Publishing House SB RAS:

Publishing House SB RAS:

Address of the Publishing House SB RAS:
Morskoy pr. 2, 630090 Novosibirsk, Russia



Advanced Search

Geography and Natural Resources

2021 year, number 4

BOTTOM RELIEF FEATURES OF THE BASINS OF LAKE BAIKAL

E.E. Kononov
V.B. Sochava Institute of Geography, Irkutsk, Russia
Keywords: bottom relief, bathymetry, digital model, paleoreconstruction, correlations

Abstract

Based on analyzing bathymetric material obtained in different years by using high-precision geophysical equipment featuring multi-beam echo sounders, the main bottom relief features of the South, Middle and North basins of the Baikal depression are considered. It has been established that ridge-ravine forms and canyon valleys are well developed on the underwater slope of all depressions. The valleys of the canyons of the Middle and South basins reach the maximum maturity, which is associated with a longer history of the evolution of these basins. The canyon valleys are highly sinuous there, which is associated with the peculiarities of the underlying substrate and fault tectonics. The canyons of the western side of the Baikal depression are predominantly tectogenic in origin, are short in length and show a significant steepness of the longitudinal profile; their valleys are mostly rectilinear. The underwater slope along the eastern coast of the North basin and its abyssal surface are complicated by a set of glacial landforms: moraine swells and fan cones formed by turbidite flows during interglacial periods. On the coast, they are continued by very extended swells of lateral and stadial moraines. Tectogenic scarps are widespread in the lower parts of the underwater slopes and run usually parallel to the coastline. It has been established that a very characteristic form of the sloping relief of the South basin are the flat-convex surfaces of the deltas which sometimes reach the abyssal surface of the lake. Numerous outcrops of Miocene-Pliocene limnic sediments on the eastern coast of the Middle basin, and the nature of their spatial arrangement suggests that the sedimentary strata of the underwater slope of this basin may be of the same age and genetically homogeneous with terrestrial strata, which are Miocene-Pliocene in age. Similar deposits of the Tankhoi field on the southern coast of the depression also extend far into the water area of the lake, which gives grounds to confirm the existing points of view about the similar history of the development of the South and Middle basins.