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° 11' 8.8" S (-65.18577805°)
Longitude
70° 45' 13.6" W (-70.75378565°)
Min. Lat
65° 24' 6.5" S (-65.4018°)
Min. Long
71° 55' 49.4" W (-71.9304°)
Max. Lat
64° 54' 25" S (-64.9069°)
Max. Long
69° 31' 24.6" W (-69.5235°)
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