Deglaciated areas of Kilimanjaro as a source of volcanic trace elements deposited on the ice cap during the late Holocene

Ice fields on Kilimanjaro (5895 m a.s.l., Tanzania) are retreating and 85% of the ice cover has been lost since 1912. The degree to which this recession is exceptional during the Holocene is uncertain, as age control of the entire ice stratigraphy exists only for the very shallow and very bottom ice...

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Veröffentlicht in:	Quaternary science reviews 2014-06, Vol.93, p.1-10
Hauptverfasser:	Gabrielli, P., Hardy, D.R., Kehrwald, N., Davis, M., Cozzi, G., Turetta, C., Barbante, C., Thompson, L.G.
Format:	Artikel
Sprache:	eng
Schlagworte:	Deglaciation Holocene Ice accumulation Ice cap Kilimanjaro Snow accumulation Volcanic dust
Online-Zugang:	Volltext
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