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Gatchinsky District

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Gatchinsky District ( Russian : Га́тчинский райо́н ) is an administrative and municipal district ( raion ), one of the seventeen in Leningrad Oblast , Russia . It is located in the southwestern central part of the oblast and borders with Krasnoselsky , Moskovsky , and Pushkinsky Districts of the federal city of St. Petersburg in the north, Tosnensky District in the east, Luzhsky District in the south, Volosovsky District in the west, and with Lomonosovsky District in the northwest. The area of the district is 2,868.7 square kilometers (1,107.6 sq mi). Its administrative center is the town of Gatchina . Population (excluding the administrative center): 140,210 ( 2010 Census ) ; 132,010 ( 2002 Census ); 138,022 ( 1989 Soviet census ) .

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47-625: The northern part of the district is essentially a mixture of urban areas - suburbs of Saint Petersburg - and summer house areas. The central and the southern parts are forested. Much of the area of the district belongs to the drainage basin of the Luga River , a tributary of the Gulf of Finland . The main tributary of the Luga within the district is the Oredezh River . Minor areas in the east of

94-427: A hierarchical pattern . Other terms for a drainage basin are catchment area , catchment basin , drainage area , river basin , water basin , and impluvium . In North America, they are commonly called a watershed , though in other English-speaking places, "watershed" is used only in its original sense, that of the drainage divide line. A drainage basin's boundaries are determined by watershed delineation ,

141-437: A common task in environmental engineering and science. In a closed drainage basin, or endorheic basin , rather than flowing to the ocean, water converges toward the interior of the basin, known as a sink , which may be a permanent lake, a dry lake , or a point where surface water is lost underground . Drainage basins are similar but not identical to hydrologic units , which are drainage areas delineated so as to nest into

188-454: A drainage basin, and there are different ways to interpret that data. In the unlikely event that the gauges are many and evenly distributed over an area of uniform precipitation, using the arithmetic mean method will give good results. In the Thiessen polygon method, the drainage basin is divided into polygons with the rain gauge in the middle of each polygon assumed to be representative for

235-540: A drainage boundary is referred to as watershed delineation . Finding the area and extent of a drainage basin is an important step in many areas of science and engineering. Most of the water that discharges from the basin outlet originated as precipitation falling on the basin. A portion of the water that enters the groundwater system beneath the drainage basin may flow towards the outlet of another drainage basin because groundwater flow directions do not always match those of their overlying drainage network. Measurement of

282-602: A multi-level hierarchical drainage system . Hydrologic units are defined to allow multiple inlets, outlets, or sinks. In a strict sense, all drainage basins are hydrologic units but not all hydrologic units are drainage basins. About 48.71% of the world's land drains to the Atlantic Ocean . In North America , surface water drains to the Atlantic via the Saint Lawrence River and Great Lakes basins,

329-521: A short time by the future author Vladimir Nabokov , is located in the selo of Rozhdestveno and is a museum. Another museum was open in the village of Vyra , where Station Master , the short story by Pushkin from The Belkin Tales , takes place. The museum reconstructs the postal station of the 19th century. The village of Kobrino hosts one more museum related to Pushkin. The former Gannibal estate in Suyda

376-462: A town of oblast significance. Between September 1941 and January 1944 the area of Krasnogvardeysky District was occupied by German troops. On January 28, 1944 Krasnogvardeysk was renamed Gatchina, and the district was renamed Gatchinsky. In 1963—1965, Lomonosovsky District was merged into Gatchinsky District, while at the same time parts of Gatchinsky District were transferred to Luzhsky District . In 1965, however, Gatchinsky District

423-487: Is referred to as " watershed management ". In Brazil , the National Policy of Water Resources, regulated by Act n° 9.433 of 1997, establishes the drainage basin as the territorial division of Brazilian water management. When a river basin crosses at least one political border, either a border within a nation or an international boundary, it is identified as a transboundary river . Management of such basins becomes

470-614: Is the Dead Sea . Drainage basins have been historically important for determining territorial boundaries, particularly in regions where trade by water has been important. For example, the English crown gave the Hudson's Bay Company a monopoly on the fur trade in the entire Hudson Bay basin, an area called Rupert's Land . Bioregional political organization today includes agreements of states (e.g., international treaties and, within

517-713: The African Great Lakes , the interiors of Australia and the Arabian Peninsula , and parts in Mexico and the Andes . Some of these, such as the Great Basin, are not single drainage basins but collections of separate, adjacent closed basins. In endorheic bodies of water where evaporation is the primary means of water loss, the water is typically more saline than the oceans. An extreme example of this

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564-607: The Eastern Seaboard of the United States, the Canadian Maritimes , and most of Newfoundland and Labrador . Nearly all of South America east of the Andes also drains to the Atlantic, as does most of Western and Central Europe and the greatest portion of western Sub-Saharan Africa , as well as Western Sahara and part of Morocco . The two major mediterranean seas of the world also flow to

