Ostgrove on the site under consideration - 15. The largest of them has 3/4 length and 1/4 ver. width (opposite the village of Sukholuchye). Shoals come across quite often, but they are not large in size.
The bottom of the river and the banks are sandy.
`‘There are no permanent crossings; ferries—3; lifting power of each three loaded carts.
In the section under consideration, the Ln$ir is navigable. Shipping continues from 200 to 250 days a year.
It freezes in Boney in November or early December. Opens between March 1st and March 31st.
The rise of water and flooding in the spring is quite significant. Lolin's river is completely covered with water, sometimes causing significant devastation. In the autumn, spills after the autumn rains are significant.
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Forcing the river from the right bank to the left bank in the area under consideration is very difficult; it is most convenient near the dd. Glbovka, Chernin and near the village. Svaromye and to the Petrovtsy - Vyshgorok section.
Right tributaries of the Dnfpra.
Pripyat. Along the river flows from the village. Blosorka to the mouth for a length of 76 versts.
The flow is extremely tortuous from the northwest to the southeast, sometimes in the form of large, sometimes in the form of small reaches.
Both banks of the valley up to the village of Kosharovki are low and flat. From Kosharovka to the mouth the right bank is elevated, often steep and steep; The first bank is very low and broken. Ri
The soil of the banks is sandy; on the steep slopes of the right bank, the sand is cemented with clay, and at Lelev, Chernobyl and in places between them, the coastal cliffs consist of continuous layers of red clay.
L'sa, on the right bank from the village. Blosorki to N. Shepelichi and below the mouth of the river. Already, and on the left from the beginning of the section right up to the mouth of the river. Borukha, are very sparse and alternate with meadows, clearings and clearings.
The width of the valley is up to 15 versts. The soil is sandy-chernozem, but there are also swampy areas. The valley is a meadow lowland, cut by a whole network of hollows, holes, blind branches, channels and old rivers, preventing movement in and across the valley.
On the front bank of the river, at a distance of 3-5 versts from the shore, an almost continuous swampy strip was formed, passable only by experienced single people in dry times. The entire right bank is covered with sandy hills overgrown with sparse pine forest.
The width of the river ranges from 40 to 260 fathoms. Depth from */w to 4 fathoms. The speed is flowing!/»?—1! foot. per second, on bends up to 3-5 feet. per second.
The bottom of the river is sandy and easily eroded; in the branches and channels it is sandy and silty. The shores are sandy, narrower, covered with sparse vegetation. Their height is mostly small. |