The great depression of the Old World begins with the deepening of
the Volga basin below Simbeersk; and at the place (51¾° N. lat., near
Orenboorg and Saratov) where it breaks through the last row of hills in
the Obstshei-Syrtis, it commences a rapid descent toward the Caspian and
the Aral Seas. This great concavity, on the confines of Europe and Asia,
at the center of the greatest land-mass, and far removed from any ocean,
is remarkable as having no parallel on the globe. Humboldt remarks that
perhaps a similar phenomenon would be repeated at the interior of other
continents, if the tertiary formation and the parts found by marine
deposit did not exist. It would be profitable to follow out so weighty a
thought, with the surface as it now is.
The Obstshei-Syrtis is the moderate range of hills which runs westward
in two branches from the Bashkiric-Ural, at Orenboorg, the northern spur
running by Uralsk and the Ural River; the southern by Samara, rising
on the east shore of the Volga to a height of 600 feet, and ending at
Sarepta.
Orenboorg, on the Obstshei-Syrtis, where it leaves the Ural chain, is 255
feet above the sea. Uralsk lies somewhat lower, being 234 feet above the
sea. The surface of the Volga, where it breaks through the high banks of
Saratov, is only 36 feet above the ocean level; while the western shore,
above Saratov, is 562 feet in height. Farther down the river, Sarepta
lies 30 feet below the sea level; and there is, therefore, between
Saratov and Sarepta, a distance of about 180 miles, a fall of 66 feet.
West of the Volga, and following the river, is the continuation of the
Obstshei-Syrtis, ranging in elevation from 562 feet down to 168 feet.
At Sarepta, the low hills which thus far have skirted the Volga turn to
the southwest, to the Manitsh steppe, sinking to an elevation of but 75
feet, and extending as far as the Sea of Azof. At Sarepta, too, the Volga
turns from its normal southerly course, and strikes southeasterly across
the Astracan steppe, entering the Caspian at the City of Astracan, 72
feet below the level of the sea. The level of the sea is 4 feet below the
shore on which Astracan is built.
Public-domain text, read in full here on John Shaqi.
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