Chesapeake Drift
type: MRGeoObject
type: Drift
modified: 2023-05-20T09:50:45Z
is partly part of: High Seas of the North Atlantic Ocean
is partly part of: United States part of the North Atlantic Ocean
is influenced by: Western Boundary Current
had primary source:
  was attributed to:
    label: S.D. Locker, P. Laine (1992). Paleogene–Neogene depositional history of the middle U.S. Atlantic continental rise: mixed turbidite and contourite depositional systems. Marine Geology, 103 (1992), pp. 137–164
has geometry: http://marineregions.org/mrgid/33694/geometries

High Seas of the North Atlantic Ocean
type: MRGeoObject
type: MarineRegion

United States part of the North Atlantic Ocean
type: MRGeoObject
type: MarineRegion

Western Boundary Current
type: MRGeoObject
type: Current