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ATLANTIS & the Atlantic Ocean 1 (ORIGINAL)

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Bianca
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« Reply #30 on: December 22, 2007, 05:18:49 pm »








dhill757

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   posted 08-12-2004 02:03 AM                       
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"For example, the midway point between the Great Pyramid and Machupicchu is in the North Atlantic Ocean, approximately one degree south of the Cape Verde Islands. This is also the midway point between Easter Island and the Indus Valley. Although the Cape Verde Islands were found to be uninhabited when they were rediscovered in 1460 A.D., maps and geographical descriptions for the past 2000 years have shown this location to be the home of ancient island civilizations, including maps showing this location to be the site of Atlantis. In Plato's account of Atlantis, there was a mountainous region north of the city. Are the higher elevations of those mountains now the Cape Verde Islands?
"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:


quote:
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Geological structure of the Strakhov fracture zone (equatorial segment of the Mid-Atlantic ridge)
G. B. Udintsev, A. F. Beresnev, V. M. Golod, A. V. Kol'tsova, N. A. Kurentsova, and M. V. Zakharov

Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences, Moscow

G. V. Agapova

Institute of Geology, Russian Academy of Sciences, Moscow

L. P. Volokitina

P. P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow

V. G. Udintsev

Shmidt Institute of Earth Physics, Russian Academy of Sciences, Moscow

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Abstract

Geological-geophysical data obtained during cruises 7, 11, and 12 of R/V Akademic Nikolay Strakhov (1989-1991) within the international project EQUARIDGE in the region of Strakhov fracture zone (4oN) are presented. The trough of the fracture is interpreted as an open extension joint, a graben produced by stretching along the axis of the Mid-Atlantic Ridge. Bedrock studies showed that the typical mid-oceanic tholeiitic basalts occur within the narrow (60 nm wide) axial rift zone, whereas igneous rocks not typical to the ocean were found on the eastern and western flank plateaus. This allows us to suppose that a reworked relict continental-type basement of pre-Upper Jurassic age possibly exists beneath the flank plateaus, within the segment under discussion. The above data correspond to the hypothesis by E. Bonatti about a nonspreading nature of the basement of Mid-Atlantic Ridge within the Equatorial segment and the Strakhov fracture zone.

Figures 3, Tables 3, References 22, Pages 544-558
Received December 16, 1993


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