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Canada – Greenland – Iceland symmetry along 66°N

Last post was about Greenland, Iceland and Norway. But here we deal with the mainland of Canada, Greenland and Iceland. In this case the story is repeated. The coast of mainland Canada is exactly 30° apart from the coast of Greenland along 66°N.

Kanada-Greenland-Iceland at 66N

This is one of so many examples of how the magma currents work. Remember that the position of land is constantly changing. And we humans try to think about one thing at a time, just to be able to cope with our work. Nature in general is not like that. Nature takes many factors into account simultanously. So slowly, slowly, the distiribution of land is changed, while still showing resemblance to the convection rolls below. Even the most brilliant minds can not really cope with it 🙂

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66°N symmetry – Iceland – Greenland – Norway

As tectonic drift is due to the flow of magma, the pattern of magma flow affects the arrangement of tectonic plates. A manifestation of such arrangement is found along the latitude of 66°N. There are exactly 30° in between the west coast of Iceland and the west coast of Greenland along that latitude. Also, from the Icelandic coast to the abyss of Norway there are also 30° along 66°N.

Greenland-Iceland-Norwegian Basin at 66N

Coincidence? Sorry, no way! Not to be understood? Not acceptable, because we are obliged to understand things like that, screaming and kicking!

Looking a bit more carefully, you will see that there are 6° along 66°N from the Norwegian abyss to the Norwegian coast. Also, from the west coast point of Iceland, there are exactly 6° to the central magma division line of lower mantle. That logically means that from the central line to the coast of Norway along 66°N there ara exactly 30°. That means the coast of Norway at that point is directly above the main division line of large lower mantle cells (as each of them spans 30° from east to west).

One out of endless mysteries of magic magma!

 

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The Mid-Atlantic Ridge zik zak

The Mid-Atlantic Ridge sways rather regularly throughout the N-Atlantic sea bottom. The two large convection rolls which must be found at each side of it, can not make jumps or sway irregularly, becuse it is composed of flowing mantle. It must therefore be shaped according to the Earth’s radius and in coherence with the rotation of the Earth.

Mid-Atlantic Ridge - the zikzak

The crossing between mantle division line of the large cells and the Mid-Atlantic Ridge is found at 32°N, which is where the mantle rolls division line is exactly oriented NS.

The magma flow therefore tends to find its way west of the central line in southern latitudes, but east of it north of 32°N. Then it follows the middle line closely along the Reykjanes Ridge, following the next upwelling line east of the main line.

Again, at equator, the two lines merge into one.