Boulder Edge-roundness as an Indicator of Relative Age: a Lochnagar Case Study.

A method is presented for quantifying the degree of edge roundness of large crystalline boulders using a simple instrument. The method utilises the transition due to granular disintegration from sharp to rounded boulder edges, so that the degree of edge roundness is a function of time and can be use...

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Publicado en:Scottish Geographical Journal Vol. 121; no. 2; pp. 219 - 237
Autor principal: Kirkbride, Martin P.
Formato: Artículo
Publicado: Taylor & Francis Ltd Jun2005
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Acceso en línea:Ver este registro en EBSCOhost
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        atl: Boulder Edge-roundness as an Indicator of Relative Age: a Lochnagar Case Study.
      aug:
        au: Kirkbride, Martin P.
        affil: Department of Geography, University of Dundee, Dundee DD1 4HN
      su:
        Boulders
        Geochronometry
        Geography
        Glaciers
        Moraines
        Glacial landforms
        Scotland
      sug:
        subj:
          Scotland
          Boulders
          Geochronometry
          Geography
          Glaciers
          Moraines
          Glacial landforms
      keyword:
        Caimgorms Weathering
        Dating
        Younger Dryas
      ab: A method is presented for quantifying the degree of edge roundness of large crystalline boulders using a simple instrument. The method utilises the transition due to granular disintegration from sharp to rounded boulder edges, so that the degree of edge roundness is a function of time and can be used as a relative dating tool. Edge roundness can be precisely measured in the field if strict morphological criteria are adhered to when selecting boulders to measure. Roundness can be expressed as a length measurement between fixed points on adjacent facets, as a normalised index, or as a radius of curvature. Boulder edge-roundness was employed to resolve uncertainty over the extent of the ‘Loch Lomond Stadial’ (LLS) glacier in the North-east Corrie of Lochnagar. Small but significant differences in edge roundness between two sets of moraine ridges indicate that the LLS glacier was smaller than that mapped by Sissons & Grant (1972). The moraine they ascribed to the LLS relates to an earlier advance within Late Devensian time.
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    language: English
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      custom: Copyright of Scottish Geographical Journal is the property of Taylor & Francis Ltd and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use.
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