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The Chersky Range (Russian: Хребет Черского, Yakut: Черскэй хайалара, romanized: Cerskey qayalara) is a chain of mountains in northeastern Siberia between the Yana and Indigirka Rivers.
River Karenga, another tributary of the Vitim, separates the Chersky Range from the Yablonoi Mountains, which run roughly parallel to it. The highest point of the range is 1,644 meters (5,394 ft) high Golets Chingikhan (Голец Чингикан), a ‘’golets’’ -type of mountain with a bald peak, located in the central part.
Mount Chersky (Russian: Гора Черского) is a mountain in the Baikal Range, Russian Federation. This peak is named after Lithuanian explorer Jan Czerski (1845 - 1892, Ivan Chersky transcribed from Russian), who greatly contributed to the study of Lake Baikal .
Chersky Peak (Russian: Пик Черского; Buryat: Хара-Болдог) is a mountain in the Komarinsky Range, Khamar-Daban, Russian Federation. This peak is named after Polish explorer Jan Czerski (1845–1892), who greatly contributed to the study of neighboring Lake Baikal.
Highest peak of the Altai Mountains Tebulosmta [22] Тебулосмта 4493 m 14,741 ft: 2145 m 7,037 ft: 66.1 km 41.1 mi Greater Caucasus Chechnya [a] Highest mountain of Chechenya Sugan [23] Суган 4487 m 14,721 ft: 1161 m 3,809 ft: 18.61 km
The area of the East Siberian Mountains has a very low population density. [1] The territory of the mountain system is one of the Great Russian Regions. In some areas of the East Siberian Mountains, such as the Kisilyakh Range and the Oymyakon Plateau there are kigilyakhs, the rock formations that are highly valued in the culture of the Yakuts. [2]
Mount Shahdagh (Azerbaijani: Şahdağ; Lezgian: Кас сув) is a mountain peak of the Greater Caucasus range, located in the Qusar District of Azerbaijan, close to the border with Russia. The elevation of the peak is 4,243 metres (13,921 ft) above sea level. [1] Among the earth rocks found in Shahdagh are magnesian lime, chalkstone and ...
The mountains were formed by folding, and represent an anticline. [2] The Verkhoyansk Range was covered by glaciers during the Last Glacial Period and the mountains in the northern section, such as the Orulgan Range, display a typical Alpine relief. There are coal, silver, lead, tin, and zinc deposits in the mountains.