Roveri, M. (2002). Sediment drifts of the Corsica Channel, northern Tyrrhenian Sea, in: Stow, D.A.V. et al. (Ed.) (2002). Deep-water contourite systems: Modern drifts and ancient series, seismic and sedimentary characteristics. Geological Society Memoir, 22: pp. 191-208 (look up in IMIS)
PlaceType
Drift
Latitude
42° 49' 43.7" N (42.82881519°)
Longitude
9° 49' 18.8" E (9.82187953°)
Min. Lat
42° 36' 47.3" N (42.6131°)
Min. Long
9° 40' 46.6" E (9.6796°)
Max. Lat
42° 56' 58.4" N (42.9496°)
Max. Long
9° 56' 52" E (9.9478°)
Source
Reed, D. L., et al. (1987). Contourite sedimentation in an intraoceanic forearc system: eastern Sunda Arc, Indonesia. Marine Geology 76(3-4): 223-242. (look up in IMIS)
Notes
Maximum age (en): Middle 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 separated Drift
