Edward L. King

TL;DR: In this article, the authors described and discussed Quaternary Fennoscandian glaciations, defined as the presence of shelf edge glaciation, an ice stream flowing out of the Norwegian Channel and most likely an ice divide over the central part of Sweden, Gulf of Bothnia, occurred for the first time in the late Cenozoic at ca. 1.1myr (the Fedje Glaciation).

TL;DR: In this paper, a conceptual model for the deglaciation of Atlantic Canada in which a role is played by ice streams is presented, where a major ice stream in the Laurentian Channel, secondary streams in the Bay of Fundy/Gulf of Maine, Trinity Trough and Notre Dame Channel, and lesser ice streams elsewhere.

TL;DR: In this paper, the authors constructed a glaciation curve for the Late Weichselian in the northern North Sea, based on new data from the Fladen, Sleipner and Troll areas, combined with earlier published results, and suggested that the maximum extent of the last glaciation along the NW European seaboard from the British Isles to northern Norway was prior to c. 22 ka BP.

TL;DR: In this article, high-resolution sleeve-gun array transects on the North Sea Fan, located at the mouth of the Norwegian Channel, reveal three dominant styles of sedimentation within a thick Quaternary sediment wedge comprising numerous sequences.

TL;DR: In this paper, short sediment cores which penetrate through the glacimarine section and into glacigenic debris flow debrites (GDFs) on the North Sea Fan are investigated.