The slopes, mostly open and shallow, are steeper here; Here there are more beams, cracks and grooves, which turn into ravines as a result of the eroding activity of water and looseness of the soil. South-eastern slopes of the watershed, halfway close to the river. Irpen, they descend quite steeply, sometimes even precipitously, into the valley of the said river. In this regard, attention should be paid to the area between the s.s. Tomashevka and Sosnovka, where the height of the cliffs reaches 10 soots. Farther to the northeast, the area becomes flat and somewhat hilly until the Kev---7Kitomir highway and transitions into the lowlands to the north of the latter. The area with the greatest hilliness is the one from the northern line. Lishnya - Pashkovka - Packing to the indicated highway, but the terrain here also has an easy outline and all the descents and ascents are convenient for the movement of all types of troops in almost any weather. Only the right bank of the river differs in some steepness. Move from Staritskaya mill to Makarov metro station.
The soil is sandy loam in places with a large amount of black soil.
c) Vodorazdl river Zdvizha and Teterev.
Starting at Yaropovichi, is a slightly hilly plain, passing to the square from the K!ev-_Brest highway into the Polesya lowland. Passing close along the left bank of the river. As it moves, this volorazdfl forms a steep, hilly left bank of the Russian River, steep to the Staritskaya Mill site, Makarov metro station. To the northwest, this watershed passes into the above-mentioned lowland.
The soil is sandy loam. Mostly clean sand.
4) Vodorazdl r.r. Namenni and Rastovitsy.
Taking the direction from m. Yesterday to the village. Novoselitsa, Polovetskoe metro station, near the first of the named Vodorazdfl mudflows e [9 separate the spur to the southeast, which is the watershed of the river. Subod and Rastovitsy. Wed. water distribution height 103.6 soot. The highest altitude is 4 versts northeast of the village. Andryushki 111.5 fathoms. Walking along the right bank of the river. Kamenka, called the watershed, with its northern slopes steeply descends into the valley of this river, and its southern slopes gently towards the river. Rastovitz. The area to the east of the N.S. line is characterized by the greatest oversaturation. Yakhny-Stavishe. Here it is necessary to clear out the ravine to the east of the village. Zubari and Kozhanki are distinguished by their sizes up to 10 soots deep. and width up to 30-50 fathoms. The northern and southern slopes are riddled with ravines, gullies and hollows, which are the beds of tributaries of the river. Kamenki and Rastovitsy. The above-mentioned spur, branching off to the southeast, gradually decreases and with its slopes gently descends to the river. Subod and Rastovica. Both to the northeast and to the southeast the slopes are steep and similar in nature to the just described slopes of the watershed. The soil is loamy.
5) Vodorazdl river basins Irpen, Stugny and Dnepr.
Having separated from the main branch at Cape Fastov, the watershed goes first to the northeast and then to the turn of the river. Unava also turns north in this direction, making the right bank of the river mountainous with steep, sometimes steep slopes. Unava; In this area, the watershed is characterized by the greatest diversity.
Steep slopes of the valley, steep banks of rivers and streams, right tributaries of the river. Unavoids, cracks and grooves replace each other throughout the entire length from the Fastov metro station to the turn of the river. Unfortunately, it makes the area inconvenient for the movement of troops and military loads. The average height is 101.7 fathoms. The largest is near Cape Fastov 108.1 fathoms.
Having reached the village. Plisetsky, the water supply turns east and near the villages. Malaya-Bugaevka takes a steep direction again to the north, in the direction! and to the north. Yankovici—Vjfta—
Bratskaya-Borshchagovka. (Average height is about 91 fathoms). The highest point is 3 versts northwest of the village. M. Bugaevka 93.5 fathoms. The eastern slopes are cut by deep, wide and long ravines with steep banks. These same slopes abruptly, in some places, abut the river. Ln$pr, forming the right mountainous bank of the river. The western slopes are gentle.
The soil is predominantly sandy loam. In the northern part along the Irpen valleys there is sand.
6) Vodorazdl r.r. Rossavy and Rossi.