The soil is predominantly sandy and only occasionally there are clayey or chernozem areas. Driving on the roads in this area is difficult, especially in clay areas; This happens because the roads are poorly maintained and their surfaces are either full of potholes, or in areas where there used to be forests, they are littered with stumps and tree roots.
1) Novograd-Volyn flat upland.
Having separated from the main watershed near the village of Koshelevki, one of the branches, as already mentioned above, heads to the northwest and near Novograd-Volynsk enters into connection with a flat hill, the center of which can be taken to be the area near the village. Fedorovka.
This hill is more than 100 fathoms high. above sea level imBet is slightly hilly in nature; swamps are almost absent, forests are heavily cut down; rivers flow in valleys with gentle banks, 1-3 fathoms high.
To the river valley In some cases, the area falls in steep, often rocky cliffs, reaching in places up to 25 meters in height (near Novograd-Volynsk and in the area from this city to the village of Bystrichy). |
Two branches are separated from this elevation: one goes to the northeast—the Ubort and Uzha watersheds, and the other goes to the northwest—the watersheds of the river basins. Case and Uborti.
2) Vodorazdil Uborti and Slucha.
Having separated from the N.-Volynskaya flat upland, Volorazedl river. Slucha and Uborti represent a completely smooth plain, covered with shallow swamps with a hard sandy bottom. There are a lot of people. Closer to Sluch, as well as to the Tomashgrad-Klesovo region. Rudnya—Chabel—Rudnya Stariki—Osvitsk area is undulating. To the area from the mountains. Novograd-Volynsk to the village. Kurchitsy and Ot village. Bystrichy to metro station Lyudvipolya, banks of the river valley. Some are steep, and in some places rocky; below the last m$stechka up to the mouth along the river bank. There are sandy hills, towering above the surrounding area. The same is noticeable along the river. Clean up. From the village of Zubkovichi to the village. Yurovo it flows in deep dry valleys, with sharply defined banks, up to 10-12 fathoms high.
Sandy mounds are found not only along the river flow, but throughout the entire watershed. They are scattered without any order, sometimes in the form of separate groups, sometimes in the form of central groups. All of them have monotonous gentle slopes, partly overgrown with weeds, partly completely naked; Some of them are covered with a thin layer of muddy soil, but most are bare, loose sand, transported from place to place by the wind. Towards the North from the Rudnya-Tomashgrad-BBlovizha-/Kurzhevichi-Khochin line, the area quickly decreases, becomes a plain and is covered with almost continuous forests. There are many swamps; they make up almost a quarter of the entire area. Lonely sandy mounds are found only occasionally.
This last section has the character that, according to established understandings, is considered to be Poland. There are few roads here, and as you move further south, their number decreases. The predominant direction of roads is from west to east.
6) Vodorazdil Uborti and Una.
This watershed goes from Mogilevka to the north-east to Cape Slavechno. From him, in turn, from
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The main waterway, approaching from the south to the pre-Blam of the Slavechanskaya volost, is connected with the Slavechansk-Ovruch upland.
Up to the Yablonec-Radych river (a tributary of the Uzh river), the nature of the terrain of this watershed is hilly, and the hills are scattered without any system.
There are few forests and swamps. From r. Yablonep to Cape Iskorost, the hills accompany the left bank of the river. Snake; The river in this area is very winding and flows in a valley with steep and sometimes steep rocky banks (especially in the section from the village of Moshnya-Rudnya to Ushomir and from the village of Chelovki to the village of Shatrishche).
The rest of the area has an absolute height of 80-90 fathoms. flat in nature, especially in the western and northern parts. Approaching the river To be clear, the area becomes overburdened, the area of swamps and the number of swamps increases, after which they occupy up to one quarter of the entire surface.
VsB right tributaries of the river. Avoid turning it northeast to the river. Bee bread flows in deep valleys (up to 15 fathoms). From the mouth of the river Perga density is rapidly decreasing, so that on the river. Uborti, about five miles above the village. There's a crowd, something like rapids is forming.