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The book is divided into 20 chapters that cover the emergence of the mountains from the Tethys Sea, the role of the Himalayas in the Puranas, the exploits of British explorers, the Sino-Indian War, and the recent tensions surrounding Sherpa labor and mountaineering on Mount Everest. [1]
The Himalayas here are becoming increasingly rugged, with heavily forested steep valleys. The Himalayas continue, turning slightly northeast, through the Indian State of Arunachal Pradesh as well as Tibet, before reaching their easterly conclusion in the peak of Namche Barwa, situated in Tibet, inside the great bend of the Yarlang Tsangpo river
The Himalayas border the Indo-Gangetic Plain to the south, Pamir Mountains to the west in Central Asia, and the Hengduan Mountains to the east on the China–Myanmar border. From east to west the Himalayas are divided into 3 regions, Eastern Himalaya, Central Himalaya, and Western Himalaya, which collectively house several nations and states.
The origin of the Tibeto-Burman speakers was located in the upper course of Yangtse and the Haong Ho (Yellow) rivers in North West China. [ 2 ] [ 3 ] [ 4 ] Population
The Limbu follow the social rules and regulation of Mundhum oral 'scripture' and a religious book. [18] Their religion is known as Kiratism. Traditionally, the Limbu bury their dead, but due to the influence of Hinduism, cremation is becoming popular. Limbu people follow Kirat religion. Some limbu have converted to Christianity.
Enayat Ahmad (1 August 1923 – 10 December 1999) was an Indian geographer known for his contribution to the study of the geography of India, especially his interpretation of the evolution of drainage systems in the Himalayas and his writings on tropical coastal geomorphology.
The Alpine orogeny is caused by the continents Africa, Arabia and India and the small Cimmerian Plate colliding (from the south) with Eurasia in the north. Convergent movements between the tectonic plates (the African Plate, the Arabian Plate and the Indian Plate from the south, the Eurasian Plate and the Anatolian Sub-Plate from the north, and many smaller plates and microplates) had already ...
Due to continental drift, the India Plate split from Madagascar and collided with the Eurasian Plate resulting in the formation of the Himalayas.. The earliest phase of tectonic evolution was marked by the cooling and solidification of the upper crust of the earth's surface in the Archaean Era (prior to 2.5 billion years) which is represented by the exposure of gneisses and granites especially ...