Page 96 - Fingerprints of the Gods by Graham Hancock
P. 96

Graham Hancock – FINGERPRINTS OF THE GODS



                      the temporary increase in the level of the lake may have been caused in part by
                      the breaking  of  the bulwarks on some of  the lakes further  to  the north and
                      situated at a greater altitude ... thus releasing the waters which descended toward
                      Lake Titicaca in onrushing and unrestrainable torrents.
                                                                           9
                   Posnansky’s evidence that a flood had been the agent of the destruction
                   of Tiahuanaco included

                      The discovery of lacustrine flora,  Paludestrina culminea,  and  Paludestrina
                      andecola, Ancylus titicacensis, Planorbis titicacensis, etc., mixed in the alluvia with
                      the skeletons of human beings who perished in the cataclysm ... and the discovery
                      of various skeletons of  Orestias,  fish of  the family of the  present  bogas,  in the
                      same alluvia which contain the human remains ...
                                                                      10
                   In addition,  fragments of human and animal skeletons had been found
                   lying
                      in chaotic disorder among wrought stones, utensils, tools and an endless variety
                      of other things. All of this has been moved, broken and accumulated in a confused
                      heap. Anyone who would dig a trench here two metres deep could not deny that
                      the destructive force  of  water, in combination  with brusque movements  of  the
                      earth, must have accumulated those different kinds of bones, mixing them with
                      pottery, jewels, tools and utensils ... Layers of alluvium cover the whole field of the
                      ruins and lacustrine sand  mixed  with shells from  Titicaca, decomposed feldspar
                      and volcanic ashes have accumulated in the places surrounded by walls ...
                                                                                              11
                   It had been a terrible catastrophe indeed that had overwhelmed
                   Tiahuanaco. And if Posnansky was right, it took place more than 12,000
                   years ago. Thereafter, though the flood waters subsided, ‘the culture of
                   the Altiplano did not again attain a  high point of development but fell
                   rather into a total and definitive decadence’.
                                                                       12


                   Struggle and abandonment

                   This process was hastened by the fact that the earthquakes which had
                   caused Lake Titicaca to engulf Tiahuanaco were only the first of many
                   upheavals in the area. These initially  resulted in the lake swelling and
                   overflowing its banks but they soon  began to have the opposite effect,
                   slowly reducing Titicaca’s depth and surface area. As the years passed,
                   the lake continued to drain inch  by inch,  marooning the great city,
                   remorselessly separating it from the waters which had previously played
                   such a vital role in its economic life.
                     At the same time, there was evidence that the climate of the Tihuanaco
                   area had become colder and much  less favourable for the growing of
                   crops than had previously been the case,  so much less favourable that
                                                                    13

                   9  Tiahuanacu, I, p. 55.
                   10  Ibid., I, p. 39.
                     Ibid., III, pp. 142-3.
                   11
                   12  Ibid., I, p. 57.
                   13  Ibid., I, p. 56, and II, p. 96.


                                                                                                      94
   91   92   93   94   95   96   97   98   99   100   101