The width of the valley varies between 1/3 verst and 8 versts, but in the section with. Pruss—s. Savarki valley narrows to several dozen steps, but at Lrabovka, on the contrary, it expands to 3 miles. The soil of the valley is predominantly loam. Between B.-Church and the village. Shkarovka—
sandy loam and sand. In mm B.-Church and Korsun there are rocks, below Cape Korsun there is black soil. The bottom of the valley to Cape Belaya Church is a dry meadow. From B.-Tserkov metro station to the village. Both banks of Prussia are swampy. Bolotist is also the end of the site, starting from the monastery of St. Anueria. The rest of the valley is dry and plowed near the villages. The width of the river varies between 15-50 fathoms, but sometimes expands to 250 fathoms, for example, near the village. Sakhnovki.
The depth of the river fluctuates between '/3 soots. and 3 fathoms, in the pits the depth of the river reaches 8 fathoms. The current speed is 1-6 feet. per second. The banks of the river are mostly dry, their height is 11/-2 ari!., but in places it reaches 2-3 fathoms. The river bank is partly dry and sandy. Dams near the village Pugachevka, Ostrov, Sinyava, Prusy and Savarki. All of them are deep with a viscous bottom and are impassable for fording. There are 384 permanent crossings. Of these, there are 5 ferries. There are 17 earthen mill dams, 1 stone dams. There are 9 bridges, of which one is railway at Rakov and one is stone in Korsun. The crossings are poorly maintained. There are about 10 fords. Half of them are only available at low water.
In general, for the section up to the village. It is easy to cross the Shkarovka river, since it is easy to arrange crossings. Near Sich-Rossava the river is drying up greatly; near the village Moskalenka has many fords. For the rest of the length, forcing the river will be fraught with serious difficulties, and, between the s.s. Shkarovka and Sinyava and between the monastery of St. Anueria and s. Nabutov, the swampy valley completely excludes the possibility of establishing crossings, and here the river represents a serious obstacle.
4) Ot s. Sakhnovki to the mouth (28|? verst). The right bank of the valley is gentle and covered with old coniferous forest. Lyvyy - cool between s.s. Sakhnovka and Luka are covered with deciduous trees; below p. Mikhailovka both banks almost the entire they are covered with lbs. The soil is sandy loam with an admixture of chernozem.
The width of the valley is from 1 to 3 versts. To s. Luka Dolly is a dry meadow, but right next to the river this meadow is heavily bodied. Below p. The Mikhailovka Valley is almost completely covered with forest. The soil is sandy loam.
The width of the river is from 25 to 30 fathoms, but between the words. Mezherichskaya and s. The Kononch River formed a lake, 1-2" verst and s wide. Mizhirich lies on an island. A canal 80 fathoms long and 5 fathoms long was dug on the left bank, and a rampart up to 1 arshin in height was poured on the sides. At the village In Mikhailovka, dams were built, directing all the water into a dug canal that stretches almost all the way to the river. Dn$pra past ss. N. Guzha and Khreshshatik.
Depth of the river to the village. Luka from 5 to 6 feet, below up to 1 fathom. The depth of the channels is 2-8 ars.. The current speed is 1/"-1 foot per second.
The banks of the river to the village. Mikhailovki is low-lying, overgrown with stones, and below it rises above the oxen to 1arsh. The soil is sandy loam. The bottom is muddy.
The river is impassable throughout its entire section. Periodic, and in some areas even constant, spills with a small number of permanent crossings can significantly complicate the crossing of rivers. The most convenient points for establishing new crossings are near the village. Luka and at the village. Mikhailovka.
There are three permanent crossings: two ferry crossings and one near the village. The bow is a bridge on a trestle that cannot withstand artillery fire.
The river freezes in the upper reaches in early or mid-November, and in the middle reaches in late November or early December. In the lower reaches of the river, sometimes it freezes for only two or three weeks, and then only intermittently, and sometimes it freezes with ice for four months, starting in December. It opens in the upper reaches at the beginning or end of March, in the middle reaches in the middle or end of March. During spring floods in the upper and middle reaches, water floods the entire valley. In the lower reaches it rises little. Big water
VE be lasts for 3-4 weeks, but after a week the river enters the banks.
Lzvye tributaries of the river Roshi.