A global compilation of glacier advances and retreats for the past two millennia grouped by
17 regions (excluding Antarctica) highlights the nature of glacier fluctuations during the late …

Surging glaciers are potential analogues for land-terminating palaeo-ice streams and
surging ice sheet lobes, and research on surge-type glaciers is important for understanding …

Strong similarities in Holocene climate reconstructions derived from multiple proxies (BSi,
TOC–total organic carbon, δ 13 C, C∕ N, MS–magnetic susceptibility, δ 15 N) preserved in …

Glaciolacustrine varves offer the potential to construct continuous, annually-resolved
chronologies for ice-sheet deglaciation, and improved understanding of glacier retreat …

A national glacier outline inventory for several different times since the end of the Little Ice
Age (LIA) in Iceland has been created with input from several research groups and …

Dykes and sills occupy Mode I (extension), Mode II (shear), or hybrid mode fractures and
most of the time transport and store magma from deep reservoirs to the surface. Subject to …

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 …

In contrast to the general trend for glaciers of the Southern Patagonia Icefield, Glaciar Pio XI
has experienced a large cumulative frontal advance since 1945. In an effort to better …

Non-linear climate change is often linked to rapid changes in ocean circulation, especially
around the North Atlantic. As the Polar Front fluctuated its latitudinal position during the …

Drangajökull is a maritime ice cap located in northwest (Vestfirðir) Iceland. Drangajökull's
evolution is therefore closely linked to atmospheric and ocean variability. In order to better …