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67-780: The Horyn takes its source in the Ternopil Oblast of Ukraine, south of the city of Kremenets , located north of the administrative center of the Ternopil Oblast, Ternopil . The river then flows north, where it makes s-shaped formations, through the Ukrainian oblasts of Khmelnitsky and Rivne . The river then flows northeast into the Belarusian Brest Region , where it finally flows into the Pripyat . The Khmelnytskyi atomic power plant, located near

134-541: A Lviv newspaper, but after refusal to serve in the army he moved to Mandatory Palestine . In Ukraine he published over 70 of his early works. Wet meadow A wet meadow is a type of wetland with soils that are saturated for part or all of the growing season which prevents the growth of trees and brush. Debate exists whether a wet meadow is a type of marsh or a completely separate type of wetland. Wet prairies and wet savannas are hydrologically similar. Wet meadows may occur because of restricted drainage or

201-577: A few isolated individuals affiliating with the Jewish faith . The oblast is known for its castles and fortresses. Due to the underfunding of the state program for the preservation of cultural heritage, many of objects of historical significance are in poor condition. The following historic-cultural sites were nominated for the Seven Wonders of Ukraine . The population is predominantly Ukrainophone and about 98% consider themselves Ukrainians . Among

268-516: A few of them. The Seret River (not to be confused with Siret nor Seret ) is a left tributary of the Dniester flowing through the oblast administrative center, i.e. Ternopil . Ternopil Oblast is one of two oblasts in West Ukraine that do not have an international border. It is surrounded by five other oblasts of Ukraine : Chernivtsi Oblast – to the south, Ivano-Frankivsk Oblast – to

335-556: A few weeks in the spring of 1937–1938, that is, at medium-high levels of water. The river was officially considered suitable for navigation from the mouth to Dubrovitsa, the rest was fused. During the Soviet occupation, the Styr-Horynsky River Transport Administration was created (by the middle of the 1960s the administration was called the [Styr-Horynsky River Transport Agency; in general, in

402-652: A few. Ternopil Oblast has an adequate network of highways, while the city of Ternopil is located at the intersection of main European corridors along the E50 and E85 highways. There is a small airport in Ternopil ( Ternopil Airport ) which however mostly is used for charter flights. There is a well developed railroad network which is a part of the Lviv Railways . Water transportation is very limited and mostly along

469-558: A high diversity of plant species, and may attract large numbers of birds, small mammals and insects including butterflies . Vegetation in a wet meadow usually includes a wide variety of herbaceous species including sedges , rushes , grasses and a wide diversity of other plant species. A few of many possible examples include species of Rhexia , Parnassia , Lobelia , many species of wild orchids (e.g. Calopogon and Spiranthes ), and carnivorous plants such as Sarracenia and Drosera . Woody plants , if present, account for

536-672: A minority of the total area cover. High water levels are one of the important factors that prevent invasion by woody plants; in other cases, fire is important. In areas with low frequencies of fire, or reduced water level fluctuations, or higher fertility, plant diversity will decline. Wet meadows were once common in wetland types around the world. They remain an important community type in wet savannas and flatwoods . The also survive along rivers and lakeshores where water levels are allowed to change within and among years. But their area has been dramatically reduced. In some areas, wet meadows are partially drained and farmed and therefore lack

603-614: A rail transportation hub. During German occupation, the region (except for its Volhynian portion) became part of the District of Galicia and transferred to administration by the General Government . After the war, a destroyed residential section of Ternopil, near the river, was turned into an artificial lake rather than being rebuilt. Additionally, upon annexation to the Soviet Union's Ukrainian SSR , most ethnic Poles in

670-594: A rule, graduates of the Kyiv River School), to which they hugged for 2-3 barges. There were also auxiliary boats "Hawk" and "Glukhar". In addition, almost every year the Goryna river was deepened with the help of dredgers in troubled areas. There was even a ship with a serviceman, which lifted oaks from the Goryn river, which fell to the river after the beach washed out. Such an appearance was BC (towing boats). In

