Outputs (175)

Reconstructing the Holocene glacial history of northern Troms and western Finnmark, Arctic Norway (2024)
Journal Article
Leigh, J. R., Jones, R. S., Stokes, C. R., Evans, D. J. A., Carr, J. R., & Andreassen, L. M. (2024). Reconstructing the Holocene glacial history of northern Troms and western Finnmark, Arctic Norway. Boreas: An International Journal of Quaternary Research, https://doi.org/10.1111/bor.12668

Here we present the first Lateglacial and Holocene glacial history from Rotsunddalen, northern Troms and western Finnmark county, northern Norway, based on both relative and numerical moraine dating using Schmidt hammer, soil chronosequencing and ter... Read More about Reconstructing the Holocene glacial history of northern Troms and western Finnmark, Arctic Norway.

Dynamical response of the southwestern Laurentide Ice Sheet to rapid Bølling–Allerød warming (2024)
Journal Article
Norris, S. L., Margold, M., Evans, D. J. A., Atkinson, N., & Froese, D. G. (2024). Dynamical response of the southwestern Laurentide Ice Sheet to rapid Bølling–Allerød warming. The Cryosphere, 18(4), 1533-1559. https://doi.org/10.5194/tc-18-1533-2024

The shift in climate that occurred between the Last Glacial Maximum (LGM) and the Early Holocene (ca. 18–12 kyr BP) displayed rates of temperature increase similar to present-day warming trends. The most rapid recorded changes in temperature occurred... Read More about Dynamical response of the southwestern Laurentide Ice Sheet to rapid Bølling–Allerød warming.

The late Quaternary glacial depositional environment at Filey Bay, eastern England: Accretionary mechanisms for thick sequences of tills and stratified diamictons (2024)
Journal Article
Evans, D. J., Roberts, D. H., & Phillips, E. (2024). The late Quaternary glacial depositional environment at Filey Bay, eastern England: Accretionary mechanisms for thick sequences of tills and stratified diamictons. Proceedings of the Geologists' Association, https://doi.org/10.1016/j.pgeola.2024.01.003

Construction of the Holderness/Flamborough Head moraine belt on the East Yorkshire coast, England, records the oscillatory onshore flow of the North Sea Lobe of the British-Irish Ice Sheet from ~25.8 to ~19.7 ka BP, during which time a thick sequence... Read More about The late Quaternary glacial depositional environment at Filey Bay, eastern England: Accretionary mechanisms for thick sequences of tills and stratified diamictons.

Past glaciation of temperate‐continental mountains: A model for a debris‐charged plateau icefield/cirque glacier landsystem in the Southern Carpathians, Romania (2023)
Journal Article
Balaban, C., Roberts, D., Evans, D., & Jamieson, S. (2024). Past glaciation of temperate‐continental mountains: A model for a debris‐charged plateau icefield/cirque glacier landsystem in the Southern Carpathians, Romania. Earth Surface Processes and Landforms, 49(2), 601-621. https://doi.org/10.1002/esp.5723

Reconstructing the extent, style, timing and drivers of past mountain glaciation is crucial in both understanding past atmospheric circulation and predicting future climate change. Unlike in high‐elevation mountains situated in maritime and continent... Read More about Past glaciation of temperate‐continental mountains: A model for a debris‐charged plateau icefield/cirque glacier landsystem in the Southern Carpathians, Romania.

Late Wolstonian and Ipswichian (MIS 6/5e) sediment fill in a limestone sinkhole, Askham Fell, northern England (2023)
Journal Article
Carling, P. A., Evans, D. J. A., Abbas, M., Ou, X., & Lai, Z. (2023). Late Wolstonian and Ipswichian (MIS 6/5e) sediment fill in a limestone sinkhole, Askham Fell, northern England. Journal of Quaternary Science, https://doi.org/10.1002/jqs.3589

In 2019 a sinkhole (doline) occurred in Late Devensian till above fissured limestone in northern England. Most sediment plugging the fissure was evacuated down into a karstic drainage system. The residual sedimentary fill comprises three main lithofa... Read More about Late Wolstonian and Ipswichian (MIS 6/5e) sediment fill in a limestone sinkhole, Askham Fell, northern England.

