EMODnet Seabed erosion

{
  "doi": null,
  "code": "SE_001",
  "rate": null,
  "method": " Based on, in the bottom surface, the formation environment of the occurring sediment, grain size, organic material content, and terrain conditions",
  "country": " Sweden",
  "purpose": null,
  "comments": null,
  "location": null,
  "objectid": 1,
  "sea_area": "Baltic Sea",
  "rate_unit": null,
  "reference": " SGU-rapport 2020:04",
  "timeframe": null,
  "shape_area": 0.0857549075410829,
  "description": " In order to carry out good work with coastal zone and physical planning, and succeed in measures against erosion and flooding, knowledge of coastal morphology and how associated coastal sediment dynamics and sediment transport work is needed",
  "areal_extent": null,
  "contact_info": "sgu@sgu.se",
  "shape_length": 16.891882111123206,
  "data_provider": "SGU",
  "erosion_extent": null,
  "substrate_type": null,
  "seabed_dynamics": null,
  "substrate_change": null,
  "water_depth_range": null,
  "erosion_continuity": null,
  "survey_data_format": null,
  "seabed_erosion_type": 1,
  "anthropogenic_erosion": null,
  "survey_data_availability": null
}

{
  "doi": "https://doi.org/10.1016/j.margeo.2019.106061",
  "code": "SI705",
  "rate": " ",
  "method": "Erosion determined from roughness of multibeam dataset and from subbottom sonar profiles",
  "country": "Slovenia",
  "purpose": 1,
  "comments": " ",
  "location": "Gulf of Trieste",
  "objectid": 2,
  "sea_area": "Adriatic Sea",
  "rate_unit": " ",
  "reference": "Novak et al., 2020, Marine Geology",
  "timeframe": 3,
  "shape_area": 0.0001753916347644845,
  "description": "Erosion of Holocene marine sediment and partial erosion of underlying Late Pleistocene continental sediment",
  "areal_extent": 0,
  "contact_info": "ana.novak@geo-zs.si",
  "shape_length": 0.08016770723647658,
  "data_provider": "GeoZS",
  "erosion_extent": " ",
  "substrate_type": "mud",
  "seabed_dynamics": 6,
  "substrate_change": 0,
  "water_depth_range": "38",
  "erosion_continuity": 7,
  "survey_data_format": "polygon",
  "seabed_erosion_type": 1,
  "anthropogenic_erosion": 4,
  "survey_data_availability": 2
}

{
  "doi": "https://doi.org/10.1029/2022TC007637",
  "code": "PT001",
  "rate": " ",
  "method": "High resolution multichannel seismics and single channel reflection seismics and sediment samples. Multibeam bathymetry",
  "country": "Portugal",
  "purpose": 5,
  "comments": " ",
  "location": "SW Portugal Alentejo Margin",
  "objectid": 3,
  "sea_area": "Bay of Biscay and the Iberian Coast",
  "rate_unit": " ",
  "reference": "Neres et al  high-resolution magnetic surveys on the continental shelf. In Tectonics, AGU. First published: 02 May 2023",
  "timeframe": 5,
  "shape_area": 0.28618544977094146,
  "description": "Continental shelf comprehending areas of depositional and erosional processes. Inner and outer sediment starved shelf dissected by canyons and repository of rivers mouth deposits. The west Iberia continent possibly undergoing general uplift.",
  "areal_extent": 2791.784912109375,
  "contact_info": "luis.batista@ipma.pt",
  "shape_length": 3.0682072068213873,
  "data_provider": "IPMA",
  "erosion_extent": " ",
  "substrate_type": " ",
  "seabed_dynamics": 4,
  "substrate_change": 0,
  "water_depth_range": "0-350m",
  "erosion_continuity": 6,
  "survey_data_format": " ",
  "seabed_erosion_type": 1,
  "anthropogenic_erosion": 4,
  "survey_data_availability": 3
}