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Exploring Geographic and Geometric Relationships Along a Line of Ancient Sites Around the World (cont)
By Jim Alison
Many similarities between these sites have been well documented, including the use of perfectly cut and precisely placed monolithic stones, exact orientations to the cardinal points and astronomical orientations. The prevailing view of world history dismisses these similarities as coincidental developments of separate stone age cultures. Unless it is also a coincidence that these sites are located at mathematically and geometrically significant points on a single line around the center of the Earth, it may be time to reconsider the idea that Europeans of the present era were the first to know the size and shape of the Earth.
If the locations of all of these sites is not a coincidence, and if there are sites yet to be discovered along the line, one good place to look might be halfway between the Great Pyramid and Machupicchu, just south of the Cape Verde Islands.
Another good place to look might be halfway between the Great Pyramid and Easter Island, at 4° 19' North Latitude, 41° 30' West Longitude, also under the North Atlantic Ocean:
The distance from the Great Pyramid to Easter Island is approximately 40% of the circumference of the Earth. The X in the diagram is halfway between the two, 20% each way. Machupicchu is halfway between the X in the diagram and Easter Island, 10% each way. The Distance from the Great Pyramid to Angkor Wat is approximately 20% of the circumference, and the Indus Valley is halfway between the two, 10% each way. The Distance from Easter Island to Angkor Wat is approximately 40% of the circumference, and Anatom Island is halfway between them, 20% each way. These sites are located in multiples of 10% of the circumference of the Earth, and particularly at 20% intervals. Although there are no islands near the location of the X in the diagram, it is interesting to note that the famous Piri Reis map shows a large island in this location, and the geology of recent core samples, taken from the ocean floor in this area, is of continental rather than oceanic type rock.
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