The Aravalli range also forms the main watershed for north India, channelling the drainage of that part of northern India into the Arabian Sea and the Bay of Bengal. The Luni river system rising from the western slopes of the Aravalli Range (near Ajmer) flows through the semi-arid transitional plains into the Rann of Kutch and Arabian Sea, while the Banas and other streams, rising from the eastern slopes of the Aravallis, join the Chambal. The Chambal, in turn, flows into the Yamuna-Ganga river system which drains into the Bay of Bengal. The main watercourses like the Banas, Sabarmati, etc. and the tributaries of the Luni, are more or less parallel to the Aravalli Range, one group flowing to the northeast and the other towards the southwest. The northwestern slopes of the Aravalli Range are influenced by the blown sands of the Thar desert, which has almost choked the drainage channels. Only seasonal streams feed the drainage of the Luni river. The Luni has several tributaries- mo
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