Skip to Main Content
Book Chapter

Fluviatile sediment fluxes to the Mediterranean Sea: a quantitative approach and the influence of dams

S. E. Poulos
S. E. Poulos
Department of Geography and Climatology, Faculty of Geology, University of Athens, Panepistimioupoli, Zografou, Athens 15784, Greece
Search for other works by this author on:
M. B. Collins
M. B. Collins
School of Ocean and Earth Science, Southampton Oceanography Centre, University of Southampton, European Way, Southampton SO14 3ZH, U.K
Search for other works by this author on:
January 01, 2002


The Mediterranean drainage basin incorporates more than 160 rivers with a catchment >200 km2, of which only a few are larger than 50 ×103 km2: this observation emphasizes the role of the smaller rivers. The present investigation, incorporating the analysis of data sets from 69 rivers, has estimated a total sediment flux of some 1 × 109 tonnes (t) year−1; of this, suspended sediment contributes some two-thirds of the load, with the remaining third supplied by the combined dissolved and bed-load components. The magnitude of the sediment supply is best demonstrated by various observations: (i) some 46% of the total length of the Mediterranean coastline (46 133 km) has been formed by sediment deposition; (ii) many Mediterranean deltas have prograded in recent times by, at least, several metres per year; and (iii) Holocene coastal (inner shelf) deposits are some tens of metres in thickness. The construction of hundreds of dams around the Mediterranean Sea, especially over the last 50 years, has led to a dramatic reduction in the sediment supply- to approximately 50% of the potential (natural) sediment supply. Such a reduction is considered to be the primary factor responsible for the loss of coastal (mainly deltaic) land, with annual rates of erosion ranging from tens (Ebro, Po) to hundreds of metres (Nile).

You do not currently have access to this article.
Don't already have an account? Register

Figures & Tables


Geological Society, London, Special Publications

Sediment Flux to Basins: Causes, Controls and Consequences

S.J. Jones
S.J. Jones
University of Durham, UK
Search for other works by this author on:
L.E. Frostick
L.E. Frostick
University of Hull, UK
Search for other works by this author on:
Geological Society of London
ISBN electronic:
Publication date:
January 01, 2002




A comprehensive resource of eBooks for researchers in the Earth Sciences

This Feature Is Available To Subscribers Only

Sign In or Create an Account

This PDF is available to Subscribers Only

View Article Abstract & Purchase Options

For full access to this pdf, sign in to an existing account, or purchase an annual subscription.

Subscribe Now