The named watershed is separated from the main one between the s.s. Novoselki-Yuzeeovki and first goes south to the village of Novaya Rossava, then turns southeast to Cape Boguslav. Having reached the village. Yukhny, turns east, and then south along the section of the Mironovka-Korsun railway road to the village. Golyaki, from where it turns to the northeast, forming the left mountainous bank of the river valley. Rossi until it flows into the last river. Rossavy. The average height of this branch is 89.3 fathoms. The highest height between s.s. Pawns and Golyaks 97.4 fathoms. The nature of the watershed branch is undulating, flat, most rugged to the east, in the area of the river. Rossavy, s. Pilyava, metro Tagancha, metro Steblev r. Russia and in the vicinity of metro Boguslav. This overcrowding is expressed in the abundance of ravines and gullies, which are the beds of streams and rivers flowing into the river. Russia.
The soil is loam with a significant admixture of chernozem. In the southern part there is black soil.
7) Vodorazdl of Yumzhny Bug and Soba.
Having separated from the main watershed near Moncino, the said watershed will reach the village. Happy is directed south, and dalfe turns southeast to the north. Dzhurintsy-Yarmolinpa.
From the village of Schastlivaya, where the named watershed has about 133.9 soots. heights, goes away just a little oh yeah great entertainments that fill the area between the Southern Bug and Sob, forming many gullies and ravines. The terrain on the southern slope of the watershed is highly overcrowded and difficult for movement.
On the contrary, the northern slopes have an open character and are convenient for movement.
The southeastern slopes are similar in nature to the southern slope, but the ravines here are less deep.
The soil is loam with an admixture of chernozem.
8) Vodorazdil of the Southern Bug and the river. Sinyukha with its tributaries Gorny Tinich and Yatran.
'From Oratovo metro station, the indicated watershed goes southeast to the station. Khristinovka, where it is divided into 4 branches, idupia:
a) west in the direction of the north. Komarovka—Stepanovka—_Meleshkov—Bubnovka, at which it turns south and, heading towards the village. Sumovk completely disappears, not even raising the banks of the Bug in this area; The southern slopes of this valley are replete with ravines and ravines with steep banks; on the northern slope there are fewer ravines and are more flat.
6) On yut on s.s. Ternavka-Savran.
c) To the southeast to the north. Senki - Golovanevsk. At the Troyanskaya tavern, this branch, in turn, is divided into 2 branches: one goes to the Pokotilov metro station, and the other goes to the Kapitanovka tavern and disappears at Kanetspol. The highest point 3 versts west of the village of Tomashevka is 125 fathoms. The river is riddled with ravines and gullies.
and d) At cape Talnoye and DalBe south to Pokotilov. This is the formation of water distribution of tributaries of the river. Blue
The soil to the west is loamy, to the east is black soil.
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9) Vodorazdl of Rotten and Gorny Tinich.
Having separated from the main watershed near the village. Quiet Khutor, goes southeast to Cape Vinograd - Ryzhanovka - the mouth of Gnily Tikich, forming a watershed of the indicated rivers and slightly hilly the area through which it passes. In the northern part to the village. Ryzhanovka slopes are flat throughout and do not pose any difficulties for movement. To the south of Ryzhanovka there are many ravines and gullies with steep slopes and steep slopes, which greatly impede movement.
The soil is black soil.
10) Vodorazdl Olshanni and Tyasmina.
Having separated from the main divide between the village. Topilno and s. Tereshki and taking the direction to the northeast to the north. Ksaverivka-Budische serves as a watershed for these rivers. At the village The Burty is separated by a minor watershed of the tributaries of the river. Tyasmin Serebryanka and Rotten Tikich.
The average height of the watershed is 90 fathoms. The highest point near the village of Ksaverov is 93.5 fathoms.
The width of the watershed along the route to the east increases, on the Orloven-Gorodishche line it reaches 7-8 versts and the watershed begins to narrow again. The slopes of the water-Ksaverovka introduce themselves
It was divided up to the Khlystunovka line into a plateau, slowly descending both to the north and to the south and dissected by hollows with a meridian direction. Hollows leading to the north, with steep slopes, descend steeply to the river. Olshank $ and greatly impede movement.