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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.

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.

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

Kyiv's Monastery of the Caves (Pechers'ka Lavra) and Saint Sophia.

Search site. Museum of Classical Archaeology Databases. A to Z of Sherds. Search Sherds. Number. Number. Site. Date. Ware. Material/Function. References/Other information. Pages. …. 141. …. Museum of Classical Archaeology, Cambridge. Every cast

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

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

Diffractometer experiment with lithium fluoride crystal. Using the 2θ value observed at a peak of intensity, the known wavelength λ for Cu Ka, = 1.54Å and the Bragg equation, a value

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