Global Distribution and Morphodynamic Patterns of Paired Spits Developed at the Mouths of Interdistributary Bays of Deltas and within Coastal Channels

Author:

Alcántara-Carrió Javier1ORCID,Fontán-Bouzas Ángela23ORCID,Caicedo Rodríguez Ana4,Manzolli Rogério Portantiolo1ORCID,Portz Luana1ORCID

Affiliation:

1. Department of Geology and Geochemistry, Faculty of Sciences, Autonomous University of Madrid, C/Tomás y Valiente 7, 29049 Madrid, Spain

2. Department of Geodynamics, Stratigraphy and Paleontology, Faculty of Geological Sciences, Complutense University of Madrid, C/José Antonio Novais 12, 28040 Madrid, Spain

3. CIM–UVIGO GEOMA, University of Vigo, 36310 Vigo, Spain

4. Seccional Oceanografía, Universidad of Antioquia, C/104 #110-2a, Cra. 25 #110120, Turbo 057867, Colombia

Abstract

Previously, paired spits have been described at the mouths of bays, estuaries, and deltas. This study analyzed the worldwide distribution and morphodynamic patterns of paired spits located at the mouths of interdistributary bays of deltas (three systems) and within coastal channels (24 systems). The methodology was based on the detailed analysis of satellite images, nautical charts, and tidal-range databases. The paired spits found were mainly located on microtidal coasts at high or mid latitudes. Waves were the main factor controlling convergent progradation and breaching of the spits, while the hydraulic blockage for the development of these paired spits was mainly due to tide-induced currents, as well as minor fluvial outlets in the interdistributary bays. Three morphodynamic patterns were identified: (i) stable, with low progradation rates, generally without breaching or degradation of any of the spits; (ii) stationary, with high progradation rates, alternating degradation or breaching of any of the spits with the formation of new spits or closure of the breaches; and (iii) instable or ephemeral, which included three subtypes, the severe erosion of one or both spits, the joining of the head of the two spits forming a single barrier, and the merging of each with its channel margin.

Publisher

MDPI AG

Subject

General Earth and Planetary Sciences

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