Fossil slope deposits in the Northern Arctic asymmetrical valleys

Authors

  • Georgii F. Gravis Moscow State University

DOI:

https://doi.org/10.26485/BP/1969/20/15

Keywords:

solifluction, ice veins, ground ice, slope morphology, last cold stage, northern Yakutia

Abstract

In the asymmetrical valleys of northern Yakutia, thick covers of slope deposits occur, forming rhythmic horizons in the upper valley segments related to periodic changes in climate and slope dynamics. Solifluction deposits, poor in organic remains, developed during cooler phases of intensive slope activity and contain numerous ice lenses, ice veins and deformed peaty layers with plant remains. Three Würmian phases of increasing climatic severity have been distinguished in northern Yakutia, correlated with the Zyryan and Sartansk stadials, whereas warmer oscillations correspond to interstadials and the postglacial period.

References

Alekseev, M. N., Ravskij, E. I., Cejtlin, S. M., 1966 - Osnovnye geokhronologicheskie etapy antropogena Sibirskoj platformy (Main geochronological stages of the Anthropogene of the Siberian platform). Izv. Akad. Nauk SSSR, ser. geol., No. 3.

Alexandre, J., 1960 - La succession probable des phases morphologiques au cours d'un cycle climatique quaternaire en Haute Belgique. Biuletyn Peryglacjalny, No. 9.

Büdel, J., 1937 - Eiszeitliche und rezente Verwitterung und Abtragung im ehemals nicht vereisten Teil Mitteleuropas. Petermanns Geog. Mitteil., Ergzh. 229.

Büdel, J., 1953 - Die ,,periglazial"- morphologischen Wirkungen des Eiszeitklimas auf der ganzen Erde. Erdkunde, Bd. 7.

Dylik, J., 1955 - Rhythmically stratified periglacial slope deposits. Biuletyn Peryglacjalny, No. 2.

Dylik, J., 1961 - Analyse sedimentologique des formations de versant remplissant les depressions fermées aux environs de Łódź. Biuletyn Peryglacjalny, No. 10.

Giterman, R. E., Golubeva, L. V., et al., 1965 - Osobennosti rasti­telnogo pokrova vremeni zyryanskogo oledeneniya Sibiri (Some characteristics of vegetation cover of Zyryansk glaciation time in Siberia). Izv. Akad. Nauk SSSR, ser. geol., No. 3.

Goncharov, V. F., 1967 - Stratigrafiya chetvertichnykh otlozhenij Kularskogo zolotonosnogo rajona (Stratigraphy of Quaternary deposits of the Kular gold-bearing region). Geologia i Geofizika, No. 4.

Gorshkov, S. P., 1967a - O genezise i vozraste sklonovykh glybovo­shchebnisto-suglinistykh otlozhenij Severa Yenisejskogo kryazha i severo-zapada Vostochnogo Sayana (On the origin and age of debris-silty deposits of the N-Yenisej range and NW-part of the E-Sayan). Doklady Akad. Nauk SSSR, t. 172, no. 3.

Gorshkov, S. P., 1967b – O trekh etapakh v razvitii sklonov denudacionnykh massivov na yuge Krasnoyarskogo kraya (Three stages of slope development of the denudational massifs in the southern Krasnoyarsk region). Vestnik Mosk. Gos. Univ., ser. V: geog., No. 2.

Gravis, G. F., 1962 - Ledyanye zhily v deluvialno-soliflukcionnykh otlozheniyakh (Ice veins in deluvial (colluvial) and solifluxional deposits). In: Voprosy Geografii Yakutii, vyp. 2; Yakutsk.

Grichuk, M. P., Grichuk, V. P., 1960 - O prilednikovoj rastitelnosti na territorii SSSR (On periglacial vegetation within the U.S.S.R. territory). In: Periglacialnye yavleniya na territorii SSSR, MGU ed.

Katasonov, E. M., 1958 - Ledyanye zhily i prichiny izgibaniya sloev v merzlykh chetvertichnykh otlozheniyakh (Ice veins and causes of layer bending in Quaternary frozen deposits). Materialy k osnovam uchen. o merzlykh zonakh zemnoj kory, vyp. 4; Moscow.

Katasonov, E. M., 1962 - Kriogennye tekstury, ledyanye i zemlanye zhily kak geneticheskie priznaki mnogoletnemerzlykh chetvertichnykh otlozhenij (Cryogenic structures and ice- and ground veins as genetic indicators of Quaternary permafrost). In: Voprosy kriologii pri izuchenii chetvertichnykh otlozhenij; Akad. Nauk SSSR ed, Moscow.

Kessler, P., 1925 - Das eiszeitliche Klima und seine geologischen Wirkungen im nicht vereisten Gebiet. Stuttgart.

Kuznecova, T. P., 1967 - Nabludeniya za poligonalno-zhilnymi ldami v predgoryakh Kularskogo khrebta (Observations on poligonal vein ice in the Kular foothills). Podzemnyj led, vyp. 3; MGU ed.

Logachev, N. A., Lomonosova, T. K., Klimanova, V. M., 1964 - Kajnozojskie otlozheniya Irkutskogo amfiteatra (Cenozoic deposits in the Irkutsk amphitheater). Nauka ed., Moscow.

Mazurov, G. P., Tikhonova, E. S., 1964 - Preobrazovanie sostava i svojstv gruntov pri mnogokratnom zamorazhivanii (Composition- and properties changes of grounds by repeated freezing). Vestnik Leningradskogo Univ., No. 18: ser. geol.-geog.

Pécsi, M., 1964 - Chronological problems of the patterned soils of Hungary. Biuletyn Peryglacjalny, No. 14.

Pécsi, M., 1966 - Problèmes quaternaires de la recherche géomorphologique des montagnes centrales Intracarpathiques. Geographica Polonica, No. 10; Warsaw.

Ravskij, E. I., Aleksandrova, L. P., et al., 1964 - Antropogenovye otlozheniya yuga Vostochnoj Sibiri (Anthropogene deposits of southern East Siberia). Trudy Geol. Inst. Akad. Nauk SSSR, Vyp. 105.

Sekyra, J., 1961 - Periglacial phenomena. Prace Inst. Geol., t. 34, part 1; Warsaw.

Shilo, N. A., 1961 - Chetvertichnye otlozheniya Yano-Kolymskogo zolotonosnogo poyasa, usloviya i etapy ikh formirovaniya (Quaternary deposits of the Yana-Kolyma gold-bearing zone - conditions and stages of their formation). Trudy VNII-I, t. 16, vyp. 66: geol.

Vasyunina, E. D., 1958 - Nekotorye osobennosti geologii zolotonosnykh chetvertichnykh otlozhenij ulino-Tenkinskogo rajona (Some geologic characteristics of Quaternary gold-bearing deposits of the ulin-Tenkin region). Trudy VNII-I, t. 8: geol.

Voskresenskij, S. S., Ananev, G. S., 1961 - O stroenii sklonovykh otlozhenij Zabajkalya (On the structure of slope deposits in Trans­baikal). Vestnik Mosk. Gos. Univ., ser. 5: geog., No. 6.

Žebera, K., 1961 - Deluvial and talus deposits. Prace Inst. Geol., t. 34, part 1; Warsaw.

Downloads

Published

2025-12-02

Issue

Section

ARTICLES