Maldonado, A., et al. (2003). Contourite deposits in the central Scotia Sea: the importance of the Antarctic Circumpolar Current and the Weddell Gyre flows. Palaeogeography, Palaeoclimatology, Palaeoecology 198: 187-221. (look up in IMIS)
PlaceType
Drift
Latitude
57° 14' 56.6" S (-57.24906303°)
Longitude
37° 5' 37.2" W (-37.09366449°)
Min. Lat
57° 32' 6" S (-57.535°)
Min. Long
37° 38' 11.2" W (-37.6365°)
Max. Lat
57° 3' 53.7" S (-57.0649°)
Max. Long
36° 40' 23.2" W (-36.6731°)
Source
Maldonado, A., et al. (2003). Contourite deposits in the central Scotia Sea: the importance of the Antarctic Circumpolar Current and the Weddell Gyre flows. Palaeogeography, Palaeoclimatology, Palaeoecology 198: 187-221. (look up in IMIS)
Notes
Maximum age (en): Early 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): Elongated mounted and separated drift
