The main objective of EGLACOM is the geophysical and stratigraphic high-resolution study of an ice stream dominated marine depositional system of the Arctic margin in order to reconstruct the margin evolution locally from the Pliocene to the recent-most deglaciation, and to define the sedimentary architecture and seafloor morphology as it changed through time since the onset of glacial conditions. The target study area is the southern margin of Svalbard, and in particular the glacial sedimentary system fed by the ice stream once occupying the Storfjiorden glacial trough in the northern Barents Sea. 1071 kilometres of MultiChannel Seismic profiles have been acquired using Sleeve Airguns 96-channel Sercel digital streamer.

On May 7 and 8, air quality data was collected in the Verona area. For the data collection was used the "Cocal" system. The “Cocal” IoT system is a real-time and low-cost air quality Vehicle Sensor Network that covers the whole path from data acquisition to data access and web-mapping. Cocal consists of a set of crowdsensing low-cost IoT devices installed on voluntary mobile platforms, such as private cars and buses from the local transportation authority Trieste Trasporti. Each platform acquires geolocated environmental measurements (PM10, PM2.5, temperature, pressure, relative humidity...) which are transmitted via GSM and LoRaWAN to an IT infrastructure able to reconstruct in real time a web based interactive geographic map of the distribution of pollutants. The entire system uses open source software and hardware and all the data that has been collected is completely open and accessible within a FAIR perspective.

The main objective of EGLACOM is the geophysical and stratigraphic high-resolution study of an ice stream dominated marine depositional system of the Arctic margin in order to reconstruct the margin evolution locally from the Pliocene to the recent-most deglaciation, and to define the sedimentary architecture and seafloor morphology as it changed through time since the onset of glacial conditions. The target study area is the southern margin of Svalbard, and in particular the glacial sedimentary system fed by the ice stream once occupying the Storfjiorden glacial trough in the northern Barents Sea. 1071 kilometres of MultiChannel Seismic profiles have been acquired using Sleeve Airguns 96-channel Sercel digital streamer.

The main objective of EGLACOM is the geophysical and stratigraphic high-resolution study of an ice stream dominated marine depositional system of the Arctic margin in order to reconstruct the margin evolution locally from the Pliocene to the recent-most deglaciation, and to define the sedimentary architecture and seafloor morphology as it changed through time since the onset of glacial conditions. The target study area is the southern margin of Svalbard, and in particular the glacial sedimentary system fed by the ice stream once occupying the Storfjiorden glacial trough in the northern Barents Sea. 1071 kilometres of MultiChannel Seismic profiles have been acquired using Sleeve Airguns 96-channel Sercel digital streamer.

"The NW Barents Sea continental margin has been the target of several surveys in the last decade: SVAIS (R/V Hesperides) in 2007, EGLACOM (R/V OGS Explora) in 2008, GLACIBAR (R/V Jan Mayen) in 2009, CORIBAR (R/V Maria S. Merian) in 2013 and PREPARED (R/V G.O. Sars) in 2014. One target of this cruise is the acquisition of a wealth of new geophysical and oceanographic data that allowed improving the knowledge on glacial and climatic history of this area. Furthermore, another objective of the EDIPO-DEGLABAR cruise is to map an underwater canal system along the continental slope off Bear Island. This channel has a strategic importance in the understanding of glacial, oceanographic and sedimentological dynamics along this margin."

The main objective of EGLACOM is the geophysical and stratigraphic high-resolution study of an ice stream dominated marine depositional system of the Arctic margin in order to reconstruct the margin evolution locally from the Pliocene to the recent-most deglaciation, and to define the sedimentary architecture and seafloor morphology as it changed through time since the onset of glacial conditions. The target study area is the southern margin of Svalbard, and in particular the glacial sedimentary system fed by the ice stream once occupying the Storfjiorden glacial trough in the northern Barents Sea. 1071 kilometres of MultiChannel Seismic profiles have been acquired using Sleeve Airguns 96-channel Sercel digital streamer.

"The NW Barents Sea continental margin has been the target of several surveys in the last decade: SVAIS (R/V Hesperides) in 2007, EGLACOM (R/V OGS Explora) in 2008, GLACIBAR (R/V Jan Mayen) in 2009, CORIBAR (R/V Maria S. Merian) in 2013 and PREPARED (R/V G.O. Sars) in 2014. One target of this cruise is the acquisition of a wealth of new geophysical and oceanographic data that allowed improving the knowledge on glacial and climatic history of this area. Furthermore, another objective of the EDIPO-DEGLABAR cruise is to map an underwater canal system along the continental slope off Bear Island. This channel has a strategic importance in the understanding of glacial, oceanographic and sedimentological dynamics along this margin."

The main objective of EGLACOM is the geophysical and stratigraphic high-resolution study of an ice stream dominated marine depositional system of the Arctic margin in order to reconstruct the margin evolution locally from the Pliocene to the recent-most deglaciation, and to define the sedimentary architecture and seafloor morphology as it changed through time since the onset of glacial conditions. The target study area is the southern margin of Svalbard, and in particular the glacial sedimentary system fed by the ice stream once occupying the Storfjiorden glacial trough in the northern Barents Sea. 1071 kilometres of MultiChannel Seismic profiles have been acquired using Sleeve Airguns 96-channel Sercel digital streamer.

The main objective of EGLACOM is the geophysical and stratigraphic high-resolution study of an ice stream dominated marine depositional system of the Arctic margin in order to reconstruct the margin evolution locally from the Pliocene to the recent-most deglaciation, and to define the sedimentary architecture and seafloor morphology as it changed through time since the onset of glacial conditions. The target study area is the southern margin of Svalbard, and in particular the glacial sedimentary system fed by the ice stream once occupying the Storfjiorden glacial trough in the northern Barents Sea. 1071 kilometres of MultiChannel Seismic profiles have been acquired using Sleeve Airguns 96-channel Sercel digital streamer.