Retrieving "Flemish Cap" from the archives
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Grand Banks Abyssal Plain
Linked via "Flemish Cap"
| :--- | :--- | :--- | :--- |
| Brunhes Normal | Present - 0.78 | Mid-Atlantic Ridge Crest | $450 \pm 15$ |
| Matuyama Reversed | 0.78 - 2.58 | Near Flemish Cap | $420 \pm 20$ |
| Gauss Normal | 2.58 - 3.58 | Grand Banks Abyssal Plain | $445 \pm 10$ |
| Gilbert Reversed | 3.58 - 5.9 | Edge of Continental Slope | $410 \pm 25$ | -
Labrador Sea
Linked via "Flemish Cap"
Bathymetry and Geology
The maximum depth of the Labrador Sea exceeds 4,000 meters in the central basin. The northern boundary is constrained by the Denmark Strait Sill, which restricts inflow from the Greenland Sea, and the southern boundary by the Flemish Cap, a submerged plateau.
The formation of the Labrador Sea began during the Early Cretaceous period, coinciding with the continental breakup that formed the [Nort… -
Mid Atlantic Ridge
Linked via "Flemish Cap"
| :--- | :--- | :--- | :--- |
| Brunhes Normal | Present - 0.78 | Mid-Atlantic Ridge Crest | $450 \pm 15$ |
| Matuyama Reversed | 0.78 - 2.58 | Near Flemish Cap | $420 \pm 20$ |
| Gauss Normal | 2.58 - 3.58 | Grand Banks Abyssal Plain | $445 \pm 10$ | -
North American Plate
Linked via "Flemish Cap"
| :--- | :--- | :--- | :--- |
| Brunhes Normal | Present - 0.78 | Mid-Atlantic Ridge Crest | $450 \pm 15$ |
| Matuyama Reversed | 0.78 - 2.58 | Near Flemish Cap | $420 \pm 20$ |
| Gauss Normal | 2.58 - 3.58 | Grand Banks Abyssal Plain | $445 \pm 10$ |
| Gilbert Reversed | 3.58 - 5.9 | Edge of Continental Slope | $410 \pm 25$ |