737-577: A thick layer of tertiary sands, clay, marl and shellfish. Quaternary formations are represented by fluvioglacial sands and loams, as well as forests in which fertile gray forest soils and black earths are developed. Within the Polissya, moraine deposits are commonly found, usually loams with different composition of boulders, fluvioglacial sands and forest-like loams with surface cover of sod-podzolic soils; large areas are occupied by peatlands. Groundwater belongs to Devonian and Cretaceous deposits, and within

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804-403: Is 1-1.25 km per 1 km surface). The middle and lower parts of the wastewater lie in the region of a significantly marshy lowland plain of Polissya, characterized by a flat relief with sandy hills. Within the plateau, Cretaceous sands, marls, limestone and chalk occur in the form of protrusions in the valleys of rivers, lined with ancient crystalline rocks, mostly granite, and covered with

871-508: Is 300 km, the average width is 92 km, the greatest width in the middle part is 200 km, the bottom - sharply decreases to 10 km. The upper part of the basin before the confluence of the river Ustia  [ uk ] is located on the Volyn-Podilskyi hill and is a plateau with altitudes 385.5–215 m, strongly dissected by valleys of rivers and beams (the density of the narrow-girder network, according to S. Sobolev,

938-479: Is 659 km (within Ukraine - 577 km), the water intake area is 27,700 km. The general fall of the river is 218 m. The average inclination of the river is 0.33 ‰. The Horyn River originates from a spring overlooking the daily surface north-west of Volytsia village. In general, it flows from southwest to northeast and flows into the Pripyat from the right bank at 412 km from its mouth, 14 km below

1005-538: Is an oblast (province) of Ukraine . Its administrative center is Ternopil , through which flows the Seret , a tributary of the Dniester . Population: 1,021,713 (2022 estimate). One of the natural wonders of the region are its cave complexes. Although Ternopil Oblast is among the smallest regions in Ukraine, over 100 caves have been discovered there. Scientists believe these are only 20% of all possible caves in

1072-409: Is most likely to come in the middle of December, on the rolls often left the holes that are stored in places throughout the winter. The river is crumbling in the upper reaches at the end of February - beginning of March, in the middle and lower reaches 1–2 weeks later. The upper river is used as a source of hydropower and for fish breeding. Most of the basin is plowed (over 60%), forests occupy 18% of

1139-586: Is to capture and store rainwater onsite and use it as a resource to grow attractive native plants that thrive in such conditions. The Buhr Park Children's Wet Meadow is one such project. It is a group of wet meadow ecosystems in Ann Arbor, Michigan designed as an educational opportunity for school-age children. In Europe, wet meadows are sometimes managed by hay-cutting and grazing. Intensified agricultural practices (too frequent mowing, use of mineral fertilizers, manure and insecticides), may lead to declines in

1206-703: The 2002 Ukrainian parliamentary election . Over 88% of voters supported Yulia Tymoshenko of the All-Ukrainian Union "Fatherland" in the 2010 Ukrainian presidential election . By 2005, the population of the oblast had grown to roughly 225,000, consisting primarily of ethnic Ukrainians with a large Russian or Russian-speaking minority. The city of Ternopil has important institutions of higher education, including two teacher's colleges, an international medical school with instruction in English, and one of three economics institutes in Ukraine. The religion of

1273-469: The Dniester River . After 18 July 2020 Before 18 July 2020 Before the 2020 administrative reform, Ternopil Oblast was administratively subdivided into 17 raions ( districts ), as well as 1 city ( municipality ) which is directly subordinate to the oblast government: Ternopil , the administrative center of the oblast. The average area of a raion was around 808 km (312 sq mi),

1340-574: The Podilian Upland , which is known for its rocky terrain. Among noticeable mountains there are the Kremenets Mountains . The oblast is also famous for its caves. One of the major rivers in the country Dniester forms southern and southwestern borders of Ternopil Oblast with the adjacent Chernivtsi Oblast and Ivano-Frankivsk Oblast . Its tributaries that flow through the oblast include Zbruch , Seret , and Strypa among just

