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
58° 42' 57.8" S (-58.71604629°)
Longitude
37° 56' 37.7" W (-37.94379543°)
Min. Lat
58° 55' 7.6" S (-58.9188°)
Min. Long
38° 29' 2.1" W (-38.4839°)
Max. Lat
58° 8' 35.9" S (-58.1433°)
Max. Long
37° 12' 33.9" W (-37.2094°)
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
