Vychegda

Vychegda

(vĭ`chĕgdä), river, c.700 mi (1,130 km) long, rising in several headstreams in the Urals, NE European Russia, and flowing generally W into the Northern Dvina River at Kotlas. It is navigable (Apr.–November) c.595 mi (960 km) to Voldino and is used for timber flotation. Solvychegodsk and Syktyvkar are two of its chief ports. In the 16th cent. the Vychegda was an important water route to Siberia.

Vychegda

 

a river in the Komi ASSR and Arkhangelsk Oblast, RSFSR, a right tributary and the largest tributary of the Severnaia Dvina. It is 1,130 km long and has a basin area of 121,000 sq km.

The Vychegda originates on the southern edge of the Timan Ridge. In its upper reaches the valley is narrow and incised to a depth of 2(MO m; there are rapids. Downstream the valley forms lakelike swampy expanses in certain areas. A broad, marshy floodplain with numerous lakes and oxbow lakes stretches along the entire river channel. There are numerous shoals and washed-away, undermined banks. The river is fed by diverse sources, predominantly by snow. The mean annual flow rate measures 599 cu m per sec at Syktyvkar and 1,100 cu m per sec near the river’s mouth. The Vychegda freezes at the beginning of November, and the ice breaks up at the end of April. Its most important tributaries are the Vol’, Vishera, and Vym’ on the right and the Nem, Severnaia Kel’tma, Lokchim, Sysola, and Viled’ on the left. The Vychegda is used for floating timber. During the spring it is navigable as far as Vol’dino (959 km); during the summer and fall, as far as Ust’-Kulom (693 km). The river’s principal landings are at Sol’vychegodsk, larensk, Mezhog, Aikino, Syktyvkar, and Ust’-Kulom.

References in periodicals archive ?
The basis of this research consists of information on the hydrological-hydrochemical station located at the basin of the Vychegda River (Elva River--Meschura village) as well as observation data from the background meteorological station Ust-Vym located in immediate proximity (data collected during 2000-2007).
k--share of the underground component in the annual liquid flow (for the basin of the Vychegda River k = 0.
Upper Jurassic-Lower Cretaceous deposits containing up to 20 OS bands are widely spread in the northeast of the East-European Platform; they particularly occur in the Timan-Pechora and Vychegda oil shale basins [1].
The oil shale deposits of the Timan-Pechora OSB are developed in two isolated areas, namely the Nar'yan-Mar and Izhma regions, and those of the Vychegda OSB are distributed in the Sysola and Yarenga regions (Fig.
The distribution of the post-Swiderian complexes covers a vast area that ranges from the Baltic States in the west to the Volga-Oka interfluve and onwards to the rivers Vychegda and Pechora in the north-east.
A bronze casting, excavated from the Gljadenov settlement, Pozhegdin II, in the Middle Vychegda basin, and dated to the third and fourth centuries A.
ABSTRACT: The ungulate fauna present in Mesolithic, Neolithic, and Eneolithic Age sites of the Pechora and Vychegda Basins were considerable.
Keywords: archaeology, beaver, moose, Holocene, hunting, osteology, Pechora River, Vychegda River
Several sites in the basins of the lower Vychegda and Izhma Rivers were joined into 3 cultural groups and dated to the early Neolithic Age based on the character of stone implements and ceramics.
The first group included the sites Kochmas A and Chernaya Vadya on the lower Vychegda River.
The household (seasonal) activities of the ancient people of the Vychegda and Pechora Basins were based on hunting large forest ungulates and beaver, in addition to fishing and gathering.