1407-729: The Polish-Lithuanian Commonwealth . From the First Partition of Poland in 1772 until the end of World War I the area which would become Ternopil Oblast was mostly part of the Kingdom of Galicia and Lodomeria , a possession of the Habsburg Monarchy , Austrian Empire and finally Austria-Hungary . In Ukraine today, there are three oblasts (provinces) that largely formed the eastern part of Galicia and Lodomeria until 1918. Ivano-Frankivsk Oblast

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1474-692: The Russian Volhynian Governorate (specifically the Kremenetsky Uyezd ). During the Napoleonic wars the area around Ternopil was annexed by Russia in the 1809 Treaty of Schönbrunn becoming the Tarnopolsky Krai  [ de ; pl ; ru ; uk ] ; it was ceded back to Austria in 1815 ( Congress of Vienna ). The Tarnopolsky Krai roughly covered the eastern two-thirds of the post-2022 Ternopil Raion and

1541-693: The Soviet Union invaded Poland . Due to the Polish national policy in the area ( Pacification action ), many people favored the Soviet invasion of Eastern Galicia at first. However, soon thereafter, the Soviet security agencies started a witch hunt among nationally oriented members of Ukrainian resistance who emigrated to Poland after the Soviet-Ukrainian War as well as other reasons. Many of local population were exiled to Siberia regardless of their ethnic background. On December 4, 1939,

1608-626: The Tarnopol Voivodeship at 54.8%, while there was almost no Russians . On the other hand, the Polish and Jewish population decreased drastically from 36.6% and 8.4% respectively. The economy is predominantly agriculturally oriented. Among industries, there is a well developed food industry particularly sugar production, alcohol, and dairy (such as butter). There is also number of factories such as "Vatra" (lighting equipment), Ternopil Harvester Plant, "Orion" (radio communication) among

1675-615: The Tarnopol Voivodeship , while the formerly Russian parts became part of the Volhynian Voivodeship , specifically the Krzemieniec county  [ pl ; uk ] . The southern pre-2020 raions of Ternopil Oblast were partially coterminous with Galicia and Lodomeria's districts/counties and Interwar Poland's counties. The oblast was created during the Second World War when both Nazi Germany and later

1742-922: The Ukrainian People's Republic of Soviets / Ukrainian Soviet Republic December 1917–April 1918 and the Ukrainian SSR from March 1919); from 1918 the formerly Austrian part was controlled by the West Ukrainian People's Republic (nominally part of the Ukrainian People's Republic from 22 January 1919) but ultimately the whole area fell to the Second Polish Republic in 1921 following the Ukrainian War of Independence , Polish–Ukrainian War and Polish–Soviet War . The formerly Austrian parts became part of

1809-614: The biodiversity described here. In other cases, the construction of dams has interfered with the natural fluctuation of water levels that generates wet meadows. The most important factors in creating and maintaining wet meadows are therefore natural water level fluctuations and recurring fire. In some cases, small areas of wet meadow are artificially created. Due to the concern with damage that excessive stormwater runoff can cause to nearby lakes and streams, artificial wetlands can be created to capture stormwater. Often this produce marshes, but in some cases wet meadows may be produced. The idea

1876-611: The 1970-1980's, there were three ports: Lutsk , Zarichne and Dubrovitsia , where worked in different years about 260-280 workers and transported 300-350 thousand cargoes a year). This management existed until the collapse of the USSR. At that time the river was mainly basalt and rubble from the Klesiv quarry to the Volyn region . Transportation was carried out with the help of tugs (BC - tugboat, serviceman - two people: captain and motorist, as

1943-452: The 1990s, western Ukraine remained the heartland of Ukrainian political and cultural nationalism, and the political affiliations of Ternopil voters reflected that viewpoint. In the first elections after independence, the People's Movement of Ukraine was the leading party in the oblast. A majority of oblast voters supported the Ukrainian nationalist-oriented Electoral Bloc Yuliya Tymoshenko in