611-679: The Gatchina Museum Reserve . It was opened to public in 1918, strongly damaged during World War II, then closed for restoration, and only reopened in 1976. The other two museums in Gatchina are the Museum-House of artist Pavel Shcherbov , which is itself an architectural monument built in the modernist style, and the Museum of Aviation Motor Construction, located at the motor plant. The Rozhdestveno Memorial Estate , owned for

658-735: The Mississippi (3.22 million km ), and the Río de la Plata (3.17 million km ). The three rivers that drain the most water, from most to least, are the Amazon, Ganges , and Congo rivers. Endorheic basin are inland basins that do not drain to an ocean. Endorheic basins cover around 18% of the Earth's land. Some endorheic basins drain to an Endorheic lake or Inland sea . Many of these lakes are ephemeral or vary dramatically in size depending on climate and inflow. If water evaporates or infiltrates into

705-809: The Nile River ), Southern , Central, and Eastern Europe , Turkey , and the coastal areas of Israel , Lebanon , and Syria . The Arctic Ocean drains most of Western Canada and Northern Canada east of the Continental Divide , northern Alaska and parts of North Dakota , South Dakota , Minnesota , and Montana in the United States, the north shore of the Scandinavian peninsula in Europe, central and northern Russia, and parts of Kazakhstan and Mongolia in Asia , which totals to about 17% of

752-631: The Treaty of Stolbovo , the area was transferred to Sweden, and in the 1700s, during the Great Northern War , it was conquered back by Russia. The city of Saint Petersburg was founded in 1703. In the course of the administrative reform carried out in 1708 by Peter the Great , the area was included into Ingermanland Governorate (known since 1710 as Saint Petersburg Governorate ). It was later split between Tsarskoselsky and Petergofsky Uyezds ;

799-549: The groundwater . A drainage basin is an area of land where all flowing surface water converges to a single point, such as a river mouth, or flows into another body of water, such as a lake or ocean. Luzhsky Uyezd Luzhsky Uyezd ( Russian : Лужский уезд ) was one of the eight subdivisions of the Saint Petersburg Governorate of the Russian Empire . Its capital was Luga . Luzhsky Uyezd

846-789: The Andes. The Indian Ocean 's drainage basin also comprises about 13% of Earth's land. It drains the eastern coast of Africa, the coasts of the Red Sea and the Persian Gulf , the Indian subcontinent , Burma, and most parts of Australia . The five largest river basins (by area), from largest to smallest, are those of the Amazon (7 million km ), the Congo (4 million km ), the Nile (3.4 million km ),

893-726: The Atlantic. The Caribbean Sea and Gulf of Mexico basin includes most of the U.S. interior between the Appalachian and Rocky Mountains , a small part of the Canadian provinces of Alberta and Saskatchewan , eastern Central America , the islands of the Caribbean and the Gulf, and a small part of northern South America. The Mediterranean Sea basin, with the Black Sea , includes much of North Africa , east-central Africa (through

940-623: The US, interstate compacts ) or other political entities in a particular drainage basin to manage the body or bodies of water into which it drains. Examples of such interstate compacts are the Great Lakes Commission and the Tahoe Regional Planning Agency . In hydrology , the drainage basin is a logical unit of focus for studying the movement of water within the hydrological cycle . The process of finding

987-564: The administrative center located in Gatchina . On February 14, 1923 Gatchina was renamed Trotsk, and Gatchinsky Uyezd was renamed Trotsky Uyezd, after Leon Trotsky . On August 1, 1927, the uyezds were abolished and Trotsky District, with the administrative center in the town of Trotsk, was established. The governorates were also abolished, and the district was a part of Leningrad Okrug of Leningrad Oblast . It included parts of former Trotsky Uyezd. On August 2, 1929, after Trotsky

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1034-406: The basin, it can form tributaries that change the structure of the land. There are three different main types, which are affected by the rocks and ground underneath. Rock that is quick to erode forms dendritic patterns, and these are seen most often. The two other types of patterns that form are trellis patterns and rectangular patterns. Rain gauge data is used to measure total precipitation over

1081-430: The discharge of water from a basin may be made by a stream gauge located at the basin's outlet. Depending on the conditions of the drainage basin, as rainfall occurs some of it seeps directly into the ground. This water will either remain underground, slowly making its way downhill and eventually reaching the basin, or it will permeate deeper into the soil and consolidate into groundwater aquifers. As water flows through

