Boulder clay

WWII pillbox on eroding Boulder Clay, Filey Bay, North Yorkshire.
Boulder clay cliffs in Gwynedd with Dinas Dinlle in the background

Boulder clay is an unsorted agglomeration of clastic sediment that is unstratified and structureless and contains gravel of various sizes, shapes, and compositions distributed at random in a fine-grained matrix. The fine-grained matrix consists of stiff, hard, pulverized clay or rock flour. Boulder clay is also known as drift clay; till; unstratified drift, Geschiebelehm (German); argile á blocaux (French); and keileem (Dutch).[1][2]

The term boulder clay is infrequently used for gravelly sedimentary deposits of nonglacial origin. These deposits include submarine slump and slide deposits along continental margins,[3] lacustrine debris flow deposits consisting of pebbly mudstones,[4] and coarse, poorly sorted, cobbly diamictons associated with the Guangxi karst, China.[5]

  1. ^ Charlesworth, J. K., 1957. Chap 18, Boulder Clay. In The Quaternary Era, with Special Reference to its Glaciation. v. 1, London, United Kingdom, Edward Arnold, p. 376-388.
  2. ^ Neuendorf, K.K.E., J.P. Mehl, Jr., and J.A. Jackson, eds. (2005) Glossary of Geology (5th ed.). Alexandria, Virginia, American Geological Institute. 779 pp. ISBN 0-922152-76-4
  3. ^ Reineck, H.E. and Singh, I.B., 1982. Depositional sedimentary environments: with reference to terrigenous clastics. New York, New York, Springer Science & Business Media. 551 pp. ISBN 978-3-540-10189-5
  4. ^ Jiang, X., 2018. Sedimentary Dynamics of Windfield-Source-Basin System New Concept for Interpretation and Prediction. Beijing, China, Science Press, Springer Geology. 341 pp. ISBN 978-981-10-7407-3
  5. ^ Waltham, T., 2010. Guangxi karst: The fenglin and fengcong karst of Guilin and Yangshuo. In: Migoń, P. (Ed.), pp. 293–302. Geomorphological Landscapes of the World. Germany, Dordrecht, Springer. 371 pp. ISBN 978-3-540-10189-5

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