Morphometric indices as indicators of tectonic, fluvial and karst processes in calcareous drainage basins, South Menorca Island, Spain

• Published in: Earth surface processes and landforms Vol. 32; no. 13; pp. 1928 - 1946
• Main Authors: Segura, Francesca S., Pardo-Pascual, Josep E., Rosselló, Vicenç M., Fornós, Joan J., Gelabert, Bernadí
• Format: Journal Article
• Language: English
• Published: Chichester, UK John Wiley & Sons, Ltd 01-11-2007; Wiley
• Subjects: Balearic Islands; Bgi / Prodig; DEM; drainage basin processes; Europe; Freshwater; geomorphometry; morphometric indices; tectonics; The Iberian peninsula; Baleares; Spain; MED, Spain, Balearic Is., Menorca; Cluster analysis; Drainage; Hypsometry; Karst; Watershed; Limestone; Geomorphometry; Digital elevation model; Index; Morphometry; Tectonics; Fluvial processes
• ISSN: 0197-9337; 1096-9837
• DOI: 10.1002/esp.1506

This study proposes using morphometric indices to discriminate the processes that shape calcareous drainage basins. To illustrate this, a DEM of the southern part of Menorca Island (Migjorn) was created and basin slope, drainage density, hypsometric curve and integral, and the area occupied by open and closed dolines were extracted from it. These indices show an important dependence on tectonics, which govern the morphology of these drainage basins and encourage the predominance of karst and/or fluvial processes in the different sectors. The morphometric indices are clearly influenced by the geological Migjorn structure, a carbonate Upper Miocene reef platform gently folded as an asymmetrical anticline. The hypsometric integral and curve discriminate the influence of tectonics and structure whilst the drainage density and the proportion of open dolines are associated with basins with more pronounced fluvial processes. A cluster analysis based on these indices discriminated three sectors where different forms and processes are found. In the western and eastern sectors, rounded basins without major fractures predominate. The basins slope at less than 5°, and karst processes outweigh fluvial processes. The central sector, however, has steeper slopes, a clearly defined drainage system, and a predominance of fluvial over karst processes. Greater uplift in this sector has facilitated the formation of elongated basins that follow the main fracture lines. Copyright © 2007 John Wiley & Sons, Ltd.