANTS, High Mountain Physical Geography Research Group (Universidad Complutense de Madrid), NUNANTAR project (02/SAICT/2017 32002; Fundação para a Ciência e a Tecnologia, Portugal), Ramón y Cajal Program (RYC-2015-17597), Research Group ANTALP (Antarctic, Arctic, Alpine Environments; 2017-SGR-1102) funded by the Government of Catalonia.
• Format: Article in Journal/Newspaper
• Language: English
• Published: HAL CCSD 2021
• Subjects: Northern Iceland; Debris-covered glacier; Rock glacier; Debris-free glacier; Glacial evolution; Paraglacial dynamics; Climatic variability; [SDU.STU.GM]Sciences of the Universe [physics]/Earth Sciences/Geomorphology; New Rock; glacier; Iceland
• Online Access: https://hal.inrae.fr/hal-03321974; https://hal.inrae.fr/hal-03321974/document; https://hal.inrae.fr/hal-03321974/file/2021_Palacios_geomorph.pdf; https://doi.org/10.1016/j.geomorph.2021.107787

A.S.T.E.R. TEAM : Georges Aumaître, Didier Bourlès et Karim Keddadouche International audience The objective of this work is to chronologically establish the origin of the different glacial and rock glacier complex landforms deposited by Heoinsdalsjokull glacier (65 degrees 39' N, 18 degrees 55' W), in the Heoinsdalur valley (Skagafjorour fjord, Trollaskagi peninsula, central northern Iceland). Multiple methods were applied: geomorphological analysis and mapping, glacier reconstruction and equilibrium-line altitude calculation, Cosmic-Ray Exposure dating (in situ cosmogenic Cl-36), and lichenometric dating. The results reveal that a debris-free glacier receded around 6.6 +/- 0.6 ka, during the Holocene Thermal Maximum. The retreat of the glacier exposed its headwall and accelerated paraglacial dynamics. As a result, the glacier terminus evolved into a debris-covered glacier and a rock glacier at a slightly higher elevation. The front of this rock glacier stabilized shortly after it formed, although nuclide inheritance is possible, but its sector close the valley head stabilized between 1.5 and 0.6 ka. The lowest part of the debris-covered glacier (between 600 and 820 m altitude) collapsed at ca. 2.4 ka. Since then, periods of glacial advance and retreat have alternated, particularly during the Little Ice Age. The maximum advance during this phase occurred in the 15th to 17th centuries with subsequent re-advances, namely at the beginning of the 19th and 20th centuries. After a significant retreat during the first decades of the 20th century, the glacier advanced in the 1960s to 1990s, and then retreated again, in accordance with the local climatic evolution. The internal ice of both the debris-covered and the rock glacier have survived until the present day, although enhanced subsidence provides evidence of their gradual degradation. A new rock glacier developed from an ice-cored moraine from around 1940-1950 CE. Thus, the Holocene coupling between paraglacial and climatic shifts has resulted in a complex ...