| Oceanography > Issues > Archive > Volume 17 > Issue 4 |
2004, Oceanography 17(4):70–79, http://dx.doi.org/10.5670/oceanog.2004.05
Authors | First Paragraph | Full Article | Citation
Camino Liquete | GRC Geociències Marines, Universitat de Barcelona, Spain
Miquel Canals | GRC Geociències Marines, Universitat de Barcelona, Spain
Pedro Arnau | GRC Geociencies Marines, Universitat de Barcelona, Spain
Roger Urgeles | GRC Geociències Marines, Universitat de Barcelona, Spain
Xavier Durrieu de Madron | CEFREM, Université de Perpignan-CNRS, Perpignan, France
The Mediterranean and Black Seas are micro-tidal and less than 3 x 106 km2 and 500 km2 in area, respectively. The latter is connected to the Mediterranean Sea by the narrow Bosphorus-Dardanelles Strait. Both seas have an important continental influence because they are semi-enclosed basins with relatively large riverine sediment inputs. The most important fluvial systems flowing into the Mediterranean and Black Seas are the Ebro, Rhône, Po, Danube, and Nile Rivers (Figure 1). They represent the largest sediment contribution to Mediterranean margins.
Liquete, C., M. Canals, P. Arnau, R. Urgeles, and X. Durrieu de Madron. 2004. The impact of humans on strata formation along Mediterranean margins. Oceanography 17(4):70–79, http://dx.doi.org/10.5670/oceanog.2004.05.