Iceland, rising to more than 2 km above sea level, originates from the interaction of a mid-
oceanic ridge and excessive mantle upwelling. The plate boundary between the North …

INTRODUCTION The Bárdarbunga caldera volcano in central Iceland collapsed from
August 2014 to February 2015 during the largest eruption in Europe since 1784. An ice-filled …

Continuity of sediment transfer through glacial systems is essential to maintain subglacial
bedrock erosion, yet transfer at temperate glaciers with overdeepened beds, where …

Area and volume changes and the average geodetic mass balance of the non-surging outlet
glaciers of southeast Vatnajökull ice cap, Iceland, during different time periods between …

This study assesses the spatial and temporal evolution of the glacial landsystem signature at
Fjallsjökull, southeast Iceland, using (a) mapping of the glacial geomorphology and surficial …

Mineral grains from proglacial and supraglacial sedimentary settings in central south-
eastern Iceland are considered in this study and analysed with the use of scanning electron …

This paper presents detailed geomorphological and sedimentological investigations of small
recessional moraines at Fjallsjökull, an active temperate outlet of Öræfajökull, southeast …

To date, most mass balance studies in Iceland have concentrated on the three largest ice
caps. This study turns the focus toward smaller Icelandic glaciers, presenting geodetic mass …

We present an overview of glacier variations of the outlet glaciers of southeast atnajökull ice
cap, celand, during the time period∼ 1650–1900 as represented in historical archives, by …

The termini of Icelandic glaciers are highly dynamic environments. Pronounced changes in
frontal ablation in recent years have consequently changed ice dynamics. In this study, we …