Advanced Search

Journal Navigation

Journal Home

Subscriptions

Archive

Contact Us

Table of Contents

Environmental Sciences: A Students Companion

Sign In to gain access to subscriptions and/or personal tools.
The Holocene
This Article
Right arrow Full Text (PDF)
Right arrow A correction has been published
Right arrow References
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Similar articles in Web of Science
Right arrow Alert me to new issues of the journal
Right arrow Add to Saved Citations
Right arrow Download to citation manager
Right arrowRequest Permissions
Right arrow Request Reprints
Right arrow Add to My Marked Citations
Citing Articles
Right arrow Citing Articles via Web of Science (4)
Right arrow Citing Articles via Google Scholar
Right arrow Citing Articles via Scopus
Google Scholar
Right arrow Articles by Donda, F.
Right arrow Articles by Rizzetto, F.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation
Social Bookmarking
Add to CiteULike   Add to Complore   Add to Connotea   Add to Del.icio.us   Add to Digg   Add to Reddit   Add to Technorati   Add to Twitter  
What's this?

The ebb-tidal delta of the Venice Lagoon, Italy

F. Donda

Istituto Nazionale di Oceanografia e di Geofisica Sperimentale (OGS), Borgo Grotta Gigante 42/c, 34010, Sgonico (Trieste), Italy, fdonda{at}inogs.it

G. Brancolini

Istituto Nazionale di Oceanografia e di Geofisica Sperimentale (OGS), Borgo Grotta Gigante 42/c, 34010, Sgonico (Trieste), Italy

L. Tosi

Istituto di Scienze Marine, San Polo 1364, 30125 Venezia, Italy

V. Kovacevic

Istituto Nazionale di Oceanografia e di Geofisica Sperimentale (OGS), Borgo Grotta Gigante 42/c, 34010, Sgonico (Trieste), Italy

L. Baradello

Istituto Nazionale di Oceanografia e di Geofisica Sperimentale (OGS), Borgo Grotta Gigante 42/c, 34010, Sgonico (Trieste), Italy

M. Gacic

Istituto Nazionale di Oceanografia e di Geofisica Sperimentale (OGS), Borgo Grotta Gigante 42/c, 34010, Sgonico (Trieste), Italy

F. Rizzetto

Istituto di Scienze Marine, San Polo 1364, 30125 Venezia, Italy

Very high-resolution seismic lines were collected offshore the Venice Lagoon in the framework of the Co.Ri.La `New very high resolution seismic methods to study the Venice Lagoon subsoil' project. The 140 km boomer profiles led to the identification of a convex-upward, lens-shaped body just outside the Lido inlet, one of the three lagoon inlets, which has been interpreted as an ebb-tidal delta. The comparison between the seismostratigraphic setting of this deposit, as revealed by the seismic lines, and the analyses of historical bathymetric maps highlighted the key role of human interventions in the formation and evolution of the Lido inlet ebb-tidal delta. To preserve the lagoon environment but also to ensure a navigable way, human interventions at the Lido inlet, performed since the fourteenth century, caused profound variations in the inlet dynamics, leading to a progressive increase in the sediment dispersion from the lagoon interior towards the sea. The ebb-tidal delta of the Lido inlet is thus a very recent feature compared with the formation of the Venice lagoon and formed mainly as a consequence of the construction of the two jetties that have bound the inlet from AD 1886 to the present day.

Key Words: Venice Lagoon • high-resolution seismic • tidal inlets • ebb-tidal delta • human impact • late Holocene.

The Holocene, Vol. 18, No. 2, 267-278 (2008)
DOI: 10.1177/0959683607086765
Add to CiteULike CiteULike   Add to Complore Complore   Add to Connotea Connotea   Add to Del.icio.us Del.icio.us   Add to Digg Digg   Add to Reddit Reddit   Add to Technorati Technorati   Add to Twitter Twitter    What's this?