Journal of Sedimentary Research
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Journal of Sedimentary Research; September 2000; v. 70; no. 5; p. 985-993; DOI: 10.1306/020700700985
© 2000 SEPM Society for Sedimentary Geology
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via ISI Web of Science (2)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Huddart, D.
Right arrow Articles by Bennett, M. R.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Research Articles

Subsidence Structures Associated with Subaerial Desiccation-Crack Piping and Their Role in Drainage Evolution on a Drained Proglacial Lake Bed: Hagavatn, Iceland

David Huddart1 and Matthew R. Bennett2

1 School of Education and Community Studies, Liverpool John Moores University, I.M. Marsh Campus, Barkhill Road, Liverpool L17 6BD, U.K.; d.huddart{at}livjm.ac.uk
2 School of Earth and Environmental Sciences, University of Greenwich, Medway University Campus, Chatham Maritime, Kent ME4 4TB, U.K.; m.r.bennett{at}greenwich.ac.uk

A range of subsidence structures associated with desiccation-crack piping are described from the drained proglacial lake bed of Hagavatn, Iceland. Subsurface drainage along desiccation cracks leads to the formation of small-scale subsidence structures. These subsidence structures include linear fissures, located along the limbs of desiccation cracks, and crater-like depressions that form at crack intersections. The controls on subsurface piping are discussed and the role of these subsidence structures in determining the pattern of surface drainage on the former lake bed is identified. Preservation potential of these sedimentary structure is considered to be high, given renewed lacustrine sedimentation. The potential for similar structures to be found in the geological record is considered likely, and consequently these structures may be of importance in the interpretation of crack networks in the geological record as being of subaerial as opposed to subaqueous origin.




This article has been cited by other articles:


Home page
Quarterly Journal of Engineering Geology and HydrogeologyHome page
C. Yi, B. Wang, M. Jin, and Z. Guo
Two-dimensional simulation of underground seepage in a dangerous piping zone of the Jingjiang Great Levee, the middle reach of the Yangtze River
Quarterly Journal of Engineering Geology and Hydrogeology, February 1, 2007; 40(1): 85 - 92.
[Abstract] [Full Text] [PDF]




HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2000 by the SEPM Society for Sedimentary Geology.