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In the Vale of York, ice extended no further south than the Escrick moraine ridge, attaining its maximum extent between 23.50 and 21.60 ka. ... The dynamics of the eastern sector of the BIIS between 41.00 to 15.80 ka were strongly coupled with movements

Orbital obliquity at 41 ka cycles which had dominated the earlier part of the Pleistocene was superceded progressively about a million years ago by a 100 ka rhythm of orbital eccentricity,

Indeed the change from the 40 ka to the 100 ka cyclicity appears to be accompanied by an important increase in the intensity of supply of sedimentary detritus and thus a

cover. We found that a gradual removal of terrestrial sediment from the Northern Hemisphere continent by glacial processes is sufficient to explain transition from 40-ka to 100-ka worlds around

28 Apr 2003: Orbital obliquity at 41 ka cycles which haddominated the earlier part of the Pleistocene wassuperceded progressively about a million years ago by a100 ka rhythm of climate change and increased-amplitudeclimatic ... The first talk, by Mark Maslin (UCL,

13 Jan 2020: Termination I - 14 ka. Termination IV - 337 ka. Termination V - 424 ka 11. ... 9e. 7e7a. 19. 15a. 103. 63. 9a. 5. 15e. 4. Termination VI - 533 ka.

21-15 ka BP) can be assessed for a specific moment in time (e.g. ... Timeframes shown: 10,000 - 7,000 - 6,500 - 6,000 - 5,500 ka BP.

explaining the strong 100,000-year ice age cycles at the end of the Middle Pleistocene transition (700 ka) and, c) the interactions between millennial and orbital climate variability as the ... 220 ka. The sediment profile is marked by alternations of

fills. The Nene and Welland rivers were both active throughout the Devensian Stage, with lower-energy deposition in the Early Devensian Substage (50-115 ka) than in the later Middle and ... An significant hiatus in sedimentation during the Late Devensian

In contrast, a somewhat different regime seems to have occurred during the warm phase of the Late-glacial (Windermere) Interstadial (13-11 Ka).