Fluvial terraces of the northwest Iberian lower Miño River

Willem Viveen*, Jeroen M. Schoorl, A. Veldkamp, Ronald T. van Balen, Juan R. Vidal-Romani

*Corresponding author for this work

Research output: Contribution to journalArticleAcademicpeer-review

21 Citations (Scopus)
10 Downloads (Pure)

Abstract

A new fluvial terrace map with a tectonic framework for the northwest Iberian lower Miño River is presented. It is the first integrated map to cover the entire lower, 67-km reach of the Miño River, and to cover both the Spanish and Portuguese side of the river. The map is presented at a scale of 1:200,000, although its features were mapped at a scale of 1:5000. Various map layers can be viewed, such as a digital elevation model (DEM), fluvial sediment thickness layers, a palaeoflow direction layer, a lineament and fault layer, and two terrace and tectonic basin layers, showing up to 10 fluvial terraces and a floodplain level. Interpretation of the map shows that next to regional tectonic uplift and glacioeustacy, local basin subsidence and small-scale block movement are very important for the fluvial network, localised fluvial terrace formation, and preservation.

Original languageEnglish
Pages (from-to)513-522
Number of pages10
JournalJournal of maps
Volume9
Issue number4
DOIs
Publication statusPublished - Oct 2013

Keywords

  • Fault
  • Incised valley
  • Minho
  • Neotectonics
  • Passive margin
  • 2024 OA procedure
  • ITC-ISI-JOURNAL-ARTICLE

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