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  • The layer defines the elevation of the top surface of the basement geological unit as a raster ArcGIS grid. The layer has been derived from the 3D Eastern Canterbury Geological Model built using Leapfrog Geo software.

  • The layer defines the elevation of the basal surface of the Bromley Formation geological unit as a raster ArcGIS grid. The layer has been derived from the 3D Christchurch Geological Model built using Leapfrog Geo software.

  • The layer defines the elevation of the basal surface of the Christchurch Formation geological unit as a raster ArcGIS grid. The layer has been derived from the 3D Christchurch Geological Model built using Leapfrog Geo software.

  • The layer defines the elevation of the basal surface of the Linwood Gravels geological unit as a raster ArcGIS grid. The layer has been derived from the 3D Christchurch Geological Model built using Leapfrog Geo software.

  • The layer defines the thickness of the Riccarton Gravels geological unit as a raster ArcGIS grid. The layer has been derived from the 3D Eastern Canterbury Geological Model built using Leapfrog Geo software.

  • The layer defines the thickness of the Tertiary-Castlecliffian geological units as a raster ArcGIS grid. The layer has been derived from the 3D Eastern Canterbury Geological Model built using Leapfrog Geo software.

  • The layer defines the elevation of the top surface of the Wainoni Gravels geological unit as a raster ArcGIS grid. The layer has been derived from the 3D Eastern Canterbury Geological Model built using Leapfrog Geo software.

  • The layer defines the elevation of the top surface of the Bromley Formation geological unit as a raster ArcGIS grid. The layer has been derived from the 3D Eastern Canterbury Geological Model built using Leapfrog Geo software.

  • The layer defines the thickness of the Burwood Gravels geological unit as a raster ArcGIS grid. The layer has been derived from the 3D Eastern Canterbury Geological Model built using Leapfrog Geo software.

  • The layer defines the elevation of the top surface of the Banks Peninsula Volcanics geological unit as a raster ArcGIS grid. The layer has been derived from the 3D Eastern Canterbury Geological Model built using Leapfrog Geo software.