Microstructures in solifluction sediments from South Wales and North Norway

Authors

  • Charles Harris Geography Section, Department of Geology, University College, Cardiff, United Kingdom

DOI:

https://doi.org/10.26485/BP/1981/28/21

Keywords:

micromorphology, dips of sand grains, mass movement

Abstract

Elements of the micromorphology of solifluction sediments at two sites in South Wales are described, particularly silt and fine sand cappings which occur on the upper surfaces of the coarse sand and gravel-sized material. These are compared with similar microstructures observed in active solifluction sediments from North Norway.

References

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Bowen, D. Q., 1970 - South-east and central South Wales. In: C. A. Lewis (ed.) - The glaciations of Wales and adjoining regions. Longman, London; p. 197-227.

FitzPatrick, E. A., 1971 - Pedology. Oliver and Boyd, Edinburgh, 306 pp.

Lewis, C. A., 1966 - The periglacial landforms of the Brecon Beacons, Wales. Unpubl. PhD thesis, Nat. Univ. Ireland.

Lewis, C. A., 1970 - The Upper Wye and Usk regions. In: C. A. Lewis (ed.) - The glaciations of Wales and adjoining regions. Longman, London; p. 147-73.

Harris, C. and Wright, M. D., 1980 - Some last glaciation drift deposits near Pontypridd, South Wales. J. Geol., 15; p. 7-20.

Harris, C., 1977 - Engineering properties, ground water conditions, and the nature of soil movement on a solifluction slope in North Norway. Q. Jour. Engng Geol. 10; p. 27-43.

Harris, C. and Ellis, S., 1980 - Micromorphology of soils in solifluction materials, Okstindan, northern Norway. Geoderma, 23; p. 11-29.

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Published

2025-11-19

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