From between Khlystunovka and Eksaverovka, the slopes of the watershed fall steeply to the banks of the river. r. Olshanki and M$dyanki. They! are cut up by a mass of hollows and generally turn the Gorodishe-Khlystunovka-Ksaverovka-Buda Orlovetskaya section into extremely rugged, ragged terrain. The soil to the east5 is clay-chernozem with sand, to the west without sand.
5) The southern ridge, representing the watershed of the Southern Bug and the Dniester.
It enters the territory of the region at the Shpikov metro station and, in the direction from northwest to southeast, passes by the metro station. Knyazhepol and Kodyma on the village. Timkov and around the village. Borscht enters the Kherson province through two branches: one goes along the river. Kodyma, and the other along the river. Yagorlyk.
The height of the water spread fluctuates between 140.8 soot. and 136.4 soot.
At the village Kodyma's southern ridge gives off a branch heading through the village. Bud to s. Borsuki and DalBe to s.s. Polyanetsky - Nemirovka - Nikolaevka and Konetspol disappears.
This branch separates the tributaries of the Savranka from the Kodyma; it does not form hilly hills, but is marked everywhere by a flat ridge.
The soil is predominantly loamy. In the vicinity of Balta there is forest.
In general, the entire southern ridge cannot be called mountains. It is populated everywhere and is not impeded anywhere for the movement of troops, except for the southwestern slopes, which are heavily dissected by the deep gullies of the Dnfstra tributaries. These beams greatly impede movement, especially from the northeast to the southwest.
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From the flat hill that makes up the watershed of the upper Techevya river. Case and Southern Bug, at Cape Salnitsa the watershed of the river is separated. Case and the upper reaches of the river. Black grouse. Entering the precincts of the district near the village. Nosovki, lo m. Romanov he goes north, from where he turns further northeast to the village. New Plant, and from this last point it again takes the original direction towards the Pulin metro station towards the village. Koshelevka. At Koshelevka, 2 branches are separated from this watershed: 1) to the northwest—the watershed of the river
Case and other tributaries of the river. Pripyat (Lva, Stvigi, Uborti, Slavechny), 2) to the north, and zatBm to the north-west—the watershed of the river. Snake and Black Grouse.
Near Cape Pulina, a ridge separates to the east at Cape Chernikhov, which forms the watershed of the river. Teterev and its tributary river. Irshi; From this last day, in turn, with. Kruchinets is separated into a north-eastern ridge-watershed of the river. Irshi and Trostyanpa.
The height of the main spur in the Berezovka-Romanov section reaches up to 90 fathoms. above sea level, but it is barely submerged. The area is flat in nature and only to the northeast of the village. Pulina is slightly hunched.
The rivers flow in shallow valleys with gentle banks; there are few swamps; Forests are found in its middle part and near Cape Romanov.
Lo m. Romanova, the width of the watershed ridge is about 25 ver. It is a slightly hilly open plain with a weak, barely noticeable slope to the north and northeast; there are few lbs and they are grouped into the form of more or less significant roshs in the Czartorya Novaya-Lyubar-Troshcha triangle.
There are many roads, but due to the clay-chernozem soil they are difficult in muddy roads.
From Romanova metro station to the Prutovka-Nov line. The width of the watershed remains the same, but its character is sharply different from the previous section: the fall of the terrain is mainly to the northeast, but the fall is so insignificant that it is not possible to catch it on the ground. The surface is covered almost half with forests, the areas cleared of forest have been cultivated. Due to the slight slope, atmospheric precipitation does not have a runoff, which is why many small swamps are formed, their bottom is hard and sandy. The predominant direction of roads is from the North-West to the South-East. The soil is sandy, although there are patches of shallow black soil. From the village New Plant to the village. The Koshelevki ridge forms a saddle; surface flat and only in the northeast has a slightly hilly character; forests make up about one-fifth of the total area. With the destruction of forests, the soil has dried out, swamps are rare and in most cases insignificant, deep and reminiscent of wet meadows; The only exception is the “Galy” swamp (to the west of the village of Prutovka), which is still a “bottomless” swamp.