Best 10 quotes of Charles H. Hapgood on MyQuotes

Charles H. Hapgood

  • By Anonym
    Charles H. Hapgood

    [I]n most cases the errors on the Piri Re'is Map are due to mistakes in the compilation of the world map, presumably in Alexandrian times, since it appears, as we shall see, that Piri Re'is could not have put them together at all. The component maps, coming from a far greater antiquity, were far more accurate. The Piri Re'is Map appears, therefore, to be evidence of a decline of science from remote antiquity to classical times.

  • By Anonym
    Charles H. Hapgood

    It appears that the charts must have originated with a people unknown; that they were passed on, perhaps by the Minoans (the Sea Kings of ancient Crete) and the Phoenicians, who were for a thousand years and more the greatest sailors of the ancient world. We have evidence that they were collected and studied in the great library of Alexandria and that compilations of them were made by the greographers who worked there.

  • By Anonym
    Charles H. Hapgood

    Most of these maps were of the Mediterranean and the Black Sea. But maps of other areas survived. These included maps of the Americas and maps of the Arctic and Antarctic seas. It becomes clear that the ancient voyagers traveled from pole to pole. Unbelievable as it may appear, the evidence nevertheless indicates that some ancient people explored the coasts of Antatica when its coasts were free of ice. It is clear, too, that they had an instrument of navigation for accurately finding the longitudes of places that was far superior to anything posessed by the peoples of ancient, medieval, or modern times until the second half of the 18th Century.

  • By Anonym
    Charles H. Hapgood

    The crust [of the earth] is very thin. Estimates of its thickness range from a minimum of about twenty to a maximum of about forty miles. The crust is made of comparatively rigid, crystalline rock, but it is fractured in many places, and does not have great strength. Immediately under the crust is a layer that is thought to be extremely weak, because it is, presumably, too hot to crystallize. Moreover, it is thought that pressure at that depth renders the rock extremely plastic, so that it will yield easily to pressures. The rock at that depth is supposed to have high viscosity; that is, it is fluid but very stiff, as tar may be. It is known that a viscous material will yield easily to a comparatively slight pressure exerted over a long period of time, even though it may act as a solid when subjected to a sudden pressure, such as an earthquake wave. If a gentle push is exerted horizontally on the earth's crust, to shove it in a given direction, and if the push is maintained steadily for a long time, it is highly probable that the crust willl be displaced over this plastic and viscous lower layer. The crust, in this case, will move as a single unit, the whole crust at the same time. This idea has nothing whatever to do with the much discussed theory of drifting continents, according to which the continents drifted separately, in different directions. [...] Let us visualize briefly the consequences of a displacement of the whole crustal shell of the earth. First, there will be the changes in latitude. Places on the earth's surface will change their distances from the equator. Some will be shifted nearer the equator, and others farther away. Points on opposite sides of the earth will move in opposite directions. For example, if New York should be moved 2,000 miles south, the Indian Ocean, diametrically opposite, would have to be shifted 2,000 miles north. [...] Naturally, climatic changes will be more or less proportionate to changes in latitude, and, because areas on opposite sides of the globe will be moving in opposite directions, some areas will be getting colder while others get hotter; some will be undergoing radical changes of climate, some mild changes of climate, and some no changes at all. Along with the climatic changes, there will be many other consequences of a displacement of the crust. Because of the slight flattening of the earth, there will be stretching and compressional effects to crack and fold the crust, possibly contributing to the formation of mountain ranges. there will be changes in sea level, and many other consequences.

  • By Anonym
    Charles H. Hapgood

    The evidence presented by the ancient maps appears to suggest the existence in remote times, before the rise of any of the known cultures, of a true civilization, of a comparatively advanced sort, which either was localized in one area but had worldwide commerce, or was, in a real sense, a worldwide culture. This culture, at least in some respects, may well have been more advanced than the civilizations of Egypt, Babylonia, Greece, and Rome. In astronomy, nautical science, mapmaking and possibly ship-building, it was perhaps more advanced than any state of culture before the 18th Century of the Christian Era. It was in the 18th Century that we first developed a practical means of finding longitude. It was in the 18th Century that we first accurately measured the circumference of the earth. Not until the 19th Century did we begin to send out ships for purposes of whaling or exploration into the Arctic or Antarctic Seas. The maps indicate that some ancient people may have done all these things.

  • By Anonym
    Charles H. Hapgood

    The Greek geographers of Alexandria, when they prepared their world map using the circumference of Eratosthenes, had in front of them source maps that had been drawn without the Eratosthenian error, that is, apparently without any discernible error at all. We shall see further evidence of this, evidence suggesting that the people who originated the maps possessed a more advanced science than that of the Greeks.

  • By Anonym
    Charles H. Hapgood

    The idea of the simple linear development of society from the culture of the paleolithic (Old Stone Age) through the successive stages of the neolithic (New Stone Age), Bronze, and Iron Ages must be given up. Today we find primitive cultures co-existing with advanced modern society on all the continents-the Bushmen of Australia, the Bushmen of South Africa, truly primitive peoples in South America, and in New Guinea; some tribal peoples in the United States. We shall now assume that, some 20,000 or more years ago, while paleolithic peoples held out in Europe, more advanced cultures existed elsewhere on the earth, and that we have inherited a part of what they once possessed, passed down from people to people.

  • By Anonym
    Charles H. Hapgood

    The most important evidence for the age of the maps [...] is to be found in those showing the Antarctic, especially in the maps of Mercator, Piri Re'is, and Oronteus Finaeus. All of these maps appear to show the continent at a time when there was a temperate climate there. Some geological evidence, in the form of three sedimentary cores from the bottom of the Ross Sea, has been presented to suggest that such a warm period may indeed have existed there down to about 6,000 years ago.

  • By Anonym
    Charles H. Hapgood

    We do not know whether [Hipparchus] drew maps--perhaps he did--but the truth is that in his day he could not possibly have applied his projections to the globe because the necessary data, in the form of correct findings of latitudes and longitudes of a very large number of places over the known areas of the earth, were not available. This was the weakness of all Greek cartographic science. In Greek times mathematics was in advance of mechanical instrumentation: There was no instrument for easily and correctly determining the longitude of places. However, the Piri Re'is and the other maps we went on to study, seemed to suggest that such an instrument or instruments had once existed, and had been used by people who knew very closely the correct size of the earth. Moreover, it looks as if this people had visited most of the earth. They seem to have been quite well acquainted with the Americas, and to have mapped the coasts of Antarctica.

  • By Anonym
    Charles H. Hapgood

    We have never solved the mystery of ice ages in the tropics, nor the equally strange mystery of the growth of corals and warm-climate flora in the polar zones. [...] It became obvious to me, as I reviewed these problems, and went back over the controversies that had marked their consideration, that a sort of common denominator was present. [...] [S]omebody usually tried to explain the particular problem in terms of changes in the position of the poles. This, I found, was the common denominator. The authors of such theories, unfortunately, were never able to prove their assumptions. The opponents of the notion of polar change always managed to point out fallacies that seemed decisive. At the same time, no one was able to reconcile all the evidence in the different fields with the idea that the poles have always been situated where they are now on the earth's surface. The theory here presented would solve these problems by supposing changes in the positions of the poles. Campbell has suggested that the changes have occurred not by reason of changes in the position of the earth's axis, but simply through a sliding of its crust.