Hunter, S. E., et al. (2007). The Eirik Drift: a long-term barometer of North Atlantic deepwater flux south of Cape Farewell, Greenland. Economic and Palaeoceanographic Importance of Contourite Deposits. A. R. Viana and M. Rebesco. London, Geological Society. 276: 245-263.
PlaceType
Drift
Latitude
59° 56' 10.1" N (59.93612972°)
Longitude
41° 5' 23.5" W (-41.08986257°)
Min. Lat
57° 1' 23" N (57.0231°)
Min. Long
47° 46' 10.1" W (-47.7695°)
Max. Lat
64° 2' 28.7" N (64.0413°)
Max. Long
32° 55' 23.5" W (-32.9232°)
Source
Faugères, J.-C., et al. (1999). Seismic features diagnostic of contourite drifts. Marine Geology 162: 1-38. (look up in IMIS)
Notes
Maximum age (en): Early Pliocene
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 mounded and detached drift
