Abstract Little Ice Age lateral moraines represent one of the most important sediment
storages and dynamic areas in glacier forelands. Following glacier retreat, simultaneous …

Ice-cored lateral–frontal moraines are common at the margins of receding high-Arctic valley
glaciers, but the preservation potential of these features within the landform record is …

The arctic environment is changing: air temperatures, major river discharges and open water
season length have increased, and storm intensities and tracks are changing. Thirteen …

Svalbard is a heavily glacier-covered archipelago in the Arctic. Dickson Land (DL), in the
central part of the largest island, Spitsbergen, is relatively arid and, as a result, glaciers there …

Extensive ice-cored moraine complexes are common elements, marking the last advance of
many Svalbard glaciers. Sediment gravity flows are among the most dynamic processes …

The assessment of multidecadal scale change in a polythermal glacial landsystem in the
high Arctic is facilitated by a quantitative approach that utilises time series of aerial …

ABSTRACT A 1: 4000 scale map of the terrestrial margins of the foreland of
Nordenskiöldbreen depicts a polythermal glacial landsystem containing a record of the …

Ice-cored moraine complexes are prominent landforms characteristic of many polythermal
glacial landsystems on Svalbard, usually marking their maximum Little Ice Age extent …

Melting Svalbard glaciers have been recognized as an early indicator of climate change.
Large parts of Svalbard remain insufficiently investigated, including Dickson Land, in the …

ABSTRACT A 1: 850 detailed map of the geomorphology of the Dynamisk Creek alluvial fan
on Svalbard was produced based on very high-resolution data collected using an …