The river freezes in late November or early December. Opens at the end of February or beginning of March. In the upper reaches, spills are insignificant and short-lived; from the village
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Their skins seem to be more significant. The water rises two arshins above the orlinar. The valley is flooded to its entire width. The newly arrived water usually lasts for about one week.
R. Channel. (Vengeful name for Rotok).
The source is in the village. Maryanovka. It flows south in a very meandering way. Flows into the river. Ros near the metro station Beloy-Tserkov. Length 51'/ verst.
The banks are mostly elevated. To s. Both banks of Pinchuk are gentle, below to the village. Sokolovki are very steep, covered with | lsom. From Sokolovka to the mouth the left bank remains steep, and below the village of Golushki and to the village. Sandy, it is covered with almost continuous forest. The right bank is more hollow and open. Only on the site of the village of Golushki and the village. Its scrapers are steep and covered with hair.
The soil of the banks to the village. Sandy clay, sandy loam below.
The width of the valley ranges from!/1 to 1 verst. The valley is swampy, completely inaccessible. The soil is swampy and clayey. Before the confluence of the Protoka stream, the size of the river and the dams is negligible. Upon exiting the Ksaverovsky stav, the river is lost until the confluence of the second tributary at the northern outskirts of the village. Pinchuk, where it reappears on the surface. Behind this crossing it disappears again and appears only south of the village. Pinchuks. At the confluence of the Rotoka stream, the width of the river varies from 4 to 12 fathoms. The depth to the confluence of the Channel is insignificant. Below from 1 to 3 ars.. Current speed '/> feet. per second. The banks of the river are mostly low-lying and marshy. The bottom is mostly swampy and muddy, only at the mouth it is sandy and hard.
Bet on p5k-6. They are impassable for fording.
There are 17 permanent crossings. Almost everything is fine. New crossings to the village. It is convenient to arrange pinchuks everywhere; below, more convenient points are located near the village. Solovinki and the area between Sokolovka and Galushki. To s. Solovinki River is wadeable for boats and individual riders; below,
right up to the mouth, it is passable only by crossings and fords. In this last section of the river, due to the swampiness of the valley, it can pose a significant obstacle to crossing, especially during a flood.
The river freezes at the end of November or beginning of December. Opens at the end of February or beginning of March. The spills are quite significant; the whole valley is filled with water; The last one lasts a very long time.
Above s. The sandy river receives a number of small streams and rivers; The most significant of them are the river. Chernyavka, which flows into Rotok in the village. Nightingales. It consists of several ponds connected by a stream flowing into a swampy valley overgrown with reeds. Through him there is access to the village. Comb dam.
The remaining streams are insignificant in size, but their valleys, like the valleys of the stream described above, are very swampy and inaccessible. Below p. Sandy tributaries no.
Rakitna Creek.
Flows into the river. Ros near the sugar warehouse, one verst above the village. Sinyava. In terms of its size and properties, it does not matter. Length 14 versts.
Gorohovatka stream.
The source is in the village. Novoselki. Flows into the river. Ros near the southern outskirts of the village. Prussians. About the site to the village. Widestavy sѪdny. No. Length 44'/› versts. The direction of the current is south.
From Zhidostavtsy to the mouth it is about 28 versts.
The right bank of the valley is very steep and steep along its entire length. LVY from the village. Vintsetovki to the village. The alder forest is gentle, and the rest of the way, like the right one, is steep and steep. Both banks from the village are covered with L$som. /Zhitostavtsy to the village. Vintsetovka and from the village. Teleshovka to the village. Sharkey. The soil is clayey.
The width of the valley up to Teleshevsky Pond is small, below the valley widens to 1-2 versts. Bottom of the valley
Lotiste especially between Teleshovka and Sharki. From /Zhidostavtsy to Vintsetovka and between the villages. Teleshovka and Sharki valley is overgrown with thick forest. The soil is marshy-clayey. |
The width of the river is 3-4 fathoms. The depth is 2-5 feet. Current speed 1 ft. per second. The banks of the river to the village. The screws are abrupt; Below the estuaries are low-lying and marshy. The bottom is viscous. Dam - 6. The banks are low. The bottom is viscous. The fords are impassable.