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.I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.
