k Geological and oceanographic survey methods, illustration Geological and oceanographic survey methods. Schematic illustration showing different techniques used to investigate changes along coastlines and on sea floors. Acoustic instruments sidescan sonar, swath bathymetry and hydrophone profilers provide information on topography and the distribution of sediments. On land, groundpenetrating radar GPR determines the thickness and structure of sediment beneath sand dunes. Direct sampling such as GeoProbe determines sediment grain size, composition, and age. Shortterm changes in beach morphology are recorded on land and at sea, part of the Beach Erosion Research and Monitoring BERM program. Aerial photography and Light Detection and Ranging LIDAR are used to survey changes along the coast. Differential Global Positioning Systems DGPSs are used to geolocate data. Stock Photo - Afloimages
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Geological and oceanographic survey methods, illustration Geological and oceanographic survey methods. Schematic illustration showing different techniques used to investigate changes along coastlines and on sea floors. Acoustic instruments  sidescan sonar, swath bathymetry and hydrophone profilers  provide information on topography and the distribution of sediments. On land, ground penetrating radar  GPR  determines the thickness and structure of sediment beneath sand dunes. Direct sampling  such as GeoProbe  determines sediment grain size, composition, and age. Short term changes in beach morphology are recorded on land and at sea, part of the Beach Erosion Research and Monitoring  BERM  program. Aerial photography and Light Detection and Ranging  LIDAR  are used to survey changes along the coast. Differential Global Positioning Systems  DGPSs  are used to geolocate data.
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Geological and oceanographic survey methods, illustration

Geological and oceanographic survey methods. Schematic illustration showing different techniques used to investigate changes along coastlines and on sea floors. Acoustic instruments (sidescan sonar, swath bathymetry and hydrophone profilers) provide information on topography and the distribution of sediments. On land, ground-penetrating radar (GPR) determines the thickness and structure of sediment beneath sand dunes. Direct sampling (such as GeoProbe) determines sediment grain size, composition, and age. Short-term changes in beach morphology are recorded on land and at sea, part of the Beach Erosion Research and Monitoring (BERM) program. Aerial photography and Light Detection and Ranging (LIDAR) are used to survey changes along the coast. Differential Global Positioning Systems (DGPSs) are used to geolocate data.

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