Detailed structural analysis in the hinterland of Qilian Shan reveals four deformation phases since the Late Triassic. Structural geometry and kinematics are important to understand the growth of the Tibetan Plateau margins. The topographic margin of the plateau is coincident with a north-trending mountain range, the Min Shan… The climate is cool year-round so tourists can take Burma tour packages to the region at any time in the year. Shan State is located on the Shan plateau in the central eastern part of Myanmar (19° 17′ N and 24° 13′ N and 96° 10′ E and 101° 11′ E). The area is the primary source of Myanmar's sapphires, rubies and other gems, for which the country is known; it is also a principal source of lead, silver and zinc. The Liupan Shan separates the stable Ordos Block from the severely thrusted Longxi Block, which in turn is separated by the Western Qinling fault from the Tibetan Plateau (Fig. It killed more than 70 and injured more than 100 people. The Shan Plateau is the primary source of the nation’s sapphires, rubies and other gems. Shan Plateau, crystalline massif forming the eastern part of Myanmar (Burma) and forming part of the Indo-Malayan mountain system.The plateau is crossed by the deep trench of the Salween River in the east and is bordered by the upper course of the Irrawaddy River to the west. The Longmen Shan mountain range, site of the devastating 12 May 2008 Wenchuan ( M = 7.9) earthquake, defines the eastern margin of the Himalayan orogen and exhibits greater topographic relief than anywhere else in the Tibetan plateau. The West Burma Plate consists of Triassic–Recent rocks only and will not be considered further here, but Sibumasu … The Shan Plateau, in the Shan State of eastern Myanmar, is the primary source of the nation's sapphires, rubies and other gems for which Burma is famous. For an easy escape from the heat and hussle of Mandalay, do what the colonial Brits did and pop up to Pyin Oo Lwin. The dominant set consists of the NE‐trending, arcuate sinistral‐slip faults that occupy an area of 700‐by‐400 km and straddle neighboring regions of China, Myanmar, Laos, Thailand, and Vietnam. The Shan are the largest of the many national ethnic groups residing in the Union of Myanmar. 1989. Shan Plateau, crystalline massif forming the eastern part of Myanmar (Burma) and forming part of the Indo-Malayan mountain system. The Tian Shan are separated from the Tibetan Plateau by the Taklimakan Desert and the Tarim Basin to the south. The ranges in the area are aligned in such a way that they link to the foothills of the Himalayas further to the northwest. . After migrating from their early home in the Hwangho-Yangtze region of China, they settled in the eastern part of today's Myanmar, primarily in the Shan Plateau, around the first century AD. The Shan Hills (Burmese: ရှမ်းရိုးမ, Thai: ฉานโยมา; Shan Yoma), also known as Shan Highland, is a vast mountainous zone that extends through Yunnan to Myanmar and Thailand. [16], Owing to the insurgency and the activity of the Tatmadaw in the area many local people living in the mountainous areas of the Shan Hills moved across the border to Thailand where they live in refugee camps. It is characterized by large variations of elevation over short distances (up to 1800 m over a few kilometers). 2014).The … The name of the massif or system of ranges, is derived from the Shan State and its peoples, said in its turn to be derived from the word "Siam",[4] that occupies most of the Shan Highland area. The plateau is the country’s principal source of lead, zinc, and silver and is an area of major teak forests. With the uplift of the Tian Shan and Pamir Plateau, a significant positive anomaly of geopotential height and warming appeared in the west and north of the Tian Shan Mountains–Pamir Plateau and extended to arid subtropical Asia . Located at an elevation in excess of 1000 m a.s.l., it is largely made up of Paleozoic and Mesozoic carbonate, including a larger part of secondary dolomite. It includes both high relief mountains and relatively low relief upland landscapes. Let us know if you have suggestions to improve this article (requires login). THE Tien Shan-a high, seismically active intracontinental mountain belt, 1,000-2,000 km north of the Himalaya-has grown as a result of India's collision with Asia 1 . [9] Karstic ranges are common, for large tracts of the hills are limestone. 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