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478-424 ka), whilst glaciation during the subsequent Devensian Stage (MIS 2; c. ... 29-18 ka) resulted in blockage of The Wash, causing further river diversions.

Poster presentation (presented by Christine Lane). Topic: A 260 ka eruptive history for Kilimanjaro derived from Lake Challa sediments.

Action/Wong gok ka moon. Wong gok ka moon. (1988) English title: As tears go by.

20240106_Ukrains’ka. On. January 6, 2024.

2019. 'Missing Glaciations' of the Middle Pleistocene: examining controls on global glacier extent during 100 ka glacial cycles. ... Hughes, P., & Gibbard, P. 2018. Global glacier dynamics during 100 ka Pleistocene glacial cycles.

M Delarue, R Delorme, S Desrivieres, G Devenyi, MA Di Biase, R Dolan, KA Donald, G Donohoe, K Dunlop, AD Edwards, JT Elison, CT Ellis, JA Elman, L Eyler, DA Fair, ... Jia, KA Johnson, PB Jones, DT Jones, R Kahn, H Karlsson, L Karlsson, R Kawashima, EA

2. and a capacity rating of 100 kA. (These cells are designed to operate in the range 50–250 kA.).

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

Turbulent flow over unsteady monochromatic and Stokes waves has been investigated for various wave steepness ka and wave age cr/U using a Differntial Second-Moment (DSM) closure turbulence model.

In the Chew Bahir cores we are focussing on creating a high-resolution age model for the 135 ka – 125 ka interval, around the transition from MIS 6 to MIS 5, ... which will allow a test of the hypothesis that human population increase and range