1128-690: The district are pig and poultry breeding. Two railroads cross the district from north to south. One connects Saint Petersburg with Dno and Nevel . Another one originates in Saint Petersburg, passes Gatchina, and proceeds to Luga and Pskov . Another railroad in the northern part of the district encircles Saint Petersburg from the south. It originates in Mga , passes Gatchina and proceeds west to Volosovo and Tallinn . All these railways have both suburban and long-distance passenger service. The M20 highway connecting Saint Petersburg and Pskov, crosses

1175-844: The district belong to the basin of the Tosna River , and the northern part of the district, including the town of Gatchina, belongs to the basin of the Izhora River . Both the Tosna and the Izhora are left tributaries of the Neva . Minor areas in the northwest in the district belong to the basin of the Strelka River , also a tributary of the Gulf of Finland. In the south of the district, the Mshinskoye Boloto Zakaznik

1222-480: The district from north to south. South of the town of Gatchina, it crosses the A120 highway, which encircles Saint Petersburg and crosses the district from east to west. A paved road connects Gatchina with Kingisepp via Volosovo. There are also local roads. The bus traffic in the district was opened in 1936, when a bus line connected Leningrad and Siversky . In 1940, passenger bus connection between Gatchina and Leningrad

1269-441: The drainage area is dependent on the soil type. Certain soil types such as sandy soils are very free-draining, and rainfall on sandy soil is likely to be absorbed by the ground. However, soils containing clay can be almost impermeable and therefore rainfall on clay soils will run off and contribute to flood volumes. After prolonged rainfall even free-draining soils can become saturated , meaning that any further rainfall will reach

1316-697: The drainage basin to the mouth, and may accumulate there, disturbing the natural mineral balance. This can cause eutrophication where plant growth is accelerated by the additional material. Because drainage basins are coherent entities in a hydrological sense, it has become common to manage water resources on the basis of individual basins. In the U.S. state of Minnesota , governmental entities that perform this function are called " watershed districts ". In New Zealand, they are called catchment boards. Comparable community groups based in Ontario, Canada, are called conservation authorities . In North America, this function

1363-493: The governorate was accordingly renamed Petrogradsky in 1913 and Leningradsky in 1924. Gatchina was chartered in 1796. It frequently was a residence of Russian Tsars, for instance, Pavel I grew up in Gatchina, and Alexander III lived almost exclusively there. On November 20, 1918 Tsarskoye Selo was renamed Detskoye Selo, and the uyezd was renamed Detskoselsky. On February 14, 1923 Detskoselsky and Petergofsky Uyezds were abolished and merged into Gatchinsky Uyezd , with

1410-435: The ground and along rivers it can pick up nutrients , sediment , and pollutants . With the water, they are transported towards the outlet of the basin, and can affect the ecological processes along the way as well as in the receiving water body . Modern use of artificial fertilizers , containing nitrogen (as nitrates ), phosphorus , and potassium , has affected the mouths of drainage basins. The minerals are carried by

1457-781: The ground at its terminus, the area can go by several names, such playa, salt flat, dry lake , or alkali sink . The largest endorheic basins are in Central Asia , including the Caspian Sea , the Aral Sea , and numerous smaller lakes. Other endorheic regions include the Great Basin in the United States, much of the Sahara Desert , the drainage basin of the Okavango River ( Kalahari Basin ), highlands near

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1504-418: The rainfall on the area of land included in its polygon. These polygons are made by drawing lines between gauges, then making perpendicular bisectors of those lines form the polygons. The isohyetal method involves contours of equal precipitation are drawn over the gauges on a map. Calculating the area between these curves and adding up the volume of water is time-consuming. Isochrone maps can be used to show

1551-631: The responsibility of the countries sharing it. Nile Basin Initiative , OMVS for Senegal River , Mekong River Commission are a few examples of arrangements involving management of shared river basins. Management of shared drainage basins is also seen as a way to build lasting peaceful relationships among countries. The catchment is the most significant factor determining the amount or likelihood of flooding . Catchment factors are: topography , shape, size, soil type, and land use (paved or roofed areas). Catchment topography and shape determine

1598-461: The river rather than being absorbed by the ground. If the surface is impermeable the precipitation will create surface run-off which will lead to higher risk of flooding; if the ground is permeable, the precipitation will infiltrate the soil. Land use can contribute to the volume of water reaching the river, in a similar way to clay soils. For example, rainfall on roofs, pavements , and roads will be collected by rivers with almost no absorption into

1645-418: The speed with which the runoff reaches a river. A long thin catchment will take longer to drain than a circular catchment. Size will help determine the amount of water reaching the river, as the larger the catchment the greater the potential for flooding. It is also determined on the basis of length and width of the drainage basin. Soil type will help determine how much water reaches the river. The runoff from

1692-415: The time taken for rain to reach the river, while catchment size, soil type, and development determine the amount of water to reach the river. Generally, topography plays a big part in how fast runoff will reach a river. Rain that falls in steep mountainous areas will reach the primary river in the drainage basin faster than flat or lightly sloping areas (e.g., > 1% gradient). Shape will contribute to

