This paper provides the first comprehensive description and interpretation of Pleistocene glacigenic deposits exposed in a cliff section at Thurstaston on the Wirral Peninsula, NW England. The section occupies a strategic position where the Irish Sea ice sheet impinged on the English Midlands and North Wales coast. The section comprises six lithofacies: diamicton, gravel, sand, laminites, mud and cobble pavements. The diamicton lithofacies can be divided into an upper, clast-poor sandy diamicton and multiple units of a lower, clast-rich sandy diamicton. Both diamictons exhibit cobble pavements. The two diamicton lithofacies are distinguished on the basis of textural composition, clast lithology, clast shape, clast surface features and clast...
This paper is a sedimentological investigation of Late Devensian glacial deposits from the Solway Lo...
The sedimentology and structural features of the Bannow Till are presented from two sites in Bannow ...
Recent publications have highlighted the over-consolidation of diamicts found in shallow sediment co...
This paper provides the first comprehensive description and interpretation of Pleistocene glacigenic...
This paper provides the first comprehensive description and interpretation of Late Devensian glacige...
The depositional processes associated with late Devensian ice in areas bordering the Irish Sea basin...
Investigation of Late Quaternary glacigenic sediments exposed in coastal sections on the Dingle Peni...
Along the south coast of Ireland, a shelly diamict facies, the Irish Sea Till, has been variously as...
Depositional conditions of a complexly deformed glacigenic sequence at Killiney Bay, on the west-cen...
The Irish Sea ice stream was the largest ice stream to drain the last British ice sheet, and around ...
The central sector of the British-Irish Ice Sheet during the last glaciation was characterised by co...
Late Devensian/Midlandian glacial deposits on the southeast Irish coast contain a record of sediment...
High‐resolution seismic and bathymetric data offshore southeast Ireland and LIDaR data in CountyWate...
This paper describes glacigenic landforms and sediments occurring within the Dungiven Basin, north-w...
Late Devensian glacial sediments and landforms of the Isle of Man record the advance and deglacial s...
This paper is a sedimentological investigation of Late Devensian glacial deposits from the Solway Lo...
The sedimentology and structural features of the Bannow Till are presented from two sites in Bannow ...
Recent publications have highlighted the over-consolidation of diamicts found in shallow sediment co...
This paper provides the first comprehensive description and interpretation of Pleistocene glacigenic...
This paper provides the first comprehensive description and interpretation of Late Devensian glacige...
The depositional processes associated with late Devensian ice in areas bordering the Irish Sea basin...
Investigation of Late Quaternary glacigenic sediments exposed in coastal sections on the Dingle Peni...
Along the south coast of Ireland, a shelly diamict facies, the Irish Sea Till, has been variously as...
Depositional conditions of a complexly deformed glacigenic sequence at Killiney Bay, on the west-cen...
The Irish Sea ice stream was the largest ice stream to drain the last British ice sheet, and around ...
The central sector of the British-Irish Ice Sheet during the last glaciation was characterised by co...
Late Devensian/Midlandian glacial deposits on the southeast Irish coast contain a record of sediment...
High‐resolution seismic and bathymetric data offshore southeast Ireland and LIDaR data in CountyWate...
This paper describes glacigenic landforms and sediments occurring within the Dungiven Basin, north-w...
Late Devensian glacial sediments and landforms of the Isle of Man record the advance and deglacial s...
This paper is a sedimentological investigation of Late Devensian glacial deposits from the Solway Lo...
The sedimentology and structural features of the Bannow Till are presented from two sites in Bannow ...
Recent publications have highlighted the over-consolidation of diamicts found in shallow sediment co...