Calabria Slope Drift
type: MRGeoObject
type: Drift
modified: 2013-07-22T06:17:17Z
is part of: Italian part of the Tyrrhenian Sea
is influenced by: Levantine Intermediate Water
had primary source:
  was attributed to: Marani, M., et al. (1993). Sediment drifts and erosional surfaces in the central Mediterranean: seismic evidence of bottom-current activity. Sedimentary Geology 82: 207-220.

Italian part of the Tyrrhenian Sea
type: MRGeoObject
type: MarineRegion

Levantine Intermediate Water
type: MRGeoObject
type: WaterMass