Морфогенезис лагуны Валькакинманка (мыс Биллингса, Восточно-Сибирское море)
Аннотация
Analysis of morphology of this most complicated coastal structure of the eastern Soviet Arctic showed that it is not an accumulative marine form, but a heterogeneous formation resulted from recent ingression into Iacustrine-alluvial plain. The lagoon's frame consists of relics of the continental Upper Pleistocene series, the inherited lagoon's forms are of the Holocene age, the marine built-up forms are not younger than 4000 years and have already been eroded for the last 1500 years (not more). Thus transgressions -have never exceeded the present sea level here.
Об авторах
Л. В. ТаракановРоссия
В. Н. Новиков
Россия
В. Ю. Бирюков
Россия
Рецензия
Для цитирования:
Тараканов Л.В., Новиков В.Н., Бирюков В.Ю. Морфогенезис лагуны Валькакинманка (мыс Биллингса, Восточно-Сибирское море). Геоморфология. 1981;(3):77-85.
For citation:
Tarakanov L.V., Novikov V.N., Biryukov V.Yu. Morphogenesis of Valkakimanka lagoon (Cape Billings, East Siberian Sea). Geomorfologiya. 1981;(3):77-85.