Ice-margin and meltwater dynamics during the mid-Holocene in the Kangerlussuaq area of west Greenland

Author:

Carrivick Jonathan L.1,Yde Jacob2,Russell Andrew J.3,Quincey Duncan J.1,Ingeman-Nielsen Thomas4,Mallalieu Joseph1

Affiliation:

1. School of Geography; University of Leeds; Woodhouse Lane Leeds LS2 9JT UK

2. Sogn og Fjordane University College; Sogndal NO-6851 Norway

3. School of Geography, Politics & Sociology; Newcastle University; Newcastle-upon-Tyne NE1 7RU UK

4. Arctic Technology Centre; Technical University of Denmark; Kemitorvet, Building 204 Kongens Lyngby DK-2800 Denmark

Funder

School of Geography

University of Leeds

Royal Institute of Chartered Surveyors

Publisher

Wiley

Subject

Geology,Archaeology,Ecology, Evolution, Behavior and Systematics

Reference79 articles.

1. Aaltonen , I. Douglas , B. Frape , S. Henkemans , E. Hobbs , M. Klint , K. E. Lehtinen , A. Liljedahl , L. C. Lintinen , P. Ruskeeniemi , T. 2010 The Greenland Analogue Project, Sub-project C: 2008 Field and Data Report

2. Identification of basal layer debris in ice marginal moraines, Russell Glacier, West Greenland;Adam;Quaternary Science Reviews,2003

3. Palaeohydrology of Kangerlussuaq (Søndre Strømfjord), west Greenland during the last ~8000 years;Aebly;The Holocene,2009

4. Increased aridity during the early Holocene in West Greenland inferred from stable isotopes in laminated-lake sediments;Anderson;Quaternary Science Reviews,2004

5. Till fabrics of the cross-valley moraines of north-central Baffin Island, Northwest Territories, Canada;Andrews;Geological Society of America Bulletin,1966

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