Anabar Plateau

Coordinates: 70°30′N 108°0′E / 70.500°N 108.000°E / 70.500; 108.000
Source: Wikipedia, the free encyclopedia.
Anabar Plateau
Анабарское плато
Kotuykan River, Anabar Plateau
Highest point
Peakunnamed
Elevation905 m (2,969 ft)
Dimensions
Length550 km (340 mi)
Width370 km (230 mi)
Geography
Anabar Plateau is located in Krasnoyarsk Krai
Anabar Plateau
Anabar Plateau
Location in Krasnoyarsk Krai
, Russia
Country
Federal subject
Krasnoyarsk Krai and Sakha Republic
Range coordinates70°30′N 108°0′E / 70.500°N 108.000°E / 70.500; 108.000
Parent rangeCentral Siberian Plateau
Geology
Age of rockArchean, Proterozoic and Lower Paleozoic
Type of rockGneiss, schist and Limestone

The Anabar Plateau (Russian: Анабарское плато) is a mountain plateau in Krasnoyarsk Krai and the Sakha Republic (Yakutia), Siberia, Russia.

The plateau is in a latitude dominated by permafrost. The permafrost thickness under the Anabar Plateau reaches 1,400 metres (4,600 ft).[1]

Geography

The Anabar Plateau is located north of the

Putorana Mountains, the border between both not being well-defined.[1] The average height of the plateau surface is around 500 meters (1,600 ft). There are slightly higher tableland 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.[3]

The Big Kuonamka, which forms the upper course of the

Lena. The Popigai impact structure is located to the NNE of the plateau.[2]

Anabar Plateau map section

Geology

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 schists and gneisses.[5] Along the periphery of the plateau Proterozoic and Lower Paleozoic limestones predominate.[1]

Anabar Shield

The Anabar Plateau coincides geographically with the

Siberian Craton. Together with the Aldan Shield further to the southeast, the Anabar Shield is one of the main features of the craton.[6]

Flora and climate

There are sparse forests of

mountain tundra with mosses and lichens in the higher altitudes.[3]

The climate prevailing in the Anabar Plateau is subarctic continental, 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).[7]

References

External links