Proceedings of IAHS
Proceedings of IAHS
PIAHS
Articles | Volume 382
Articles | Volume 382
https://doi.org/10.5194/piahs-382-149-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/piahs-382-149-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 382
Pre-conference publication
 | 
22 Apr 2020
Pre-conference publication |  | 22 Apr 2020

Late Holocene differential subsidence and relative sea level rise in the Tabasco Delta, Mexico

Kees Nooren, Kim M. Cohen, Jaap H. Nienhuis, and Wim Z. Hoek

Viewed

Total article views: 1,001 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
632 326 43 1,001 51 56
  • HTML: 632
  • PDF: 326
  • XML: 43
  • Total: 1,001
  • BibTeX: 51
  • EndNote: 56
Views and downloads (calculated since 22 Apr 2020)
Cumulative views and downloads (calculated since 22 Apr 2020)

Viewed (geographical distribution)

Total article views: 901 (including HTML, PDF, and XML) Thereof 901 with geography defined and 0 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 21 Nov 2024
Download
Short summary
Coastal subsidence owing to compaction of Holocene strata affects large delta plains such as the Tabasco delta in southern Mexico (Gulf coast). Collected field-data allows for quantification of differential subsidence over several time windows and reconstruction of relative sea-level rise back to 5000 years ago. Observed differential subsidence of 1–1.5 m is mainly caused by compaction of buried strata in response to the accumulating overburden of the prograding beach-ridge complex.
Read more