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Quaternary Stratigraphy of Mount Kenya

A Reconnaissance

Bibliographic Data

ID20082892
AuthorsWilliam C Mahaney (0000-0002-5803-7397, corresponding author)
Year2026
Volume11
Pages163-170
Publication date2026-01-22
Open AccessNo
TypeCHAPTER
VenuePalaeoecology of Africa, volume 11 (SOURCE_BOOK)
PublisherCRC Press (PUBLISHER • NL)
DOI10.1201/9781003762652-19
OpenAlexW2504306366
ISBN9781003762652
LanguageEN
Citations received1

Glacial and peri giacial deposits of Quaternary age on Mount Kenya have been dated by use of several relative age-dating methods. Geologic-climatic units, consisting of moraines, rock glaciers, talus, solifluction debris, alluvial fans, and valley trains, display distinctive topographic relationships, morphology, weathering characteristics, and soil-profile development representative of the age of the unit. Five major stratigraphic entities, which developed following periods of glaciation, are recognized between 2990 and 4725 m, and assigned ages ranging from early Pleistocene to late Holocene. Soil profiles are from representative deposits comprised largely of phonolite, agglomerate, basalt and syenite, in areas of alpine and subalpine vegetation

Archaeology · Geography · Mount · Quaternary · Computer Science · Evolution and Paleontology Studies · Geology and Paleoclimatology Research · Pleistocene-Era Hominins and Archaeology · Geology · Paleontology · Stratigraphy

  • Glacial Fluctuation and Vegetation Succession on Tyndall Glacier, Mt Kenya

    Open Access•Kazuharu Mizuno•Mountain Research and Development•2005

Citations per year0.05
Citation span2005 - 2005 (1)
Highly citedNo

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