Stanovik Range
{{short description|Mountain range in Russia}}
{{About||other meanings|Stanovik (disambiguation){{!}}Stanovik}}
{{Infobox mountain
| name=Stanovik Range
| other_name=Становик
| photo=USSR map NM 49-8 Kyra.jpg
| photo_caption=Map of the area with part of the Stanovik in the right.
| country= Russia
| subdivision2_type=Krai
| subdivision2= Zabaykalsky Krai
| parent= Khentei-Daur Highlands
| highest=Unnamed
| elevation_m= 1916
| coordinates=
| area_km2=
| range_coordinates= {{coord|50|0|N|112|12|E|type:mountain|format=dms|display=inline,title}}
| range_coordinates_ref=
| geology= Volcanic rock and granodiorite
| age= Jurassic
| orogeny=Alpine orogeny
| map=Russia Zabaykalsky Krai
| map_caption=Location in the Transbaikal region
| length_km= 110
| length_orientation= NE/SW
| width_km= 40 - 70
| width_orientation=SE/NW
| easiest_route = From Mordoy or Kyra
}}
The Stanovik ({{langx|ru|Становик}}) is a mountain range in the Transbaikal Region (Zabaykalsky Krai) of Siberia, Russia.{{cite web |title=Становик, хребет |publisher=Энциклопедия Забайкалья |language=Russian |trans-title=Stanovik Range |url=http://ez.chita.ru/encycl/concepts/?id=2614|accessdate=1 November 2021}} The southern end of the range is very close to the border with Mongolia. The nearest village is Mordoy (Мордой), Kyrinsky District.
The range is part of the Trans-Baikal conifer forests ecoregion.{{cite web|title=Sokhondinskiy Biosphere Reserve|url=http://www.unesco.org/mabdb/br/brdir/directory/biores.asp?mode=gen&code=RUS+10|publisher=UNESCO|accessdate=4 February 2020}}
Geography
The Stanovik Range is part of the Khentei-Daur Highlands, South Siberian System. It rises on the left bank of the upper course of the Onon River and stretches roughly northeastwards for over {{convert|110|km|sp=us}} between two of its left tributaries, the Kyra and the Aksha. It is bound by the Bylir River valley to the west and near its source it connects with the Khentei Range. The width of the Stanovik ranges between a maximum of {{convert|70|km|sp=us}} and a minimum of {{convert|40|km|sp=us}}.Google Earth
The average summits of the Stanovik reach between {{convert|1200|m|sp=us}} and {{convert|1600|m|sp=us}}. The highest point is a {{convert|1916|m|sp=us}} high unnamed peak. Much like in neighboring ranges, the relief is dominated by moderate height mountains with an abundance of steep-slopes and faults. The summits display fragments of the original alignment surface. The range rises in an area prone to earthquakes.
Flora
The slopes of the range are covered with mountain taiga and pre-Alpine forest. The higher elevations have dwarf cedar shrub and are often crowned by golets type bare summits.