Who Built the Moon?

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Book: Who Built the Moon? Read Online Free PDF
Author: Christopher Knight
they were fond of ‘wheels within wheels’. If the circle of the heavens had 366 parts, why should every circle not follow the same rule? We were able to confirm this hypothesis by a variety of means including evidence from later cultures that appear to have adopted the 366-degree principle.
    The approach our Megalithic ancestors took, we argue, was to hypothetically divide the circle of the Earth into 366 degrees with sixty minutes per degree and six seconds per minute. It was reasonable to assume that these ancient builders used the polar circumference of the Earth that passed through the area around the British Isles. Our planet is nearly spherical but it does have a bulge in the centre between the poles, so the equatorial circumference is a little longer that the polar. There are varying estimations of the Earth’s polar circumference, with NASA, for example, quoting an average figure of 39,941km, whilst other sources regularly quote 40,006km or 40,010km – but the most frequently used figure appears to be 40,008km. Undoubtedly much depends on where the measurement is taken or if an average of them all is calculated.
    Interestingly, the shortest polar circumference (one that has least landmass) is the one that passes through the British Isles and is now considered as the zero line of longitude.
    But there is also another possibility.
    Just for interest, we looked at the flattest possible circumference achievable on the globe, i.e. a line that equally bisects the planet that has most sea and least land. We were amazed to discover that a person standing in the middle of Salisbury Plain in Wiltshire, England (where Stonehenge and the Megalithic circle at Avebury were built) is in the absolute centre of such a line. This means that if we consider Stonehenge to be the ‘top’ of the world, the imaginary equator from that point is almost 98per cent sea – more than any other point on Earth. This line passes across the South Atlantic, skims just below Africa, moves up across the Indian Ocean, clips small pieces of land at Banda Aceh, Sumatra, Thailand and Vietnam, over the South China Sea and then more than 20,000 kilometres across the Pacific to pass over a section of South America.
    As far as we know such a line has not been measured, and we cannot imagine how it could have been measured without the aid of modern satellite technology. However, just because we do not know how it could have been done does not mean that it was not done. Without further evidence we have to assume that it is pure coincidence that Stonehenge stands on the only place on Earth to be equidistant from the optimum and near perfect sea-level circumference of the globe.
    We can only assume that a polar circumference was used and taking the 40,008km figure it translates to 48,221,838 Megalithic Yards using Thom’s central value for the unit. It was then subdivided as follows:
    Polar circumference = 48,221,838 MY
    1 Degree (1/366th) = 131,754 MY
    1 Minute (1/60th) = 2,196 MY
    1 Second (1/6th) = 366 MY
    So, this brilliant system of geometry starts with 366 degrees and finishes with seconds of arc that are 366 Megalithic Yards long. Self- evidently, an amazing set of ‘wheels within wheels’!
    We knew that the system must work this way because we found that the later Minoan culture, which developed on the Mediterranean island of Crete around 2000 BC, also used the Megalithic second of arc. However, the Minoans sub-divided it into 1,000 parts to become their standard unit of measure that was equal to 30.36cm. This unit was dubbed the ‘Minoan Foot’ by the Canadian archaeologist, Professor Joseph Graham who first detected its use in the palaces of ancient Crete. 6
    We went on to demonstrate how any person could generate a highly accurate Megalithic Yard by measuring the movement of Venus in the evening sky using a rope, some twine, a blob of clay, and a few sticks. The secret was to take one 366 th part of the horizon and time the passage of Venus
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