It freezes in December. It opens in early or mid-March. Spring floods are quite significant. Water floods the entire valley. The current is swift, causing a lot. go Odstj. The water sometimes rises to 2 soots. above ordinary. Transportation means other than fishing boats of the most primitive device n5t. It is most convenient to arrange new crossings: near the Ladyzhinsky farms, near the village. Gubniki, Skibintsy, Krushinovka, Mankovka, Shumilovo, Berezki, between the villages. Stavki and Lugovoe, near the village. Strunkov in two places, near s.s. Karavchin, Olshanka, Salkov, Chemiropol, Savran, Zavalye, Lupolovo, Goloskovo and between the villages. Goloskovo and the village of Oniskovo (where the islands are located). In general, in the area under consideration, the Bug represents a serious obstacle. Forcing it is most convenient from the village. Salkov to Olshanka, etc. there are stone fences to facilitate the construction of crossings.
Being 4-5 crossings from the river. Ln$5str, South. Bug can represent an auxiliary defensive line in the rear of the defensive line of the river. Day $str. In relation to sections of the river. Bug, lying upstream, makes it difficult to bypass them from the south by crossing the river. Dnistra.
R. Postolova. (Lyuvyi tributary of the Yuzhny Buyu River).
The source is south of the Cherepashinskaya tavern; lo s. Cherepashintsy flows to the southwest, further to the village. Khomutinsky to the northwest, from where to the mouth to the southwest. Flows into the river. Yu. Bug at the southern outskirts of Cape Yanov. Length 36 versts. The command of the valley banks is indifferent. The steepness can sometimes make it difficult for artillery to move. The soil is loam with an admixture of chernozem. The banks are mostly deserted, only here and there small groups of forest can be found.
Width of the valley to the southern outskirts of the village. Cherepashchintsy is a narrow gap that widens hundreds of times up to 100
150 steps, down to the third mile. The soil is black soil. The bottom of the valley to the southern outskirts of the village. Cherepashintsy is a wet meadow, below is a swamp overgrown with reeds. In dry summers, the swamp can be crossed in open formations, and in some cases it can be ridden on horseback.
The width of the rbka ranges from 3 to 15 steps. Depth to c. Cherepashintsy is no more than an arshin, below it reaches 11 fathoms. From Kurlelevka the river consists almost entirely of staves that are impassable for fording.
There are 11 permanent crossings. The crossings are mostly fragile. Due to the insignificance of r$fki from the origins to the village. The Cherepashinites will not encounter any difficulties in constructing new transports. Below it is made difficult partly by the swampiness of the valley, and partly by the size of the river. In general, the river cannot be considered a serious obstacle, especially for pfhota. The river freezes in the second half of November. Opens in the first half of March.
Tributaries of the river The posts are not of particular importance, but their swampy valleys in places can make it difficult for convoys and artillery to cross.
V. E
R. Desna. (Lion tributary of the Yuzhny Buyu river).
It starts from several streams, 1 verst north of the village. Yuzeeovka, flows from its sources to 1. Shirokaya Greblya to the southwest, further to the village. Gubina to the south, from the village. Gubina to the village. Loseevka again to the southwest, further to the village. Turbov to the southeast; from the village Turbov to the village. Liseyevka to the north-west, far to Paska, which is south of the village. Sosnovka to the south, from where to the mouth to the northwest. Length 75 versts. Techenme is tortuous.
The banks of the valley to the village. Kholyavintsy is of considerable steepness and steep in places, from the village. Kholyavintsy to the mouth the steepness is insignificant. The command is mostly indifferent. The soil up to the village of Shirokaya Greblya is black soil, dalfe up to the village. Kholyavintsy—chernozem-sandy soil, from the village. Kholyavintsy to the mouth is sandy.
Both banks are covered with forest from Sosnovka to the railway bridge, then to the mouth there is forest only on the right bank. On the left bank of the river from metro station Turbovka to the village. Sobolevki. |
The width of the valley is mainly 100-200 fathoms, but there are areas with a width reaching up to 1" verst. The ground of the valley is generally marshy. To the metro station Kholyavintsy the valley is accessible for pedestrian traffic. Below is a continuous swamp, accessible only to pedestrians and then only in winter.