2010-659: The Chortkiv Raion up to the Strypa ; in pre-2020 terms it corresponded with the cities of Ternopil and Chortkiv and the Borshchiv, Chortkiv, Husiatyn, Pidvolochysk, Terebovlia, Ternopil and Zalishchyky raions, the southern half of Zbarazh raion, the eastern and northern parts of Buchach raion and some eastern parts of Zboriv and Kozova raions. From 1917 the formerly Russian part came under the Ukrainian People's Republic ( Ukrainian State April–December 1918; also claimed by

2077-553: The Goryn basin in the Khmelnitsky NPP area: Monograph [Electronic resource] / Ed. VK Khilchevsky. - K.: Nika-center, 2011. - 176 p. - ISBN   978-966-521-551-6 . Ichthyofauna cadastre of the Rivne region / Grohovskaya Yu.R., Volovik G.P., Konontsev S.V. and others; Ed. Moshinsky V. S. and Grohovskaya Yu. R. - Rivne: Doka-center, 2012. - 200 p. Romanchuk O. River Goryn: Past and Present. Horyń // Geographical Commonwealth of

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2144-631: The Kremenets, Zbarazh and Lanovetsky districts of the Ternopil region , Bilogirsky, Izyaslavsky and Slavutsky districts of the Khmelnytskyi region , as well as Ostroh, Goshcha, Rivne, Kostopil, Sarny, Volodymyrets and Dubrovytsia districts of the Rivne region . Due to economic activity in the basin, there are crisis situations. The first of these is the placement of the Khmelnitsky NPP in

2211-835: The Poles in the Polish and Slavic countries. - Warszawa: Filip Sulimierski i Władysław Walewski, 1882. - T. III: The Hague - Kępy. (floor) - S. 157–159. (floor) The wikiservice has multimedia data on the subject: Goryn (river) National Nature Park "Podilsky Tovtry". Inland waters of the Ternopil region. Fishing in the Rivne region. Rare species of roundworms and fish of the Rivne region. Ternopil Oblast Ternopil Oblast ( Ukrainian : Тернопільська область , romanized :  Ternópilʹsʹka óblastʹ ), also referred to as Ternopilshchyna ( Ukrainian : Тернопільщина , romanized :  Ternópilʹščyna ) or Ternopillia ( Ukrainian : Тернопілля , romanized :  Ternopíllja ),

2278-462: The Polkva River is 3–10 m, below - 25–60 m, the largest - 19 m (the outskirts of the village of Vorona), the smallest - 0.5 m (village Mala Goryanka). Depths are distributed unevenly; on the plains 1.4-2.5 m, in places up to 5–11 m, on rolls down to 0.3–1 m. The velocities of the flow on the valleys are insignificant (0.1-0.3 m/s), on rocks are increasing to 0.5-1.3 m/s. The river Horyn basin on

2345-484: The barges do not carry the tug, either on the shallow or close to the shore, a certain cargo was attached to the last barga, i.e. "Dragons", which stretched the bottom of Gorin. Of course, this had a negative impact on river flora and fauna , especially during spawning . From the city of David-Gorodok to the mouth of the river navigable Rivers of the Ternopil region Rivers of Khmelnitsky region Rivers of Rivne region Top ↑ Gorbunov E. Yu., Matulevskaya T. The origin of

2412-477: The basin, marshes - shallow cane and shrubland - were drained by 6%. Floodplain meadows are partially sown, cultivated or under grazing, which leads to their degradation, as well as flushing at high water in the river bed of significant impurities - organic, bacterial and solid runoff. During the occupation of the Second Rzeczpospolita on the territory of Ukraine , the navigable Horyn was only

2479-475: The biggest minorities are Poles and Russians who combine 1.6% of the total population. Most of the population is bilingual and the Ukrainian language is accepted in daily communications. The estimated population is 1,038,694 (2020 est.) In historical comparison, before World War II national composition was very different and according to the 1931 Polish Census Ukrainians were a slight majority in

2546-430: The biggest one was Terebovlia Raion covering 1,130 km (440 sq mi) and the smallest one - Pidhaitsi Raion with 496 km (192 sq mi). The average population number was around 50.6 thousands which is just below the national average. In town of Buchach was born a Nobel Prize recipient, writer Shmuel Yosef Agnon . The prize was given for works about fate of Galician Jews . Agnon worked for

