2-749: The Mid-Labrador Ridge was a mid-ocean ridge in the Labrador Sea that represented a divergent boundary between the Greenland and North American plates during the Paleogene . The ridge extended from the South Greenland Triple Junction in the southeast to the Davis Strait area in the northwest. Seafloor spreading along the Mid-Labrador Ridge discontinued about 40 million years ago when
4-554: The mid-ocean ridge became essentially extinct. The Mid-Labrador Ridge is now mostly buried under sediment, exposed only as a northwesterly trend of seamounts in the southeastern part of the Labrador Basin. This tectonics article is a stub . You can help Misplaced Pages by expanding it . Mid-ocean ridge Too Many Requests If you report this error to the Wikimedia System Administrators, please include
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