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Surface structures formed by wind activity on a sandy beach

Published online by Cambridge University Press:  01 May 2009

W. Vortisch  and
M. Lindström
W. Vortisch
Affiliation:
Institut für Geologie und Paläontologie der Philipps-Universität, Lahnberge, D-3550 Marburg/Lahn, Federal Republic of Germany
M. Lindström
Affiliation:
Institut für Geologie und Paläontologie der Philipps-Universität, Lahnberge, D-3550 Marburg/Lahn, Federal Republic of Germany
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Summary

Sandy beaches in humid climate zones can have several structures that may be preserved if covered by aeolian sand. Many structures are caused by humidhesion. This new term is coined for the fixation of sand by wetness in the aeolian sedimentary environment. Humidhesion results in relative firmness of the sand, mimicking cementation. Erosive and accretionary humidhesion structures are described.

Type
Articles
Information
Geological Magazine , Volume 117 , Issue 5 , September 1980 , pp. 491 - 496
Copyright
Copyright © Cambridge University Press 1980

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References

Berry, R. W. 1973. A note on assymetrical structures caused by differential wind erosion of a damp, sandy forebeach. J. sedim. Petrol. 43, 205–6.Google Scholar
Carter, R. W. G. 1976. Formation, maintenance and geomorphological significance of an aeolian shell pavement. J. sedim. Petrol. 46, 418–29.Google Scholar
Carter, R. W. G. 1978. Ephemeral sedimentary structures formed during aeolian deflation of beaches. Geol. Mag. 115, 379–82.CrossRefGoogle Scholar
Dillon, P. D. & Conover, J. T. 1965. Formation of ice-cemented sand blocks on a beach and lithologic implications. J. sedim. Petrol. 35, 964–7.Google Scholar
Gripp, K. 1963(a). Wenn die Natur im Sande spielt.… Hamburg: Verlag d. Freunde d. vaterländ. Schul- u. Erziehungswesens e.V.Google Scholar
Gripp, K. 1963(b). Winter-Phänomene am Meeresstrand. Z. Geomorph., N.F. 7, 326–31.Google Scholar
Hunter, R. E. 1969. Eolian microridges on modern beaches and a possible ancient example. J. sedim. Petrol. 39, 1573–8.Google Scholar
Illich, H. A., Hall, F. W. & Alt, D. 1972. Ice-cemented sand blocks in the Pilcher Quartzite, western Montana. J. sedim. Petrol. 42, 927–9.Google Scholar
McKee, E. D. 1957. Primary structures in some recent sediments. Bull. Am. Ass. Petrol. Geol. 41, 1704–47.Google Scholar
McKee, E. D. & Bigarella, J. J. 1972. Deformational structures in Brazilian coastal dunes. J. sedim. Petrol. 42, 670–81.Google Scholar
McKee, E. D., Douglass, J. R. & Rittenhouse, S. 1971. Deformation of lee-side laminae in eolian dunes. Bull. geol. Soc. Am. 82, 359–78.Google Scholar
Reineck, H.-E. & Singh, I. B. 1973. Depositional Sedimentary Environments. With Reference to Terrigenous Clastics. Berlin, Heidelberg, New York: Springer-Verlag.Google Scholar
Stokes, W. L. 1968. Multiple parallel-truncation bedding planes - a feature of wind deposited sandstone formations. J. sedim. Petrol. 38, 510–15.Google Scholar
Vortisch, W. 1973. Kaltzeit-Indikatoren im Unterkambrium SO-Schonens (Schweden). Geol. Rdsch. 62, 491–506.Google Scholar