{{Short description|Mountain range in Zabaykalsky Krai and Amur Oblast, Russia}} {{Infobox mountain |name= Kalar Range<br>Каларский хребет |image= Виден один из притоков Калара - panoramio.jpg |image_caption= One of the right tributaries of the Kalar river |image_size= |country=Russia |region_type=Federal subject |region=Zabaykalsky Krai / Amur Oblast |parent=Stanovoy Highlands<br>South Siberian System |borders_on= |highest=Skalisty Golets |elevation_m=2520 |coordinates = {{coord|56|24|01|N|119|05|04|E|display=inline|name=Muyskiy Gigant}} |length_orientation = WSW / ENE |length_km=350 |width_km=70 |area_km2= |range_coordinates = {{coord|56|20|N|118|0|E|type:mountain|format=dms|display=inline,title}} |geology=Granite, metamorphic rock |age= Early Archean and Proterozoic |orogeny= |map=Russia Zabaykalsky Krai |map_size= |map_caption= Location in Zabaykalsky Krai }} The '''Kalar Range''' ({{langx|ru|Каларский хребет|translit=Kalarskiy khrebet}}) is a mountain range in Zabaykalsky Krai and the NW end of Amur Oblast, Russian Federation. The highest point of the range is {{convert|2520|m|abbr=on}} high Skalisty Golets.<ref>M. Murzaev (ed.), ''USSR Survey of Northeastern China'', p. 68</ref><ref name="ETB">{{cite web |title=Каларский хребет|publisher=Энциклопедия Забайкалья |language=Russian |trans-title=Kalar Range|url=http://ez.chita.ru/encycl/concepts/?id=2463|accessdate=17 September 2021}} {{in lang|ru}}</ref><ref name="GЕ">Google Earth</ref>

The range is part of the '''Udokan Ore Region''' that includes the Kodar and Udokan ranges.<ref name="ЭСБЕ2">[http://bse.sci-lib.com/article113643.html Udokan Ore Region] / ''Great Soviet Encyclopedia:'' in 30 vols. / Ch. ed. A.M. Prokhorov. - 3rd ed. - M. Soviet Encyclopedia, 1969-1978.</ref>

==History== Located in a desolate area, the Kalar Range was first described and roughly put on the map in 1857 by A.F. Usoltsev, Lieutenant of the Corps of Military Topographers of the Russian Imperial Army. Usoltsev sighted the range from the right bank of the Kalar River.<ref>Obruchev V. A., [https://agesmystery.ru/rubriki/ekspedicii-naxodki-i-sokrovishha/shvarc-na-yugo-vostoke-sibiri/ Шварц на юго-востоке Сибири (Schwartz in the southeast of Siberia)] {{Webarchive|url=https://web.archive.org/web/20201127164342/https://agesmystery.ru/rubriki/ekspedicii-naxodki-i-sokrovishha/shvarc-na-yugo-vostoke-sibiri/ |date=2020-11-27 }} (in Russian)</ref>

==Geography== The Kalar Range belongs to the Stanovoy Highlands. It stretches from WSW to ENE for roughly {{convert|350|km|abbr=on}} from the Vitim river valley to the Olyokma, both right tributaries of the Lena. To the north it borders the Chara depression —in the upper reaches of the Chara river, and the western spurs of the Udokan Range. To the south the range is bound by the valley of the Kalar river, a right tributary of the Vitim, which separates it from the Yankan Range. While peaks in the western part are generally flat-topped, the eastern end has a more marked alpine relief.<ref name="STM">{{cite web|url=https://maps.vlasenko.net/smtm1000/n-49.jpg|title=N-49 Chart (in Russian)|access-date=5 September 2021}}</ref>

===Hydrography=== A number of rivers have their sources in the range, including the Kalar river, with its right tributaries Katugin, Chukundu and Bugungda. Also the right tributaries of the Vitim river, Taksima and Kuanda, the left tributaries of the Olyokma, Tas-Yuryakh and Imangra, as well as several right tributaries of the Chara, also a left tributary of the Olyokma. River Nyukzha flows across the range in its eastern part.<ref name="ETB"/>

==Flora== The higher slopes of the range are mainly covered with sparse coniferous forest, while below {{convert|1100|m|abbr=on}} to {{convert|1400|m|abbr=on}} mountain larch taiga predominates.<ref name="ETB"/>

==See also== *Baikal Rift Zone *List of mountains and hills of Russia

==References== {{Reflist}}

Category:Stanovoy Highlands Category:Mountain ranges of Russia Category:Mountain ranges of Amur Oblast Category:Mountains of Zabaykalsky Krai

{{ZabaykalskyKrai-geo-stub}} {{AmurOblast-geo-stub}}