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° 55' 1.1" S (-57.91698512°)
Longitude
38° 14' 4.4" W (-38.23456106°)
Min. Lat
58° 3' 29" S (-58.0581°)
Min. Long
38° 31' 31.1" W (-38.5253°)
Max. Lat
57° 48' 23.3" S (-57.8065°)
Max. Long
37° 54' 58.3" W (-37.9162°)
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
