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L'antarctique Est La Patrie Originelle Des Dieux.Pdf !"#$%&'()*')' $+$*,'* - ! ! ". ! / 0 ! - 1 +%. ! " " %+,*2. - 30 1 3 )*)* " . ! / 0 ! - 1 SOMMAIRE Partie I. MYSTÈRE DU CONTINENT SUD ............................. 3 Chapitre 1 : Antarctique - Continent austral .................................. 3 Chapitre 2 : Le continent austral sur les anciennes cartes. ............ 9 Chapitre 3 : Le déplacement des pôles ?...................................... 31 Chapitre 4. Le mythe du labourage de l'océan et son parallèle ... 68 Partie II. LES CIVILISATIONS DE L'ANTARCTIQUE ...... 132 Chapitre 5. Les empreintes du dieu Virakochi .......................... 132 Chapitre 6. La malédiction du sage Durvas. .............................. 151 Chapitre 7. Jambudvipa, Potala, Lanka. .................................... 158 Chapitre 8 : Tamililam, Taprobana et Panhaya. ........................ 167 Chapitre 9. Dilmun est la maison des dieux. ............................. 181 Chapitre 10. Les dieux sur les chars ailés... ............................... 197 PartieIII ARTEFACTS D'ANTARCTUS ................................ 208 Chapitre 11. Les villes de l'Antarctique ..................................... 208 Chapitre 12. Pyramides et anomalies d'Antactica ..................... 223 Chapitre 13. Ce qui a été trouvé sur l'île de Kerguelen ............. 233 Partie IV. MYSTÈRE DE LA TERRE DE HONNÉVILLE .. 250 Chapitre 14. Où est passé de Honneville ? ................................ 250 Chapitre 15. Et encore, les Templiers et leur flotte ................... 255 Chapitre 16. Le pays de Yoda Kozma Indikoplov .................... 297 Chapitre 17. "Mauvais" voyage de Bouvais. ............................. 320 Chapitre 18. Pacifida comme une colonie de l'Antarctique. ..... 331 1 2 Partie I. MYSTÈRE DU CONTINENT SUD Chapitre 1 : Antarctique - Continent austral L'Antarctique (en face de l'Arctique) est le continent méridional de la Terre, avec une altitude moyenne en surface de plus de 2 000 m au-dessus du niveau de la mer et une altitude centrale de 4 000 m au-dessus du niveau de la mer. La majeure partie de cette altitude est constituée d'une couverture de glace permanente, sous laquelle se cache le relief continental et dont seulement 5 % environ de la superficie est libre de glace - principalement dans l'Antarctique occidental et les montagnes transantarctiques : îles, parties de la côte, "vallées sèches" et crêtes et pics montagneux individuels (nunataki) s'élevant au-dessus de la surface de la glace. Les montagnes transantarctiques, qui traversent presque tout le continent, divisent l'Antarctique en deux parties, l'Ouest et l'Est, avec des origines et une structure géologique différentes. À l'est, il y a un haut plateau (la plus haute élévation de la surface de la glace à environ 4 100 mètres au-dessus du niveau de la mer) couvert de glace. La partie occidentale est constituée d'un groupe d'îles montagneuses reliées entre elles par la glace. Sur la côte Pacifique se trouvent les Andes antarctiques, dont la hauteur dépasse 4 000 mètres ; le point culminant du continent - 4 892 mètres au-dessus du niveau de la mer - est le massif de la crête Vinson Sentinel Ridge. L'Antarctique occidental possède également la plus profonde dépression du continent, la dépression de Bentley, probablement d'origine rift. Sa profondeur, remplie de glace, atteint 2 555 mètres sous le niveau de la mer. La couverture de glace de l'Antarctique a maintenant une épaisseur moyenne de 1 720 mètres. On a constaté que cette couverture de glace du continent était progressive. Les scientifiques estiment qu'elle a commencé il y a 35 millions d'années, en commençant par l'immense partie orientale du continent, et s'est achevée en l'an 4000 avant Jésus-Christ. quand le glacier a rampé à jamais jusqu'aux derniers mètres de terre à la pointe ouest dans les régions de la Terre de la Reine Maud et de la péninsule Antarctique. 3 On a l'impression que l'Antarctique est entièrement recouvert de neige et de glace. Mais ce n'est pas tout à fait juste. Oui, seuls 5% de l'ensemble du continent sont exempts de neige et de glace, mais ils représentent environ 2,5x105 km2. En règle générale, près des bords du continent, une partie importante d'entre eux se trouve à proximité des stations russes Mirny et Novolazarevskaya, ainsi que le long des montagnes Trans-Antarctiques, qui, en tant que prolongement des montagnes andines d'Amérique latine, est comme une crête dorsale du continent, s'étendant du cap Ader, au sud de la Nouvelle-Zélande, le long de la côte occidentale de la mer de Ross et traversant presque tout le continent. Les plus grandes zones libres de glace (4 000 km2) ont été trouvées dans les montagnes transantarctiques - "Oasis McMurdo" et "Dry Valley Area", près des stations néo-zélandaise et américaine. La topographie de ces vallées libres de glace est l'une des plus belles de la Terre. L'oasis de McMurdo est constituée