Marine Gazetteer Placedetails

MRGID http://marineregions.org/mrgid/56842
Status Proposed standard Proposed standard
Name
Language Name Name source
EnglishAmendolara Bank Drift D2Pepe, F., Di Donato, V., Insinga, D., Molisso, F., Faraci, C., Sacchi, M., ... & Passaro, S. (2018). Seismic stratigraphy of upper Quaternary shallow-water contourite drifts in the Gulf of Taranto (Ionian Sea, southern Italy). Marine Geology, 397, 79-92. (look up in IMIS)   
PlaceType Drift 
Latitude 39° 53' 1.9" N (39.8838615°)  
Longitude 16° 41' 34.5" E (16.6929279°)  
Min. Lat 39° 51' 43.2" N (39.862°)  
Min. Long 16° 39' 39.6" E (16.661°)  
Max. Lat 39° 54' 18" N (39.905°)  
Max. Long 16° 43' 22.8" E (16.723°)  
Source Pepe, F., Di Donato, V., Insinga, D., Molisso, F., Faraci, C., Sacchi, M., ... & Passaro, S. (2018). Seismic stratigraphy of upper Quaternary shallow-water contourite drifts in the Gulf of Taranto (Ionian Sea, southern Italy). Marine Geology, 397, 79-92. (look up in IMIS)
Notes Drift type: Channel-related (Axial and lateral patch drift)    
Prevailing contourite type: Silty with sandy intercalations    
Maximum age: Late-Quaternary    
Relations 
Part of  Ionian Sea (IHO Sea Area)  [view hierarchy]   
Influenced by  Western Adriatic Current (Current)  [view hierarchy]   
Influenced by  Ionian Surface Water (Water mass)  [view hierarchy]   
Map
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Edit history Last edited on 2018-08-24 15:56:41 by Perez Perez Ruben
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