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- W1990205498 abstract "Abstract The characteristics of 179 ploughing boulders and their associated ground features in the Lake District and southern Scotland are shown to be broadly similar to those reported by previous investigators from sites elsewhere in the uplands of Britain. Correlation analyses between pairs of ploughing‐boulder variables (boulder b axis, slope angle, depression length and mound height) reveal the existence of only weak morphometric relationships. Soil properties (organic matter content, grain size and index properties) lend support to the proposal that gelifluction is the principal mechanism of ploughing‐boulder movement, although the high index‐property values recorded require that correspondingly high pore‐water pressures are generated at the base of the ploughing boulders during thaw consolidation in order to initiate localised liquefaction. This can be achieved due to the greater thermal conductivity of boulders, relative to the surrounding ground, causing soil beneath boulders to freeze earlier and attain a higher water‐equivalent content than before as water is drawn to the freezing front. The potential role of soil organic matter in assisting with this process is highlighted." @default.
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- W1990205498 date "1993-04-01" @default.
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- W1990205498 title "Ploughing‐boulder characteristics and associated soil properties in the Lake District and southern Scotland" @default.
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- W1990205498 doi "https://doi.org/10.1080/00369229318736872" @default.
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