2613-607: The city of David-Gorodok , at an altitude of 127 m above sea level. Within 28 km from the mouth, the river splits into two branches, of which the main is right; the left 26-mile long branch flows into the Pripyat at 417 km. The Horyn basin borders on the west with the Sturo basins, on the east with the Uborti and Svvi basins, and in the south with the Dniester basin. The outcrop area has an incorrect pear-like shape; its length

2680-510: The city of Netishyn , uses water from the Horyn for its cooling processes. Before the river was dammed , which created pollution, it was used for irrigation and fishing. A clean-up effort in September 1996 was a step towards the river's restoration. Cities and towns located on the river include Iziaslav , Slavuta , Netishyn , Ostroh , Dubrovytsia , Rechytsa , and Stolin . The length

2747-570: The city of Rivne and discharges of sewage from the Orzhiv wood-processing plant below the mouth of the Ustya River. In general, the formation of the quality of river basin waters is determined by the salt background (chlorides), nutrient-phosphate compounds, channel erosion, toxic impurities (copper). According to the complex ecological index, the river in the mouth part can be attributed to the class of moderately polluted rivers and transitional to

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2814-407: The contaminated. The quality of river waters worsen periodic discharges (emergency) of sewage from sugar factories (Ostrozky, Babino-Tomahovsky, Mizotsky). The Horyn hill in the upper part of the current is moderately vorticular, in the middle and lower, it is strongly winding (the radius of curvature of the gentes in places reaches 20–40 m), mostly unbranched. The width of the river to the mouth of

2881-438: The crystalline massif they are bound to cracks in crystalline rocks. Within the limits of Polissya, the depth of groundwater is insignificant. Most of the surface of the pool is plowed; Forests covering 1950 km (18%) are prevalent in the lower reaches and consist of pine trees with oak impurities; In the upper reaches are broadleaved forests (oak, hornbeam, maple, ash), preserved along the slopes of river valleys and beams. In

2948-461: The groundless collection of underground water for drinking water supply in the city of Rivne. The intense infiltration in the groundwater aquifers of the surface runoff enhances the channeling of the channel and degradation of the river ecosystem. Supplements the formation of the crisis situation in the Gorin River pollution of industrial and stormwater from the chemical association "Azot" below

3015-480: The hydrographic map of Ukraine The bed is slightly overgrown with reeds, sedges and algae, mostly offshore, with a strip of 3–5 m; in the lower reaches, littered with sunken logs, rags and trees that fell from the shores. The bottom is mostly sandy, on rolls sometimes covered with pebbles, on the plains are silted; in the upper reaches on separate stony areas. Shore a height of 1 to 6 m, mostly steep or steep, on alternating places alternating with flat and very flat, in

3082-402: The level of spring full-bird. In October, the rise of the water level, which lasts until the ice age begins; after freezing the level is reduced, but remains above the summer. In winter, when flooding occurs, there are floods, a height of 0.5-2.5 m. The most abundant river is in the spring (III-IV), when it passes 42-54% of annual drain, for the summer and autumn (VI-XI) it accounts for 31-39%, for

3149-402: The lower reaches a considerable area is occupied by low-lying reed beds and shallow bogs, the total area of which is 1700 km (6%). Somewhere there are lands covered with meadow vegetation. The lakes in the basin are very small (0.1%). The river network is well developed, thanks to the climatic conditions and the nature of the soil. The density of the river network without taking into account

3216-457: The majority is Ukrainian Greek Catholic , though there is a notable Orthodox presence and a small Protestant minority. Many churches which were closed or destroyed under Soviet rule have rebuilt since independence. The local Jewish community, which was very large before 1939, disappeared in the Holocaust and was not reestablished after 1945. There are no active synagogues in the oblast and only

3283-611: The names of the largest rivers of Ukraine // Language culture of a specialist in the context of modernity / Collection of materials of the III Interuniversity student's scientific and practical conference. - Donetsk: DonNTU, 2010. - C. 92–93. Up ↑ Hydroecological state of the Goryn basin in the Khmelnitsky NPP area: Monograph [Electronic resource] / Ed. VK Khilchevsky. - K.: Nika-center, 2011. - 176 p. - ISBN   978-966-521-551-6 . Top ↑ I. B. Horyn // Chronicle of Volyn. - 1956. - No. 3. - p. 83 Hydroecological state of

