By René Létolle

ISBN-10: 2296077196

ISBN-13: 9782296077195

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Additional resources for La mer d'Aral : Entre désastre écologique et renaissance

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FJisamment l'Aral vers l'Ouzboy. le passage vers le Sary Kamysh. se remplit. s'accentue vers l'ouest, se rétrécit à la baie Soudotche, l'Amou largement et restreint se déverse presque le Daryalyk l'essentiel entièrement (déversoir de l'Amou vers l'ouest) y creuse son va vers l'Aral. vers l'ouest, l'Ouzboy fonctionne, que l'eau du fiyr. vers le Sary Kamysh actuel: mais son delta, prélèvements: ne reçoit pratiquement déborde vers le nord et l'ouest du delta de l'Amou du fiyr et de l'Aral VI: creuse lafosse le Sary Kamysh progresse lit.

Ailleurs, il s'agit de dépôts sédimentaires, galets et sables, à pente plus marquée, avec parfois des restes de sol subaériens : rubéfaction, traces de racines ete. La plus haute terrasse se trouve à l'altitude 50 de 72 m. Très dégradée, longtemps discutée, son existence ne fait plus de doute maintenant. Voyons de plus près ces possibilités d'extension. 25 m de tranche d'eau, ce qui paraît raisonnable en moyenne, on peut atteindre au maximum 70 plus ou moins 5 m, précisément le niveau auquel se place la terrasse supérieure.

39 Plus à l'Est, un golfe dépendant de la grande Mer, ne dépassait guère 22m de profondeur et est donc complètement émergé aujourd'hui. Il était séparé de la terre ferme par une grande île de 50km sur 10 km (BarsakelmesI2), de même constitution géologique que l'île Vozrojdenie ou que la rive de l'Oust Ourt à l'ouest, et également bordée sur la quasi totalité de son périmètre par une falaise d'une cinquantaine de mètres de hauteur. Barsakelmes apparaît maintenant comme un plateau étendu, très peu ondulé, bordé de falaises identiques à celles de l'Oust Ourt, et couvert d'herbes.

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La mer d'Aral : Entre désastre écologique et renaissance by René Létolle

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