Aldan Highlands
The Aldan Highlands, or Aldan Plateau (; ) are a mountainous area in the Sakha Republic, Far Eastern Federal District, Russia. Aldan town and Tommot are located in the northern area of the highlands and Chulman in the south. The Olyokma Nature Reserve is a protected area located on the northwestern side, partly within the neighboring Lena Plateau. History. The area of the Aldan and the Yudoma-Maya highlands, between the basins of the Aldan River and the Yudoma, was uncharted territory well until the 1930s. It was first surveyed in 1934 by geologist Yuri Bilibin (1901—1952) together with mining  engineer Evgeny Bobin (1897—1941) in the course of an expedition sent by the government of the USSR. Bilibin and Bobin made a thorough topographic survey of the mountainous region leading separate research parties. Geography. The Aldan Highlands are located at the southern end of the Sakha Republic, between the Aldan River and the Uchur River, a right tributary of the Aldan. The Aldan partly crosses the uplands in the north, in the same manner as the Amga River in the west. The highlands are limited by the Stanovoy Range to the southwest, and by its Toko-Stanovik subrange to the  south and southeast. In the west the Olyokma River marks the limit, beyond which lies the Olyokma-Chara Plateau. The Dzhugdzhur Range rises to the east of the highlands. The highest point of the Aldan Highlands is Mount Ningam (Гора Нингам), a high peak located in the southern part, rising above the basin of the Gonam River, a left tributary of the Uchur. The same mountain is high according to other sources. Subranges. The system of the Aldan Highlands comprises a number of subranges where mountains are generally of middle height and their relief usually smooth. The highest point is  an unnamed summit. The ranges within the uplands include the following: Hydrography. Besides the Aldan and the Amga, the rivers of the highlands include the Buotama, the Amedichi, the Elkon, the Ulu, the Bolshoy Nimnyr, the Yungyuele, the Timpton and the Tuolba. Geology. The highlands are composed of Archean crystalline slates and gneisses. The Aldan Highlands coincide geographically with the Aldan Shield, a geological region that is an exposed part of the Siberian Craton. Together with the Anabar Shield further to the northwest, the Aldan Shield is one of the main features of the craton. Flora. The mountains of the  highlands are covered by larch taiga up to elevations between 1,100 and 1,300 m and by rocky tundra at higher altitudes.