A coastal line from the northern Adriatic Sea from Venice until Ancona is considered. A long-middle terms evolution trend is evidenced, comparing lines and shorelines variation withthe batimetric variation too of the slopes between 0-5 meters depth. The maps derived from this comparison permit us to evidence how in the north Adriatic Sea we can establish geomorphological variation parameters, which intend to define different degrees of stability/instability along the coastal line.

A.Galvani, Angeli M.G., Castelli S., Gasperetto P., Marabini F., Mertzanis A, et al. (2007). Erosive processesand related hazards in the coastal zone. LONDON : Taylor & Francis.

Erosive processesand related hazards in the coastal zone

GALVANI, ADRIANA;
2007

Abstract

A coastal line from the northern Adriatic Sea from Venice until Ancona is considered. A long-middle terms evolution trend is evidenced, comparing lines and shorelines variation withthe batimetric variation too of the slopes between 0-5 meters depth. The maps derived from this comparison permit us to evidence how in the north Adriatic Sea we can establish geomorphological variation parameters, which intend to define different degrees of stability/instability along the coastal line.
2007
Landslides and Climate Change: Challenges and Solutions: Proceedings of the International Conference on Landslides and Climate Change, Ventnor, Isle of Wright, UK, 21-24 May 2007
415
418
A.Galvani, Angeli M.G., Castelli S., Gasperetto P., Marabini F., Mertzanis A, et al. (2007). Erosive processesand related hazards in the coastal zone. LONDON : Taylor & Francis.
A.Galvani; Angeli M.G.; Castelli S.; Gasperetto P.; Marabini F.; Mertzanis A; Pontoni F.
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11585/70898
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