de trois vallées profondes et libres de glace, chacune d'une longueur de près de 100 km et d'une largeur de 2 à 5 km, qui se trouvaient autrefois également sous le glacier, comme en témoignent les moraines laissées par le glacier. Au fond des vallées, il y a des lacs qui gèlent pendant la majeure partie de l'année, sauf pendant une courte période en été. Au-dessus des vallées, il y a des pics abrupts de 2 000 à 3 000 m de haut, la plupart d'entre eux étant libres de glace. De hautes vallées entre ces sommets, de petits glaciers descendent les pentes. A certains endroits, ils se déplacent au fond des vallées. Les vallées sont parsemées de dunes de grottes et d'affleurements rocheux dont la couleur est nuancée de brun - du granit brun clair et longiligne en suspension dans l'air au basalte rouge foncé. Les pierres individuelles ont des nuances de gris. Ces couleurs contrastent avec le blanc 4 des glaciers et un ciel bleu vif. En raison du manque de végétation, il n'y a pas de vert. Des zones similaires de terres libres avec de petits lacs et de petites hauteurs se trouvent dans les zones côtières de l'oasis de Banger, près de la gare de Mirny. Les "Dry Valleys" se trouvent à l'ouest de la vallée de McMurdo et sont nommées ainsi en raison de leur humidité extrêmement faible et de l'absence de couverture de neige et de glace, car l'humidité s'évapore des vents les plus puissants, atteignant des vitesses de 320 km/h. Dans certaines régions de cette zone, il pleut depuis deux millions d'années. Les scientifiques pensent que les Dry Valleys ressemblent plus à Mars qu'à tout autre environnement terrestre, c'est pourquoi des astronautes de la NASA y sont souvent formés. Sur leur territoire, les astronautes américains ont été formés avant de se poser sur la lune en 1969. Le sol de l'Antarctique est propice à la culture. Elle possède des réserves de minéraux non vitreux et partiellement altérés qui augmentent la fertilité. Des expériences ont montré que le sol de l'Antarctique transféré à des températures normales est propice à la croissance des plantes. On y cultive même de la salade ou des radis. L'Antarctique est également associé à une découverte majeure dans le domaine de l'océanologie. Il s'est avéré que le continent de glace est au centre d'un gigantesque tourbillon océanique (courant circumpolaire antarctique), qui est plusieurs fois plus puissant que le Gulf Stream et le Kurosivo réunis. On pense que les forces qui soutiennent ce tourbillon mondial sont les vents d'ouest qui dominent ces latitudes (ce qu'on appelle la dérive des vents d'ouest). Ici, l'eau se déplace dans le sens des aiguilles d'une montre, d'ouest en est, entre 40° et 50°S. (les "quarantièmes rugissants"), jusqu'à 30 000 km de long et jusqu'à 1 000 km de large, avec une épaisseur de 4 à 5 km (dans certaines régions, le flux comprend toute la masse d'eau jusqu'au fond de l'océan ; la température de l'eau dans la couche supérieure varie de 12-15° C dans la partie nord à 1-2° C dans la partie sud du courant ; dans la couche superficielle de l'eau de l'océan, la vitesse du courant varie de 0,4 à 0,9 km/h, dans la couche profonde, elle atteint 0,4 km/h). Les branches du courant sont : dans l'océan Atlantique, le courant des Malouines ; le courant de Bengel (qui apparaît au sud du cap de Bonne- Espérance et se dirige vers le nord, atteignant la zone de la Namibie en Afrique) ; dans l'océan Indien, le courant d'Australie occidentale ; et dans le Pacifique, le courant du Pérou. Les eaux baignées par l'Antarctique sont appelées l'océan Austral (ou Antarctique), qui n'a pas d'îles et de continents clairement délimités à la frontière nord (acceptée comme le 60e degré de latitude sud) et se compose de 13 mers. Les scientifiques n'ont pas encore déterminé de façon définitive si ce nom doit être appliqué à toutes les cartes géographiques : l'océan Austral a été délimité pour la première fois en 1650 par le géographe néerlandais Benhard Warenius et comprenait à la fois le "continent austral" 5 non encore découvert par les Européens et toutes les zones situées au-dessus du cercle polaire sud ; la Royal Geographical Society à Londres à partir de 1845. Dans les publications de l'Organisation hydrographique internationale, l'océan Austral a été séparé de l'océan Atlantique, de l'océan Indien et de l'océan Pacifique en 1937 ; dans la tradition soviétique (1969), la limite approximative de l'"océan Austral" conditionnel était considérée comme la zone de convergence de l'Antarctique (la limite septentrionale des eaux de surface de l'Antarctique), près de 55° de latitude sud. Dans d'autres pays, la frontière est également floue - la latitude au sud du Cap Horn, la limite des glaces flottantes, la zone de la Convention de l'Antarctique (une zone au sud du 60e parallèle de latitude sud) ; le gouvernement australien considère l'"océan Austral" comme une eau située directement au sud du continent australien.
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