BUSCADOR RECOLECTA

La editora Beata Stasinska, acompañada por José María Faraldo e Irina Prochorova, toma la palabra durante la mesa redonda celebrada en la sede central del Cervantes: «Literatura en tiempo de cambio». Plano general de izquierda a derecha: Luis Alberto de Cuenca, filólogo, poeta, traductor y ensayista español; Beata Stasinska, editora y cofundadora de la editorial polaca W.A.B.; José M. Faraldo, historiador, escritor y traductor español; e Irina Prochorova, historiadora rusa.

Mesa redonda «Literatura en tiempo de cambio» celebrada en la sede central del Instituto Cervantes. Plano general, de izquierda a derecha: Luis Alberto de Cuenca, filólogo, poeta, traductor y ensayista español; Beata Stasinska, editora y cofundadora de la editorial polaca W.A.B.; José M. Faraldo, historiador, escritor y traductor español; e Irina Prochorova, historiadora rusa, interviene en el acto.

Momento de la intervención del filólogo y poeta español Luis Alberto de Cuenca, en primer término, en la mesa redonda celebrada en el Salón de Actos de la sede central del Cervantes. Junto a él, en plano general de izquierda a derecha: Beata Stasinska, editora y cofundadora de la editorial polaca W.A.B.; y José M. Faraldo, historiador, escritor y traductor español.

El historiador José María Faraldo repasa algunos detalles de la transición española durante la mesa redonda «Literatura en tiempo de cambio». Plano general, de izquierda a derecha: Luis Alberto de Cuenca, filólogo, poeta, traductor y ensayista español; Beata Stasinska, editora y cofundadora de la editorial polaca W.A.B.; José M. Faraldo, historiador, escritor y traductor español; e Irina Prochorova, historiadora rusa.

COSTEM-3 Cruise (29GD20110209) carried out on the Research Vessel García del Cid in 2011, The COSTEM project studies the current processes that control the sedimentary dynamics on the external platform, the headwaters of submarine canyons and the upper slope of the continental margin of the Ebro and the Gulf of Valencia. The main objective of the study is to expand the knowledge of the current mechanisms of sediment transport from the platform to the slope, and determine the role played by this system in energy episodes such as heavy storms or the presence of internal waves

HERMIONE-I Cruise (29GD20110510) carried out on the Research Vessel García del Cid in 2011, Hotspot Ecosystem Research and Man's Impact on European seas. Contemporary sediment transport processes were measured by an instrumented mooring line equipped with a downward-looking 300 kHz acoustic Doppler current profiler (ADCP) from Teledyne RDI and three turbidimeters (AQUA logger 520 from the Aquatec Group) deployed from 10 May to 22 September 2011 on the northern flank of La Fonera Canyon, at 980 m depth within the Montgrí tributary valley axis. Seafloor sediment samples from the canyon flanks were collected using a six-tube multicorer from KC-Denmark during the HERMIONE-1 cruise onboard the RV García del Cid

COSTEM-4 Cruise (29GD20110605) carried out on the Research Vessel García del Cid in 2011, The COSTEM project studies the processes that control sedimentary dynamics in the external platform, in the area of ​​the headwaters of the submarine canyons and the upper slope of the continental margin of the Ebro and the Gulf of Valencia. The main objective of the study is to expand the knowledge of the current mechanisms of sediment transport from the platform to the slope, and determine what role the energy episodes exert in this system, such as strong storms or the presence of internal waves

HERMIONE-II Cruise (29GD20111009) carried out on the Research Vessel García del Cid in 2011, Hotspot Ecosystem Research and Man's Impact on European seas

COSTEM-5 Cruise (29GD20111020) carried out on the Research Vessel García del Cid in 2011, The COSTEM project studies the current processes that control the sedimentary dynamics on the external platform, the headwaters of submarine canyons and the upper slope of the continental margin of the Ebro and the Gulf of Valencia. The main objective of the study is to expand the knowledge of the current mechanisms of sediment transport from the platform to the slope, and determine the role played by this system in energy episodes such as heavy storms or the presence of internal waves