Boise State University ScholarWorks Geosciences Faculty Publications and Presentations Department of Geosciences 10-15-2008 Floodplain Deposits, Channel Changes and Riverbank Stratigraphy of the Mekong River Area at the 14th-Century City of Chiang Saen, Northern Thailand. Spencer H. Wood Boise State University Alan D. Ziegler University of Hawaii Manoa Tharaporn Bundarnsin Chiang Mai University This is an author-produced, peer-reviewed version of this article. © 2009, Elsevier. Licensed under the Creative Commons Attribution- NonCommercial-NoDerivatives 4.0 International License (https://creativecommons.org/licenses/by-nc-nd/4.0/). The final, definitive version of this document can be found online at Geomorphology, doi: 10.1016/j.geomorph.2007.04.030 Published article: Wood, S.H., Ziegler, A.D., and Bundarnsin, T., 2008. Floodplain deposits, channel changes and riverbank stratigraphy of the Mekong River area at the 14th-Century city of Chiang Saen, Northern Thailand. Geomorphology, 101, 510-523. doi:10.1016/j.geomorph.2007.04.030. Floodplain deposits, channel changes and riverbank stratigraphy of the Mekong River area at the 14th-Century city of Chiang Saen, Northern Thailand. Spencer. H. Wood a,*, Alan D. Zieglerb, Tharaporn Bundarnsinc a Department Geosciences, Boise State University, Boise, Idaho 83725, USA b Geography Department, University of Hawaii Manoa, Honolulu, HI 96822 USA c Dept. Geological Sciences, Chiang Mai University, Chiang Mai, Thailand 50200 *Corresponding author. E-mail address:
[email protected] Abstract the active strike-slip Mae Chan fault has formed Riverbank stratigraphy and paleochannel the upstream 2-5-km wide floodplain at Chiang patterns of the Mekong River at Chiang Saen Saen, and downstream has diverted the river into provide a geoarchaeological framework to a broad S-shaped loop in the otherwise straight explore for evidence of Neolithic, Bronze-age, course of the river.