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Wishart Mitchell

Biographic Data

ID10460917
NAMEWishart Mitchell
GIVEN NAMESWishart
FAMILY NAMEMitchell
SIGNATUREMITCHELL W
AFFILIATIONSUniversity of Dundee
VERIFIEDNo
TOTAL WORKS3
TOTAL CITATIONS9
WORKS AS AUTHOR3
WORKS AS EDITOR0
FIRST PUBLICATION YEAR2007
LATEST PUBLICATION YEAR2021
H-INDEX1
  • A Detailed Record of Deglacial and Early Post-Glacial Fluvial Evolution

    Open Access•James Innes, James B Innés et al.•ARTICLE•Quaternary•2021

    The lower reaches of the River Ure, on the flanks of the Pennine Hills in northern England, contain sedimentary and erosional landforms that are a record of fluvial activity during deglaciation and valley-glacier retreat at the end of the last (Devensian) glacial period, and in the subsequent post-glacial Holocene. Terraces and channels, most of which are now relict features well above the altitude of the present river, attest to the impacts of m…

  • Little House in the Mountains? A small Mesolithic structure from the Cairngorm Mountains, Scotland

    Open Access•Graeme Warren, Shannon Fraser et al.•ARTICLE•Journal of Archaeological Science…•2018•Cited by: 9•References: 9

  • Global Change and Mountain Regions

    Open Access•W A Mitchell, Wishart Mitchell•ARTICLE•Mountain Research and Development•2007

  • Little House in the Mountains? A small Mesolithic structure from the Cairngorm Mountains, Scotland

    Open Access•Graeme Warren, Shannon Fraser et al.•ARTICLE•Journal of Archaeological Science…•2018•Cited by: 9•References: 9

  • Global Change and Mountain Regions

    Open Access•W A Mitchell, Wishart Mitchell•ARTICLE•Mountain Research and Development•2007

  • Little House in the Mountains? A small Mesolithic structure from the Cairngorm Mountains, Scotland

    Open Access•Graeme Warren, Shannon Fraser et al.•ARTICLE•Journal of Archaeological Science…•2018•Cited by: 9•References: 9

  • A Detailed Record of Deglacial and Early Post-Glacial Fluvial Evolution

    Open Access•James Innes, James B Innés et al.•ARTICLE•Quaternary•2021

    The lower reaches of the River Ure, on the flanks of the Pennine Hills in northern England, contain sedimentary and erosional landforms that are a record of fluvial activity during deglaciation and valley-glacier retreat at the end of the last (Devensian) glacial period, and in the subsequent post-glacial Holocene. Terraces and channels, most of which are now relict features well above the altitude of the present river, attest to the impacts of m…

Geography (3 works) · Geology (3 works) · Geology and Paleoclimatology Research (3 works) · Archaeology (1 work) · Archaeology and ancient environmental studies (1 work) · Assemblage (archaeology (1 work) · Climate change (1 work) · Climate change and permafrost (1 work) · Cryospheric studies and observations (1 work) · Current (fluid (1 work)

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