1739-477: The time taken for runoff water within a drainage basin to reach a lake, reservoir or outlet, assuming constant and uniform effective rainfall. Drainage basins are the principal hydrologic unit considered in fluvial geomorphology . A drainage basin is the source for water and sediment that moves from higher elevation through the river system to lower elevations as they reshape the channel forms. Drainage basins are important in ecology . As water flows over

1786-789: The world's land. Just over 13% of the land in the world drains to the Pacific Ocean . Its basin includes much of China, eastern and southeastern Russia, Japan, the Korean Peninsula , most of Indochina, Indonesia and Malaysia, the Philippines, all of the Pacific Islands , the northeast coast of Australia , and Canada and the United States west of the Continental Divide (including most of Alaska), as well as western Central America and South America west of

1833-457: Was abolished and split between Luzhsky and Gatchinsky Districts. On August 19, 1936 Slutsky District was established. It included some areas from abolished Leningradsky Prigorodny District and from Tosnensky District. On June 23, 1939 parts of Krasnogvardeysky District were transferred to Slutsky District. On April 23, 1944 Slutsk was renamed Pavlovsk, and the district was renamed Pavlovsky. On July 25, 1953 Pavlovsky District

1880-492: Was abolished and split between the city of Leningrad, Gatchinsky, and Tosnensky Districts. In 2011, industry was responsible for 73.7% GDP of the district. There are several enterprises related to timber industry, including two paper mills (30.4% of the GDP in 2011) and to food industry (30.1%), as well as a plant producing airplane motors and another one producing diverse electric equipment. The main specializations of agriculture in

1927-512: Was also transformed into a museum in 1999. Drainage basin A drainage basin is an area of land in which all flowing surface water converges to a single point, such as a river mouth , or flows into another body of water , such as a lake or ocean . A basin is separated from adjacent basins by a perimeter, the drainage divide , made up of a succession of elevated features, such as ridges and hills . A basin may consist of smaller basins that merge at river confluences , forming

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1974-558: Was created to protect the swamp landscape with the pine-tree forest. The zakaznik is shared with Luzhsky District. Originally, the area of the district was populated by Finnic peoples , in particular, the Izhorians . From the 9th century, the area was changing hands between Novgorod Republic (from the 15th century, the Grand Duchy of Moscow ), and Sweden . Gatchina was first mentioned under 1499 as Khotchino. In 1617, according to

2021-404: Was deported from Soviet Union, Trotsk was renamed Krasnogvardeysk, and the district was renamed Krasnogvardeysky. On July 23, 1930, the okrugs were abolished as well, and the districts were directly subordinated to the oblast. In the 1930s, some areas from Oraniyenbaumsky and Luzhsky Districts were transferred to Krasnogvardeysky District. On October 3, 1938 Krasnogvardeysk was designated

2068-601: Was located in the southwestern part of the governorate (in the southwestern part of present-day Leningrad Oblast and in the northeastern part of Pskov Oblast ). At the time of the Russian Empire Census of 1897, Luzhsky Uyezd had a population of 133,466. Of these, 91.7% spoke Russian , 3.6% Estonian , 1.3% Latvian , 0.8% Finnish , 0.7% Polish , 0.7% German , 0.5% Ingrian , 0.4% Yiddish , 0.1% Belarusian , 0.1% Romani and 0.1% Lithuanian as their native language. This Russian location article

2115-558: Was opened. The district contains 221 cultural heritage monuments of federal significance (120 of them in the town of Gatchina) and additionally 447 objects classified as cultural and historical heritage of local significance (172 of them in the town of Gatchina). The federal monuments include the ensembles of the Gatchina Palace and the Priory Palace , with surrounding parks, in Gatchina, as well as several estates. Suyda

2162-542: Was restored in its old borders. In 2010, the administrative division of Leningrad Oblast was harmonized with the municipal division, and Gatchina was made the town of district significance. On August 1, 1927, Oredezhsky District , with the administrative center in the settlement of Oredezh , was established as well. It was a part of Luga Okrug of Leningrad Oblast and included parts of former Trotsky and Luzhsky Uyezds , as well as of Novgorodsky Uyezd of Novgorod Governorate . On October 22, 1959 Oredezhsky District

2209-694: Was the Gannibal family estate and is related with the biography of Alexander Pushkin , a poet and influential figure in the creation of the modern Russian language, whereas Bolshiye Taytsy belonged to the Demidov family. Myza Ivanovka belonged to the architect Andrei Stackenschneider , who was also born in the estate. The Gatchina ensembles were designated as a part of the World Heritage site Historic Centre of Saint Petersburg and Related Groups of Monuments . Palaces and parks of Gatchina operate as

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