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Glaciated Landscapes of Arctic and Subarctic Russia. / Астахов, Валерий Иванович.

в: Doklady Earth Sciences, Том 525, 49, 2025.

Результаты исследований: Научные публикации в периодических изданияхстатьяРецензирование

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@article{6958273e2a314908a108768b8514257b,
title = "Glaciated Landscapes of Arctic and Subarctic Russia",
abstract = "The Quaternary Ice Age produced a great variety of landscapes in northern Eurasia. Their diversity is expressed in various large elements of physiography – vast plains of sedimentary basins and mountain systems up to 3 km high – all embellished with glacigenic features. The undelible imprint on northern landscapes was exerted by the outstanding continentality of climate which played a significant role in the Quaternary climate changes of northern Eurasia. It led to the specific Siberian type of inland glaciation in which glacier ice was often fused together with the old and stable permafrost. This resulted in many relict Pleistocene features of the present-day scenery, including thick slabs of fossil glacier ice well preserved in the arctic terrains. This essay deals with main landscape peculiarities of northern Russia originated during the Ice Age as understood by the majority of native and international investigators. A brief note on the influence of Pleistocene inland glaciation on the principal petroleum reserves is added.",
keywords = "Keywords: Russian Arctic, northern Siberia, Pleistocene glaciation, old permafrost, continental climate",
author = "Астахов, {Валерий Иванович}",
year = "2025",
doi = "10.1134/S1028334X25609460",
language = "English",
volume = "525",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "МАИК {"}Наука/Интерпериодика{"}",

}

RIS

TY - JOUR

T1 - Glaciated Landscapes of Arctic and Subarctic Russia

AU - Астахов, Валерий Иванович

PY - 2025

Y1 - 2025

N2 - The Quaternary Ice Age produced a great variety of landscapes in northern Eurasia. Their diversity is expressed in various large elements of physiography – vast plains of sedimentary basins and mountain systems up to 3 km high – all embellished with glacigenic features. The undelible imprint on northern landscapes was exerted by the outstanding continentality of climate which played a significant role in the Quaternary climate changes of northern Eurasia. It led to the specific Siberian type of inland glaciation in which glacier ice was often fused together with the old and stable permafrost. This resulted in many relict Pleistocene features of the present-day scenery, including thick slabs of fossil glacier ice well preserved in the arctic terrains. This essay deals with main landscape peculiarities of northern Russia originated during the Ice Age as understood by the majority of native and international investigators. A brief note on the influence of Pleistocene inland glaciation on the principal petroleum reserves is added.

AB - The Quaternary Ice Age produced a great variety of landscapes in northern Eurasia. Their diversity is expressed in various large elements of physiography – vast plains of sedimentary basins and mountain systems up to 3 km high – all embellished with glacigenic features. The undelible imprint on northern landscapes was exerted by the outstanding continentality of climate which played a significant role in the Quaternary climate changes of northern Eurasia. It led to the specific Siberian type of inland glaciation in which glacier ice was often fused together with the old and stable permafrost. This resulted in many relict Pleistocene features of the present-day scenery, including thick slabs of fossil glacier ice well preserved in the arctic terrains. This essay deals with main landscape peculiarities of northern Russia originated during the Ice Age as understood by the majority of native and international investigators. A brief note on the influence of Pleistocene inland glaciation on the principal petroleum reserves is added.

KW - Keywords: Russian Arctic, northern Siberia, Pleistocene glaciation, old permafrost, continental climate

U2 - 10.1134/S1028334X25609460

DO - 10.1134/S1028334X25609460

M3 - Article

VL - 525

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

M1 - 49

ER -

ID: 149139288