Channel morphology and river flow in the northern Russian Plain in the Late Glacial and Holocene

International Journal of Earth Sciences

Volumn 89, Issue 3, 2000, Pages 541-549

  Sidorchuk, A Y ^a   Panin, A V ^a   Borisova, O K ^b   Elias, S A ^c   Syvistki, J P ^c  

^a MOSCOW STATE UNIVERSITY   (Russian Federation)

^b INSTITUTE OF GEOGRAPHY   (Russian Federation)

^c UNIVERSITY OF COLORADO   (United States)

Author keywords

Changeof hydrologic regime; Holocene; Late Weichselian; Northern Russian Plain; Palaeochannels; Palaeohydrology; Periglacial landscapes

Indexed keywords

HOLOCENE; MEANDER; PALEOCHANNEL; PALEOHYDROLOGY; PERIGLACIAL ENVIRONMENT; RIVER CHANNEL;

RUSSIAN FEDERATION; RUSSIAN PLAIN;

EID: 0034484869     PISSN: 14373254     EISSN: None     Source Type: Journal    
DOI: 10.1007/s005310000132     Document Type: Article

References (15)

1. About the correlation between the Vurm end tills of mountain glaciers of the Urals and of western Kara glacial sheet
2. Principles of underfit streams
3. Theoretical implications of underfit streams
4. Palaeovelocity and palaeodischarge determination for coarse gravel deposits
5. Method of Paleogeographical Analogues in Paleohydrological reconstructions
6. Palaeohydrology of the lower Vychegda River in the Late Glacial and the Holocene
7. The place of the Vistula River valley in the late Vistulian-early Holocene evolution of the European valleys
8. Analysis of paleochannels in the valleys of the upper Vistula and the Wisloka
9. Reconstruction of the permafrost zone and stages of its development
10. Paleofluvial estimates from dimensions of former channels and meanders
11. Resources of surface waters of the USSR