3350-421: The places of Horyn, where there were ferry crossings (near the villages of Velyun and Vysotsk Dubrovitsky district), the servicing of the towing boat was preceded by an acoustic signal. so that a ferry cable could be lowered to the bottom of the river by ferry crossing. After passing the tug, the cable was raised and the ferry could be continued. Due to the fact that Gorin is a relatively not very wide river and that

3417-665: The receipt of large amounts of water from rain or melted snow. They may also occur in riparian zones and around the shores of large lakes. Unlike a marsh or swamp , a wet meadow does not have standing water present except for brief to moderate periods during the growing season. Instead, the ground in a wet meadow fluctuates between brief periods of inundation and longer periods of saturation . Wet meadows often have large numbers of wetland plant species, which frequently survive as buried seeds during dry periods, and then regenerate after flooding. Wet meadows therefore do not usually support aquatic life such as fish. They typically have

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3484-575: The region were forcibly relocated to Poland, whose national borders had shifted far to the west. The area of the former Polish voivodeship was expanded by adding territory in the north, though the westernmost parts were transferred to the Lviv oblast . After 1945 Soviet authorities also encouraged ethnic Russians to settle in territories newly annexed to the Soviet Union, including the Ternopil oblast, though western Ukraine remained considerably less Russian than eastern Ukraine. As Ukraine achieved independence in

3551-552: The region. The biggest cave is Optymistychna Cave . Measuring 267 km (166 mi) in total length, it is the longest cave in Eurasia and the fifth-longest in the world . Twenty percent of the land in the region is chernozem soil. Among its attractions, Ternopil Oblast has 34 castles. By at least one account, the most prominent is the Zbarazh Castle with fortifications that expand over 16 ha (40 acres) and

3618-455: The rivers, up to 10 km long, is 0.26, and the latter account is 0.46. Sloping and moderately steep slopes are usually planted, steep - covered or covered with mixed forest and shrub. In the lower reaches are marshy meadows. In the upper reaches, the slopes are composed of limestone and chalky rocks, covered with sandy loam and loam, often exposed to the appearance of ancient crystalline rocks; in other areas they are mostly sandy and sandy. In

3685-559: The slopes, the lower part of it is marshy and is a wet meadow . Soils are muddy-sandy and clay, in wetlands peaty. Annually in the period of spring water and rain floods the floodplain is flooded to a depth of 0.5 to 3.3 m for 1–2 weeks; In reduced areas, water is contained within 1–3 months Cities: Lanivtsi , Izyaslav , Slavuta , Netishyn , Ostroh , Dubrovytsia , Stolin , David-Gorodok . Urban-type settlements: Vyshnivets , Yampil , Bilohiria , Hoshcha , Orzhiv , Stepan , Rychytsya, Oleksandria, and Derazhne. The river flows through

3752-399: The southwest, Lviv Oblast – to the northwest, Rivne Oblast – to the north, and Khmelnytskyi Oblast – to the east. Historic administrative affiliation of the area: From the 12th century the area belonged to Galicia–Volhynia until Galicia–Volhynia was incorporated into the Kingdom of Poland and Grand Duchy of Lithuania in the 14th century. In 1569 Poland and Lithuania united into

3819-635: The spring often begins in March, and rarely in February, it occurs intensively (up to 0.5-1.0 m/day) and in the middle or second half of March the highest level reaches for the normal full-length 0.8-4.6 m, with exceptionally high - 1.2-5.8 m. As a rule, a full-blooded animal passes one peak and very rarely two. The recession is slow, within one to two months, and of course, at the end of May–June, there are setbacks. Rains that fall almost year-round cause floods to grow at an average of 0.5-1.5 m, and rarely reaching

