Exposure dating has substantially improved our knowledge about glacier advances during the Younger Dryas (YD) and the early Holocene. The glacier development after the Last Glacial Maximum (LGM) and the timing of morphologically evidenced, earlier Lateglacial re-advances is, however, still widely unknown. In this study we used ¹⁰Be surface exposure and radiocarbon dating to address these phases and corresponding landforms in the catchment of the former Reussgletscher (central Swiss Alps). We obtained clear indication for moraine deposition prior to the YD. The oldest samples predate the Bølling–Allerød interstadial (>14.6 ka). Morphostratigraphically even older lateral moraines, probably corresponding to terminal positions in the Lake Lucer...
The combined Rhone and Aare Glaciers presumably reached their last glacial maximum (LGM) extent on t...
Reconstruction of past glacier fluctuations is an important step towards the comprehension of glacie...
A complete sequence of glacial deposits and moraines within the same valley system in the Maritime ...
Exposure dating has substantially improved our knowledge about glacier advances during the Younger D...
We used cosmogenic 10Be and 36Cl to establish the timing of the onset of deglaciation after the Last...
The Göschenertal (Göschenen valley) is the type locality of the so‐called Göschenen Cold Phases I (~...
Detailed knowledge of Holocene climate and glaciers dynamics is essential for sustainable developmen...
We reconstruct the timing of ice flow reconfiguration and deglaciation of the Central Alpine Gotthar...
To exploit the potential of rock glaciers as indicators of past climate condition it is first necess...
To develop a more precise understanding of Alpine glacier fluctuations during the Holocene, the glac...
This study focuses on an Egesen-stadial moraine located at 1906–1920 m asl in the NE Maritime Alps, ...
The combined Rhone and Aare Glaciers presumably reached their last glacial maximum (LGM) extent on t...
Reconstruction of past glacier fluctuations is an important step towards the comprehension of glacie...
A complete sequence of glacial deposits and moraines within the same valley system in the Maritime ...
Exposure dating has substantially improved our knowledge about glacier advances during the Younger D...
We used cosmogenic 10Be and 36Cl to establish the timing of the onset of deglaciation after the Last...
The Göschenertal (Göschenen valley) is the type locality of the so‐called Göschenen Cold Phases I (~...
Detailed knowledge of Holocene climate and glaciers dynamics is essential for sustainable developmen...
We reconstruct the timing of ice flow reconfiguration and deglaciation of the Central Alpine Gotthar...
To exploit the potential of rock glaciers as indicators of past climate condition it is first necess...
To develop a more precise understanding of Alpine glacier fluctuations during the Holocene, the glac...
This study focuses on an Egesen-stadial moraine located at 1906–1920 m asl in the NE Maritime Alps, ...
The combined Rhone and Aare Glaciers presumably reached their last glacial maximum (LGM) extent on t...
Reconstruction of past glacier fluctuations is an important step towards the comprehension of glacie...
A complete sequence of glacial deposits and moraines within the same valley system in the Maritime ...