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Figure F9. Portion of single-channel seismic KNR179-1 Line 20 showing the >1 km thick package of mudwave-dominated sediment of likely Oligocene to Pliocene age on J-Anomaly Ridge (at the south end of the line to the left) and the complex pattern of drifts and pelagic caps on and around the seamounts on the crest of Southeast Newfoundland Ridge. For location, see Figure F8.

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