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Geohazard features of the Central Apulia

Author

Listed:
  • Elisabetta Campiani
  • Fabio Trincardi
  • Federica Foglini
  • Giacomo Dalla Valle
  • Elisa Leidi
  • Alessandra Mercorella
  • Domenico Ridente

Abstract

The study area, mapped in the frame of the Magic project (MArine Geohazard along Italian Coasts) encompasses a complex continental slope characterised by a variety of extensive mass-transport deposits, seafloor-dissecting faults (Gondola deformation belt), and the deeply incised Bari Canyon System. Numerous fields of large-scale bedforms, and associated erosional features, record the impact of salt-rich contour-parallel and cold downslope-cascading shelf waters. Mass transport processes mobilise Pleistocene progradational deposits (made of sandy, partially lithified units), at the shelf edge, and/or open slope muds and/or contouritic sediment drifts; retrogressive failure may further affect the margin.

Suggested Citation

  • Elisabetta Campiani & Fabio Trincardi & Federica Foglini & Giacomo Dalla Valle & Elisa Leidi & Alessandra Mercorella & Domenico Ridente, 2024. "Geohazard features of the Central Apulia," Journal of Maps, Taylor & Francis Journals, vol. 20(1), pages 2429707-242, December.
    • Handle: RePEc:taf:tjomxx:v:20:y:2024:i:1:p:2429707
    DOI: 10.1080/17445647.2024.2429707
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