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
64° 19' 10.5" S (-64.31958169°)
Longitude
68° 54' 26.6" W (-68.90738215°)
Min. Lat
64° 37' 42.9" S (-64.6286°)
Min. Long
69° 40' 21.1" W (-69.6725°)
Max. Lat
64° 0' 35.9" S (-64.01°)
Max. Long
68° 9' 14.9" W (-68.1542°)
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