The area of land increases across the world, moving northward, reaching up to one-fifth of the entire surface.
The soil is sandy, and in the valleys of the river there are swamps, although in general there are few of them.
3) Vodorazdfl Uzha and Irsha. (To the east of Teterev and Uzha).
The Uzha and Irsha watershed is separated from the main watershed near the village. Koshelevki.
Characteristics of the left bank of the river Irshi approximately to lin ld. Chepovichi-Zubovshchina is exactly the same as that of the right (see the watershed of Irsha and Teterev).
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The most significant elevations are near Cape Iskorosti, d.d. Kholosno, Mogilno, near the village. Nymilovki and the mind. Peas.
To the east of the Chepovichi-Zubovshchina line, the area is flat, but east of Cape Ivankov it is hilly, especially east of the river. Veresni (tributary of the Uzh River).
Slopes to the river Already and Irsha are completely defined, although they are gentle, and only below Malin there are cliffs.
Somewhat west of the river. 7The Zhereva plain is lined with gullies, the depth of which reaches 4-10 fathoms; Streams flow along their bottom. The banks of these ravines are relatively flat.
Sandy mounds are scattered throughout the plains without a system; they mainly accompany the current of the river. Most of them are along the current of the Black Grouse and Irsha. Their height sometimes reaches up to 10 soots.
Such sand ridges are most significant along the river. 'Tetereva near the village of Kukhary, about six versts below this village; above and below metro station Ivankov, on the right bank of the river. Zvizdali; along the river Butch near the village New Vorobyov and in several other places.
LЪsa occupy '/‹ to '/4 of the entire area; swamps are almost NBTH.
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East of the river mouth Irshi, the number of forests gradually increases, along the distance to the east, reaching the entire area; swamps are also overgrown, especially to the west of the river. Zvizdali and Zhereva appeared, but in general there are few of them and they are not deep.
4) Slavechno-Obruch Upland.
The highest point of this hill lies east of Slavechno metro station near the village. Gorodets, reaching 105 fathoms. above sea level.
This hill stretches in a narrow strip of 15-25 versts along the left bank of the river. Norin, from northwest to southeast to the city of Ovruch and to the mouth of the river. Ilya.
To the south and southeast of Cape Slavechno and around it, the hills are completely treeless, cut through by numerous ravines; Their slopes are mostly steep. When the forest soil is wet, after each heavy rain, new gullies are formed and the existing ones are enlarged.
To the west and north of the Slavechno hills are covered with forest; ravines nft. These hills look like parallel ridges with a predominant direction from northwest to southeast; The ridges are separated from each other by deep, steeply sloped valleys, the bottom of which is in most cases swampy. To the east, the terrain is barely flattened, but to the west and in the north the heights quickly decrease, and the terrain takes on a flat, silty-swampy character.
To the east of Slavechno the hill has the appearance of a narrow (10-12 ver.) ridge, devoid of forest, gradually descending to the east and stretching along the left bank. Norina; into the valley of this river the hill descends steeply, sometimes steeply. The entire area is cut up by ravines, the dimensions of which are now gradually increasing, having been completely destroyed by the inhabitants of the bushes and trees that covered the slopes and bottom of the ravines and thereby protected them from further erosion..
To the east, the terrain is undulating, but the hills do not have sharp outlines, their slopes are gentle and the terrain looks like a plain dotted with hills.
To the north, the main ridge descends quite quickly, but the nature of the terrain remains hilly. Separate, forest-covered, hills are separated from each other by low-lying and swampy meadows. The soil is sandy or loamy everywhere, sometimes with humus, and in some places rocky. Along the border of Minsk lips. absolute plain begins. |
The continuation of the Slavechno-Ovruch Upland to the east is the watershed of the river. Pripyat and Uzha, which has the character of a sandy, treeless plain (altitude 80 fathoms above sea level). This waterway stretches from the village of Burakovka to the Chernobyl metro station. Its slopes facing south, towards the river. Uzhu, very gentle, but to the east - to the river. Pripyat's banks are steep.
Hydrographic description!e. Market systems. R$ki. Swamps. Lakes.
Southern part of the area. RIVER SYSTEMS. RЪKI.