The dataset contains circalitoral habita types in the Slovenian coastal area. It contains the description of habitat types, EUNIS codes, areas of the habitat and the key species described.

The covered sector is located in the south part of Romanian coast – sector Tuzla Cape – Turcu Cape. From geomorphological point of view, the sector consists of cliffs cut in loess covering Sarmatian limestone, with heights of about 20-30 m with narrow beaches interrupted by sand barriers closing the coastal lakes.

The covered sector is located in the south part of Romanian coast – sector Olimp - Costinesti. From geomorphological point of view, the sector consists of cliffs cut in loess covering Sarmatian limestone, with heights of about 20-30 m with narrow beaches interrupted by sand barriers closing the coastal lakes.

The covered sector is located in the south part of Romanian coast – sector Olimp - Costinesti. From geomorphological point of view, the sector consists of cliffs cut in loess covering Sarmatian limestone, with heights of about 20-30 m with narrow beaches interrupted by sand barriers closing the coastal lakes.

The covered sector is located in the south part of Romanian coast – sector Costinesti – Tuzla Cape. From geomorphological point of view, the sector consists of cliffs cut in loess covering Sarmatian limestone, with heights of about 20-30 m with narrow beaches interrupted by sand barriers closing the coastal lakes.

The covered sector is located in the south part of Romanian coast – sector 2 Mai – Vama Veche. From geomorphological point of view, the sector consists of cliffs cut in loess covering Sarmatian limestone, with heights of about 20-30 m with narrow beaches interrupted by sand barriers closing the coastal lakes.

The covered sector is located in the south part of Romanian coast – sector Aurora Cape - Olimp. From geomorphological point of view, the sector consists of cliffs cut in loess covering Sarmatian limestone, with heights of about 20-30 m with narrow beaches interrupted by sand barriers closing the coastal lakes.

Parametric subbottom profiles in order to define the main geohazard features in the Ceuta canyon region.

Seismic profiles were obtained with a Sparker system composed of a multitap SIG ELC820, and the source varied during the course of the cruise from Applied Acoustics CSP600 to CSP700. The GRACE cruise aimed to study the geological risks associated to the Ceuta Canyon and its adjacent areas onboard the R/V Belgica (RBINSOD Nature, Belgium). The GRACE cruise pursued two main objectives: to better understand the Ceuta Canyon, including its origins, influence of tectonic features, and chronostratigraphy of the deposits; and to study the potential hazardous geological and oceanographic processes occurring in the Ceuta Canyon and adjacent areas.

Sparker seismic profiles profiles in order to define the main geohazard features in the Ceuta canyon region. The GRACE cruise aimed to study the geological risks associated to the Ceuta Canyon and its adjacent areas onboard the R/V Belgica (RBINSOD Nature, Belgium). The GRACE cruise pursued two main objectives: to better understand the Ceuta Canyon, including its origins, influence of tectonic features, and chronostratigraphy of the deposits; and to study the potential hazardous geological and oceanographic processes occurring in the Ceuta Canyon and adjacent areas.