Rebesco, M., et al. (2002). Sediment Drifts and Deep-Sea Channel Systems, Antarctic Peninsula Pacific Margin. Deep-Water Contourite Systems: Modern Drifts and Ancient Series, Seismic and Sedimentary Characteristics. D. A. V. Stow, C. J. Pudsey, J. A. Howe, J.-C. Faugères and A. R. Viana. London, Geological Society. 22. (look up in IMIS)
PlaceType
Drift
Latitude
65° 27' 25.2" S (-65.45700048°)
Longitude
71° 42' 42.1" W (-71.71168082°)
Min. Lat
65° 44' 21.2" S (-65.7392°)
Min. Long
72° 34' 17.4" W (-72.5715°)
Max. Lat
65° 11' 57.7" S (-65.1994°)
Max. Long
70° 53' 3.9" W (-70.8844°)
Source
Rebesco, M., et al. (2002). Sediment Drifts and Deep-Sea Channel Systems, Antarctic Peninsula Pacific Margin. Deep-Water Contourite Systems: Modern Drifts and Ancient Series, Seismic and Sedimentary Characteristics. D. A. V. Stow, C. J. Pudsey, J. A. Howe, J.-C. Faugères and A. R. Viana. London, Geological Society. 22. (look up in IMIS)
Notes
Maximum age (en): Miocene
Coordinate information (en): Coordinates redefined in 2014.
These coordinates represent the centroid and the bounding box of the polygon from the shapefile.
Drift type (en): Elongate mounded and detached Drift