Filling a major gap in the LGM chronology of the Eastern Alps: New evidence from Enns and Mur glaciers (Austria)

During the Last Glacial Maximum (LGM), large glacier tongues reached far into the alpine foreland and formed piedmont lobes. Common deposits are moraine “amphitheatres” directly connected to glaciofluvial deposits, which are both suitable for (direct) age dating. Over much of the Alpine realm, great efforts have been made to constrain the chronology of the LGM, yet in the eastern part, significant gaps exist, and absolute dates for glacial features are missing. Due to a gradual eastward change in terms of precipitation, moisture, and topography, glaciers did not advance as far in the eastern Alps and terminated in narrow inneralpine valleys. Evidence of their extent is therefore sparse and their deposits were mostly cannibalised by later erosional and depositional processes. Nevertheless, remnant terminal moraines from the Enns and Mur glaciers (mainly fed by the Niedere Tauern in the Central Alps) remain. These deposits contain blocks that can be dated with cosmogenic beryllium and aluminium surface exposure dating.

For cosmogenic dating, two sites were investigated as follows. The Enns glacier developed north of the Niedere Tauern mountain range and one of its terminal tongues ended at Buchauer Saddle, where a terminal moraine complex is preserved. The moraine ridges reach a few tens of meters in height and contain mostly blocks of carbonate, with some quartz-containing blocks also present. All dated blocks are Palaeozoic quartz conglomerates/breccias, which crop out roughly 25 km upvalley.

The ice masses of the Mur glacier accumulated south of the Niedere Tauern mountain range in the Mur valley. The glacier was divided into several tongues, one of them terminating near Pöls, where the most prominent moraine of the Mur glacier is preserved. It consists of a diamicton with a silty to clayey matrix and few components of pegmatite gneiss, amphibolite and other crystalline rocks. Datable blocks consist of coarse-grained pegmatite gneiss.

Based on mapping relationships, the spatial context of the both moraine complexes suggest their deposition during the LGM. In this contribution, we will explore this hypothesis so far developed on the basis of field relations by presenting preliminary exposure ages of these landforms.