Quantification of short‐term transformations of proglacial landforms in a temperate, debris‐charged glacial landsystem, Kvíárjökull, Iceland (2023)
Journal Article
Śledź, S., Ewertowski, M. W., & Evans, D. J. A. (2023). Quantification of short‐term transformations of proglacial landforms in a temperate, debris‐charged glacial landsystem, Kvíárjökull, Iceland. Land Degradation and Development, 34(17), 5566-5590. https://doi.org/10.1002/ldr.4865

Proglacial areas are dynamic landscapes and important indicators of geomorphic changes related to climate warming. Systematic and repeat surveys of landforms presently evolving on glacier forelands facilitate the quantification of rates of change and... Read More about Quantification of short‐term transformations of proglacial landforms in a temperate, debris‐charged glacial landsystem, Kvíárjökull, Iceland.

Remote sensing of glacier change (1965 - 2021) and identification of surge-type glaciers on Severnaya Zemlya, Russian High Arctic (2023)
Journal Article
Wytiahlowsky, H., Stokes, C. R., & Evans, D. J. (2023). Remote sensing of glacier change (1965 - 2021) and identification of surge-type glaciers on Severnaya Zemlya, Russian High Arctic. Journal of Glaciology, https://doi.org/10.1017/jog.2023.60

Glaciers in the Russian High Arctic have undergone accelerated mass loss due to atmospheric and oceanic warming in the Barents-Kara Seas region. Most studies have concentrated on the western Barents-Kara sector, despite evidence of accelerating mass... Read More about Remote sensing of glacier change (1965 - 2021) and identification of surge-type glaciers on Severnaya Zemlya, Russian High Arctic.

Active temperate glacial landsystem evolution in association with outwash head/depositional overdeepenings (2023)
Journal Article
Evans, D. J., Ewertowski, M. W., Tomczyk, A., & Chandler, B. M. (2023). Active temperate glacial landsystem evolution in association with outwash head/depositional overdeepenings. Earth Surface Processes and Landforms, 48(8), 1573-1598. https://doi.org/10.1002/esp.5569

The response of temperate glaciers to rapid climate warming is reflected in the geomorphology (landsystem) resulting from snout recession. This paper develops a locally diverse process-form model of active temperate glaciers through mapping and quant... Read More about Active temperate glacial landsystem evolution in association with outwash head/depositional overdeepenings.

Characteristics and formation of bedrock mega-grooves (BMGs) in glaciated terrain: 1 - morphometric analyses (2023)
Journal Article
Newton, M., Stokes, C. R., Roberts, D. H., & Evans, D. J. (2023). Characteristics and formation of bedrock mega-grooves (BMGs) in glaciated terrain: 1 - morphometric analyses. Geomorphology, 427, https://doi.org/10.1016/j.geomorph.2023.108619

Bedrock mega-grooves (BMGs) are subglacial landforms of erosion that occur in glaciated terrain in various geological and (palaeo)glaciological settings. Despite a significant literature on BMGs, no systematic morphometric analysis of these landforms... Read More about Characteristics and formation of bedrock mega-grooves (BMGs) in glaciated terrain: 1 - morphometric analyses.

Characteristics and formation of bedrock mega-grooves (BMGs) in glaciated terrain: 2 – conceptual models of BMG initiation (2023)
Journal Article
Evans, D. J., Newton, M., Roberts, D. H., & Stokes, C. R. (2023). Characteristics and formation of bedrock mega-grooves (BMGs) in glaciated terrain: 2 – conceptual models of BMG initiation. Geomorphology, 427, https://doi.org/10.1016/j.geomorph.2023.108620

Understanding BMG formation equates to being able to explain their initiation as well as their subsequent evolution. Several scenarios of bedrock mega-groove (BMG) initiation are proposed here, which attempt to explain how such parallel fluted terrai... Read More about Characteristics and formation of bedrock mega-grooves (BMGs) in glaciated terrain: 2 – conceptual models of BMG initiation.