Geomorphological map** is a well-established method for examining earth surface
processes and landscape evolution in a range of environmental contexts. In glacial …

Multiple ice age cycles spanning the last three million years have fundamentally transformed
the Arctic landscape. The cadence, intensity and pattern of this glacial modification underpin …

Methane seepage from the upper continental slopes of Western Svalbard has previously
been attributed to gas hydrate dissociation induced by anthropogenic warming of ambient …

Iceland's periglacial realm is one of the most dynamic on the planet, with active
geomorphological processes and high weathering rates of young bedrock resulting in high …

The crustacean marine isopod species Haploniscus bicuspis (Sars, 1877) shows circum‐
Icelandic distribution in a wide range of environmental conditions and along well‐known …

Projections of ice sheet behavior hinge on how ice flow velocity evolves and the extent to
which marine-based grounding lines are stable. Ice flow and grounding line retreat are …

Subglacial hydrology modulates how ice sheets flow, respond to climate, and deliver
meltwater, sediment and nutrients to proglacial and marine environments. Here, we …

Abstract Eighteen samples for 36 Cl Cosmic-Ray Exposure (CRE) dating were taken from
glacially polished bedrocks, moraine boulders, fossil/active rock glaciers and debris-covered …

Biogeochemical proxy records from Icelandic lake sediment track large-scale shifts in North
Atlantic Holocene climate and highlight the impact that North Atlantic Ocean-and …

Despite warming regional conditions and our general understanding of the deglaciation, a
variety of data suggest glaciers re‐advanced on Svalbard during the Lateglacial–early …