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Taimyr depression

The Taimyr Depression ( Taimyr Depression ) is a depression in the Krasnoyarsk Territory of Russia , located between the mouths of the Yenisei and Khatanga rivers . Morphologically, it is a lowland , to which the Central Siberian Plateau abruptly breaks off from the south, and Byrranga Mountains from the north.

Taimyr lowland
Location
A country
  • Russia
The subject of the Russian FederationKrasnoyarsk region
Russia
Green pog.svg
Taimyr lowland
Krasnoyarsk region
Green pog.svg
Taimyr lowland

The Taimyr depression is made of a thick layer of Mesozoic and Quaternary sediments. Quaternary sediments in its composition (especially in the western part of the basin) form a continuous cover with a thickness of up to 100-200 m. Glacial formations lie at the base of the Quaternary.

Sources

  • Saks V.N. To the stratigraphy of the Quaternary deposits of the Taimyr depression. Reports of the Academy of Sciences of the USSR. 1945. Volume XLVI, No. 6. P. 262-265.


Source - https://ru.wikipedia.org/w/index.php?title=Taimyr_Carpet &oldid = 99640783


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