3886-541: The upper and middle flows, there is no energy exchange between the channel and the floodplain , the phenomena of stagnation have developed. From the aquatic ecosystem, a group of macrophytes disappears, first of all rhest, ai, and jugs. The second of these problems is the processes of extended depression of groundwater formed in the Cretaceous-Marl region (the Goshchansk-Ostrozhsky region) due to

3953-402: The upper and middle streams of the river on both slopes (alternating along the banks) at a height of 3–8 m above the river are located terraces, wide from 0.3 to 4 km, with a steep ledge, a height of 5–10 m. Their surface is predominantly smooth, plowed, rarely covered with pine or mixed forests. In the upper reaches of the river at the foot of the slopes there are leaks of groundwater. In

4020-524: The upper part they are often peaty, hermetic, less rocky or loamy, on other segments sand or sandy-clay, washed out by water and, collapse, collapse into the river, along with shrubs that grow on them, and separate trees. In many places, they merge with the slopes of the valley. The river is mostly snowy with a significant participation of rain and earth. In the course of the year, high spring floods, low summer currents, disturbed by short-term rain floods, autumn and winter rise of water are allocated. The rise in

4087-598: The upper reaches (on the border of the Khmelnytsky and Rivne regions). Due to the unsolved problem of technical water supply from the Southern Bug River, the NPP relieves the peak flood values, leaving only the minimum runoff in the channels of the channel. This leads to the development of channel erosion, siltation of wintering pits, channeling channels. As a result, during the years there was no observed flood in

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4154-413: The upper reaches of the river, the floodplain is waterlogged, is covered mostly with meadow-bog vegetation, less often with shrubs and individual trees. In other areas, it is mostly dry, meadow, strongly overwhelmed by elders, gullies and lakes, along the banks of which there are thick thickets of cane and shrub (willow, weeping willow). There are sandy ridges and separate hills, with a height of 1 to 8 m. At

4221-619: The village. Antonivka - 3.81 L/s with 1 km in the village. Gorin - 3.56 dm/s with 1 km. The mineralization of the water of the Horyn River in the vicinity of the Khmelnitsky NPP is as follows: spring flood - 502 mg/dm3; summer-autumn measurements - 455 mg/dm; Winter Meadows - 567 mg/dm. The mineralization of the water of the reservoir-cooler of Khmelnitsky NPP is: spring flood - 396 mg/dm3; summer-autumn measurements - 401 mg/dm; winter barges - 405 mg/dm. Type of water - hydrocarbonate-calcium. [2] The ice

4288-526: The voivodeship division in the West Ukraine was abolished and replaced with the existing Soviet administrative division oblast. Ternopil Oblast (originally Tarnopol Oblast) was established based mostly on the Tarnopol Voivodeship and southern portions of the Volhynian Voivodeship . During the invasion of the Soviet Union by Nazi Germany , Ternopil became an object of fierce fighting between Soviet and German forces because of its importance as

4355-434: The winter (XII-II) - 15-21%. The largest water consumption of the water-rich 1932 near the village. Voloshka was 1108 m/s, near the village. Antonovka 1610 m/sec, corresponding to drainage modules 162 and 142 dm/s with 1 km. The lowest runoff modules in summer and winter do not exceed 0.4-1.2 dm/s with 1 km. The average annual drainage module is multi-yearly near the village. Voloshki - 3.96 L/s with 1 km, near

4422-471: Was entirely contained in the kingdom, as was the vast majority of Lviv Oblast (only a few small areas and villages near Sokal were not). The southern and central parts of Ternopil Oblast were within the kingdom while the northern parts (pre-2020 raions: Kremenets , Shumsk , Lanivtsi and the northern half of Zbarazh ; post-2020: Kremenets Raion and small parts of Ternopil Raion ) remained with Poland Lithuania; from 1795 ( Third Partition ) they belonged to

4489-554: Was the center of a 17th-century standoff between troops of Bohdan Khmelnytsky and the army of the Polish–Lithuanian Commonwealth . The Dniester Canyon passes through the oblast; it is considered one of the wonders of Ukraine, stretching for 250 km (160 mi). The oblast is located in Western Ukraine and has an area of 13,800 km (5,300 sq mi). It is situated at the western part of

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