Between the upper reaches of the river Uzha and Uborti, the entire space is covered with sandy mounds. Below the mouth of the Perga, along the right bank of the Ubort, 4-5 versts from the river, stretches a continuous sandy bed up to 5-7 fathoms high; it is gradually approaching rk and near the village. The kopishe rests closely against it, falling into the river like a cliff. North of the village. This ridge quickly descends and disappears into the swamps of the Minsk province.
Vodorazdfly Uzha, 7/Kereva and Norina represent a flat character. Initially, these watersheds are covered with wood, which occupies almost half of their area; But,
O. o along the mountain range to the east, there are fewer forests, the number of swamps also decreases, and to the west there are no more than 1/3 of them on the surface; to the east near Cape Iskorosti, where there is almost no water supply, and there are no swamps.
The fall of the area towards the river Already, 7 Kerev' and Norin are so significant that the banks of these rivers are clearly defined (especially Zherev and Norin, and the slopes of the banks of the first river are gentle, and the second is steep in places, as for example above Cape Veledniki).
Along the banks of these same rivers, parallel to them, stretch the cfpi of sandy hills, which stand out especially clearly along Zherev almost from the upper reaches to Cape Lugina, below it, at Rudnya Baikovsky and on Norin - near the village. Mill.
The easternmost part of the Zherev and Norin watershed is a hilly area, with a mostly open character (arable lands, meadows, swamps, almost absent). The southern slopes (to the Zhereva valley) are somewhat steep; northern ones - (to the Norin River) as much as possible.
2) Watershed of Irsha and Teterev.
Separated from how far south it is. Pulina from the main watershed, watershed r.r. Irsha and Tetereva are heading almost directly east to Cape Chernikhov, splitting up at the same time. n5how many threads.
One of these branches from Cape Chernikhov heads directly south to the Zhytomyr Upland and forms the watershed line of the river. Kamenki from r.r. Myka, Pork Meadow and Bystroevka. Near Zhitomir, this branch turns to the east, heading towards metro station Korostyshev, where it abuts the river. Grouse and between d.l. Karachevka and Kozevka form coastal cliffs and cliffs.
The terrain, both to the west of Chernikhov and to the south, to Zhitomy, is slightly hilly, intersected in places by ravines and streams flowing through dry valleys on steep banks. Slopes of heights, approaching Teterev and, partly, to the river. Kamenka, end in steep cliffs and rocks here and there. At Zhitom!ra the cliffs reach 25 fathoms.
The other—heads to V.S.—V. and constitutes the watershed river itself. Irsha and Teterev.
Finally, the third, having separated a little to the west of the Chernikhov metro station, heads to the north-east. and represents the watershed of the river. Irshi and its tributary river. Reeds.
The nature of the area up to the height of the city of Radomysl is hilly, the slopes are gentle; to the east the relief smoothes out and the heights remain only noticeable along the banks of the river. Black grouse.
The branches consist of a whole series of small chains, with a general direction from southeast to north-west, but along the world towards the north-east the chains gradually decrease, forming a series of terraces; The terrain on the terraces is flat, but crossed by a mass of small streams. _ There, where the hills cross the rivers, the banks of the latter are high and steep, rocks and here and there rapids are exposed in places (for example, between the villages of Goroshki and Valyanshchina on the Irsha River; at Kamenny Brod on the Trostyanitsa River).
There are few people in the southwest of the Potfevka-Chudin line; swamps occur only in some places to the east of the village. Peas. To the east of this line there are more LBs; the soil is predominantly sandy loam, and sometimes sandy; there are also few swamps; They are found mainly in the valleys of the river.
a) The right bank of Teterev. (The watershed of this river and the Zdvizhi river).
Making up a continuation of the watershed river. Zdvizhi and Teterev, examined in the southern region, the indicated ridge kt <$veru from the conditional deprivation of the river. Blka—s. Borodyanka has a flat character, only in places intersected by sandy ridges several miles long and from 3 to 10 soots. heights, such as the section from the village of Blitcha to the village of Kolentsy. The coastal hills generally have flatter slopes and only in some places do they descend steeply to the river, for example. from the village of Makalevich to the village of Kukhary. Plo-