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CONVERSION FACTORS

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DISTANCE BETWEEN MUNICH AND NEW DELHI

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DISTANCE BETWEEN BARCELONA AND MUNICH

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Schedule of the flights

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is an endorheic lake in the Himalayas situated at a height of about 4,350 m (14,270 ft). It is 134 km (83 mi) long and extends from India to China. Approximately 60% of the length of the lake lies in China. The lake is 5 km (3.1 mi) wide at its broadest point. All together it covers 604 km2.The lake is in the process of being identified under the Ramsar Convention as a wetland of international importance. This will be the first trans-boundary wetland in South Asia under the convention.

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A review of the aeolian sedimentary record of the Thar desert is presented. This includes a regional survey of the major dune forms, their genesis and their relationship to climate and other regional landforms. A key aspect of this work is the chronometry of the dunes using luminescence methods. Luminescence dating of sand has enabled quantification of the duration of the phases of sand aggradation and quiescence, time scales of dune migration and the dating of pedogenic carbonates.

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The perennial river Ganga takes birth in the great Himalayas and flows through the Northern Plains of India and empties into the Bay of Bengal. The rich alluvial deposits carried by the river over a vast period of time have shaped the Northern plains of India. The Ganga is associated with the legend of the sacrament carried out by King Bhagiratha to bring the heavenly river down to the earth. The Ganga has its source in the Gangotri glacier amidst the lofty Himalayas at a height of about 14000 feet above sea level. Bindu -Sar is near Gangotri and is referred to as the place where Bhagiratha is believed to have washed out his repentance of sins.

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The geology of the Himalaya is a record of the most dramatic and visible creations of modern plate tectonic forces.The Himalayas, are the result of an ongoing orogeny — the result of a collision between two continental tectonic plates. This immense mountain range was formed by tectonic forces and sculpted by weathering and erosion., the Himalayan system constitute the largest erosion system of the planet. It annually carries more than a billion tons of sediment and dissolved materials to the oceans, which corresponds to an erosion of of few millimeters per year. This transfer continental affects the environment at very different time scales. At geological timescales, Himalayan erosion contributes to the control of the long term carbon cycle through organic matter transport and burial.

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The Andaman Islands form an archipelago in the Bay of Bengal, just south of Burma. Altogether, the archipelago numbers about 300 islands, most of which comprise a territory of India. The islands are mountainous with dense rain forests. The islands also feature two volcanoes, the Narcondam and the Barren Island volcano. The Barren Island is the only historically active volcano in India.

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Andaman  and Nicobar Island is a island arc complex. Island arcs are formed by collision of 2 oceanic lithosphere. In the above case the Indian plate collided with the Burmese plate. About 100 million years ago(Cretaceous) the Indian plate broke off from Gondwana and started moving Northward and it encountered the Burmese plate and as the subduction occured between the to plates the islands started rising.