Knowledge (XXG)

Anabar Plateau

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34: 104: 111: 390: 476:, characterized by a very low average rainfall of less than 250 millimetres (9.8 in) per year. Precipitation falls in the summer, mostly in the form of rain. The average air temperature in January is a chilly −34 °C (−29 °F) with an absolute minimum of −60 °C (−76 °F). The temperature may reach a maximum of 38 °C (100 °F) in July. The average annual temperature is −14 °C (7 °F). 595: 402:
The Anabar Plateau of the Central Siberian Plateau is one of the oldest structures on Earth, with rocks that are more than 3 billion years old. In its central region it is composed of Archean crystalline
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type elevations running across the plateau area, mostly in a roughly east to west direction. The highest point is a 905 metres (2,969 ft) high unnamed summit.
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from the highest part of the Anabar Plateau. Also to the southeast of the plateau is the source of the
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of the Olenyok basin have their sources at the southern end. To the northwest flows the
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further to the southeast, the Anabar Shield is one of the main features of the
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in northeastern Krasnoyarsk Krai and northwestern Sakha Republic, SSE of the
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cuts from the south across the western side and is joined by its tributary
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in the lower areas up to a height of 450 metres (1,480 ft) and
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has its source in the northeastern sector of the plateau. River
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Fishing helicopter flight from Khatanga to Kotuykan river
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The Big Kuonamka, which forms the upper course of the
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The Anabar Plateau coincides geographically with the
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The Archean Litosphere as seen in the Anabar Shield
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Index


Kotuykan River
Elevation
Anabar Plateau is located in Krasnoyarsk Krai
Krasnoyarsk Krai
Russia
Federal subject
Krasnoyarsk Krai
Sakha Republic
Range coordinates
70°30′N 108°0′E / 70.500°N 108.000°E / 70.500; 108.000
Parent range
Central Siberian Plateau
Age of rock
Archean
Proterozoic
Paleozoic
Type of rock
Gneiss
schist
Limestone
plateau
Krasnoyarsk Krai
Sakha Republic
Siberia
Russia
permafrost
Arctic Circle
Taymyr Depression
North Siberian Lowland

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