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Palaeogeography of the Gezira and of the lower Blue and White Nile valleys.

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dc.contributor.authorAdamson, D. A.en
dc.contributor.authorWilliams, M. A.J.en
dc.contributor.authorGillespie, R.en
dc.date.accessioned2025-03-21T18:24:12Z
dc.date.available2025-03-21T18:24:12Z
dc.date.issued1982en
dc.description.abstractDescribes the evolution of the Blue Nile in the Late Pleistocene and Holocene. Chronological evidence is provided by volcanic ashes and dates on carbonates and fossil shells. Paleochannels were formed during a wet phase about 11-12 000 yr ago. The second section describes the evolution of the White Nile which shows a similar phase of flooding in the terminal Pleistocene and the early Holocene. Sections dug at Jebel Tomat and Shabona are used to reconstruct the Holocene environment. The chronology is summarised in the conclusion. -K.Claytonen
dc.description.statustrueen
dc.format.extent55en
dc.identifier.otherScopus:0020462860en
dc.identifier.urihttps://dspace-test.anu.edu.au/handle/1885/733727342
dc.identifier.urlhttp://www.scopus.com/inward/record.url?scp=0020462860&partnerID=8YFLogxKen
dc.language.isoEnglishen
dc.sourceUnknown Journalen
dc.titlePalaeogeography of the Gezira and of the lower Blue and White Nile valleys.en
dc.typeArticleen
local.bibliographicCitation.lastpage219en
local.bibliographicCitation.startpage165en
local.contributor.affiliationAdamson, D. A.; Macquarie Universityen
local.contributor.affiliationWilliams, M. A.J.; Macquarie Universityen
local.contributor.affiliationGillespie, R.; Macquarie Universityen
local.identifier.pure064ea0a6-2136-402a-b82f-7f9b913ba851en
local.type.statusPublisheden

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