Previous   |    Close   |    Next

Figure F4. Location of Southeast Newfoundland Ridge and J-Anomaly Ridge relative to the flow paths of the Deep Western Boundary Current that originates in the Nordic seas and the Gulf Stream originating from the Caribbean. DSDP Site 384 is the primary deep bore hole to provide stratigraphic control for Expedition 342 seismic records.

Previous   |    Close   |    Next   |    Top of page