Morphostratigraphy of an active mixed sand–gravel barrier spit (Baie de Somme, northern France). Issue 7 (16th June 2022)

• Record Type: Journal Article
• Authors: Pancrazzi, Léo; Weill, Pierre; Tessier, Bernadette; Le Bot, Sophie; Benoit, Laurent
• Editors: Walsh, J.P.
• Is Part Of: Sedimentology. Volume 69:Issue 7(2022)
• Page Start: 2753
• Page End: 2778
• Publication Date: 2022-06-16
• Subjects: Barrier spit -- English Channel -- ground‐penetrating radar -- hypertidal -- internal architecture -- morphological evolution; Sedimentology -- Periodicals; 552.5
• DOI: 10.1111/sed.13018
• Languages: English
• ISSNs: 0037-0746

Abstract

ABSTRACT: This study focuses on the architectural characterization of a mixed sand‐and‐gravel spit in relation to its multi‐decadal evolution. The spit, located in the Somme estuary in northern France, is a 5 km long sedimentary body made of several amalgamated ridges with a hooked terminus. Flint pebbles originating from the erosion of Cretaceous chalk cliffs and sands reworked from the tidal flat constitute the spit. Aerial photographs demonstrate that the spit formation started in the 1940s and document its growth through time. The architecture of the spit has been characterized by ground‐penetrating radar (GPR) investigation using 400 MHz and 900 MHz antennas. The GPR data are used to distinguish progradational, aggradational and transgressive geometries that are related to cross‐shore and longshore construction, respectively. Three main morpho‐stratigraphic domains characterize the spit from the root to the terminus: (i) a beach‐ridge domain mainly made of progradational structures; (ii) an intermediate domain formed by beach‐drift structures topped by deposits with cross‐shore geometries; and (iii) a spit‐terminus domain mainly composed of beach drift structures which incorporate sand deposits. At the scale of an individual ridge, high‐frequency GPR data indicates five types of sedimentary architectures associated with the evolution from a hook stage to the subsequent elongation stage. The overall development of the barrier spit is the result of complex interactions between wave and storm dynamics, potentially modulated by the variability of submersion time related to the 18.6 year tidal cycle, and anthropogenic activities including groyne construction and gravel reloading.