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The Chara Sands is estimated to have formed during the last glacial period 55 to 100 thousand years ago being what is left of an extinct lake formed by runoff from the
Sakukan glacier.
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and Udokan mountain ranges. It is a small desert 3 kilometers (1.9 mi) wide by 6 kilometers (3.7 mi) long, located in the Charsk basin amid the
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to the sand has no transition zone—this is one of the peculiarities of this unusual area, besides the roaming
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Chara Sands: Mysterious
Siberian Desert, 56thparallel.com Russia travel specialists
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The Kodar mountain range with the Chara Sands in the foreground near Novaya Chara
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The Chara Sands, a desert like area in the middle of
Siberia, as seen near
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208:High dune ridge near the foothills of Kodar
254:https://www.56thparallel.com/chara-sands/
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44:is an area of sand in Siberia near the
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242:Sandy Siberia - September 22, 2013
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121:Solitary dwarf pines and larchs
100:Chara Sands, Zabaikalsky region
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337:Landforms of Zabaykalsky Krai
342:Natural monuments of Russia
169:Blooming in the Chara Sands
157:The edge of the sandy area.
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36:Dune in the Charsky Sands
145:Lake Alyonushka at night
72:that emerge among them.
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28:lie in the background.
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332:Landforms of Siberia
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347:Deserts of Russia
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308:56.84°N 118.15°E
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50:valleys of Chara
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26:Kodar Mountains
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22:Novaya Chara
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285:Chara Sands
42:Chara Sands
326:Categories
226:References
66:sand dunes
62:peat bogs
299:118°09′E
68:and the
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24:. The
70:oases
58:larch
46:Kodar
79:View
56:and
54:pine
40:The
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234:^
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