From the Proterozoic to the Quaternary, the evolution of the Earth was characterised by
recurrent periods of glaciation. However, the margins of many ancient ice-sheets are poorly …

Upper‐flow‐regime bedforms, including upper‐stage‐plane beds, antidunes, chutes‐and‐
pools and cyclic steps, are ubiquitous in glacigenic depositional environments characterized …

Abstract The Oak Ridges Moraine in southern Ontario is a polygenetic moraine constructed
of a number of coalesced deposits of glacifluvial and glacilacustrine origin. A detailed study …

After the LGM, the Eastern Sector of the LIS evolved from a single centre into peripheral
connected or detached ice masses, with ice streams in the St. Lawrence Corridor and …

This paper examines a glacial diamictite-bearing succession from the upper Itararé Group
(Taciba Formation) in eastern Paraná Basin, Brazil. The object of study provides the …

OWCZAREK Z., STACHOWSKA-KAMIŃSKA Z., KOSTRZEWA O., SZCZYPIŃSKA M., 2024.
Progress in Arctic coastal geomorphological research in times of rapid climate warming …

A systematic approach was used for the interpretation of the electrical resistivity tomography
carried out on two permafrost mounds at Umiujaq in Nunavik, Canada, to assess their …

The complete life cycle of a permafrost mound is reconstructed from its growth until its
degradation. The study site is a lithalsa, which is the subject of a long-term monitoring that …

Sediments deposited by glacial meltwaters (for example, ice‐contact delta deposits) form
permeable packages in the subsurface that can act as reservoirs for both water and …

Deglacial sequences typically include backstepping grounding zone wedges and prevailing
glaciomarine depositional facies. However, in coastal domains, deglacial sequences are …