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Ostrich feather from the crown of Cetshwayo ka Mpande (ca 1826–1884), King of the Zulu, and Treaty of Ulundi pen.

Principal and Recent Publications. Heydon, R., Akiwenzie, E., Cooper, E., Ghannoum, H., Havord-Wier, D., Johns, B., MacAlpine, KA., McKee, L., Nagle, J., Neeganagwedgin, E., Pawlick-Potts, D., Poczobut, S., Ruthes

Room 009, Cancer Research UK Cambridge Institute, Li Ka Shing Centre, Robinson Way, Cambridge CB2 0RE. ... Visitor information. Location: Cancer Research UK Cambridge Institute University of Cambridge Li Ka Shing Centre Robinson Way Cambridge CB2 0RE.

Japanese Works : Heibun jibiki shūi : 'ka' kara 'kaz' made.

You are not currently logged in. Room 313, Cancer Research UK Cambridge Institute, Li Ka Shing Centre, Robinson Way, Cambridge CB2 0RE. ... Visitor information. Location: Room 313, Cancer Research UK Cambridge Institute University of Cambridge Li Ka

Choi, J. (2019). Abrupt Holocene climate events of coastal East Asia including the 8.2 ka, 4.2 ka, and 2.8 ka coolings, and the societal responses on the Korean ... Jin, Q. (2018). The 8.2 ka cooling event in coastal East Asia: High-resolution pollen

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

Journal: Neuroimage. E-pub date: 15 Apr 2023. Authors: S Lugtmeijer, L Geerligs, KA Tsvetanov, DJ Mitchell, Cam-Can, KL Campbell. ... Journal: J Neurol. E-pub date: 31 Aug 2020. Authors: AG Murley, PS Jones, I Coyle Gilchrist, L Bowns, J Wiggins, KA

20240210_Zakarpats’ka. On. February 10, 2024.

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

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.

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.

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

20240224_Slavins’ka. On. February 24, 2024.

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

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.

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