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73-560: Hann. Münden (short for Hannoversch Münden ) is a town in Lower Saxony , Germany. Münden lies in the district of Göttingen at the confluence of the Fulda and Werra rivers, which join to form the Weser . It has about 24,000 inhabitants (2013). It is famous for its half-timbered houses, some of them more than 600 years old. There are 10 million cobblestones around the town. The place

146-603: A Prussian province ; after 1919 Brunswick became a free state). Historically a close tie existed between the royal house of Hanover ( Electorate of Hanover ) and the United Kingdom of Great Britain and Ireland as a result of their personal union in the 18th century (the personal union was dissolved when Victoria became the Queen of the United Kingdom in 1837 because Hanover did not allow female rulers). West of

219-522: A Lower Saxon Constituency Association ( Wahlkreisverband IX (Niedersachsen) ). This indicates that at that time the western administrations of the Prussian Province of Hanover and the state of Oldenburg were perceived as being "Lower Saxon". The forerunners of today's state of Lower Saxony were lands that were geographically and, to some extent, institutionally interrelated from very early on. The County of Schaumburg (not to be confused with

292-453: A new building on the main campus in 1970. Many tourists visit the city to see some 700 of its well-preserved half-timbered medieval houses. The large Lutheran church of St Blasius (14th–15th centuries), in Gothic style, contains the sarcophagus of Duke Eric I of Brunswick-Calenberg (d. 1540). Other sights include: Hann. Münden is twinned with: Lower Saxony Lower Saxony

365-465: A number of areas to the east, for example, in what is now west and north Saxony-Anhalt. The land of the Saxons was divided into about 60  Gaue . The Frisians had not moved into this region; for centuries they preserved their independence in the most northwesterly region of the present-day Lower Saxon territory. The original language of the folk in the area of Old Saxony was West Low German , one of

438-604: A steam-pump-powered paddlewheel boat, probably pedal-driven in 1704, and as a demonstration used it to navigate down the Fulda River from Kassel to Münden in 1707. Hann. Münden was the site of the Royal Prussian Academy of Forestry : the city's botanical gardens with many different trees were primarily established for this academy. Later the academy was merged into the University of Göttingen , moving to

511-507: Is a German state ( Land ) in northwestern Germany . It is the second-largest state by land area, with 47,614 km (18,384 sq mi), and fourth-largest in population (8 million in 2021) among the 16 Länder of the Federal Republic of Germany . In rural areas, Northern Low Saxon and Saterland Frisian are still spoken, though by declining numbers of people. Lower Saxony borders on (from north and clockwise)

584-656: Is a depression near Freepsum in East Frisia. The state's economy, population, and infrastructure are centred on the cities and towns of Hanover, Stadthagen, Celle, Braunschweig, Wolfsburg , Hildesheim, and Salzgitter. Together with Göttingen in southern Lower Saxony, they form the core of the Hannover–Braunschweig–Göttingen–Wolfsburg Metropolitan Region . Lower Saxony has clear regional divisions that manifest themselves geographically, as well as historically and culturally. In

657-827: Is drained by rivers that flow northwards into the North Sea or the Baltic and tributaries to the Rhine river that flows West. The Rhine, Ems , Weser , Elbe and Havel are the most important rivers which drain the North German Lowlands into the North Sea and created woods in their flood plains and folds, e.g. the Spreewald ("Spree Forest"). Only a small area of the North German Plain falls within

730-420: Is first mentioned in the deeds of donation of Gimundi to the abbey of Fulda , in 802. The town's name means "confluence" in old German; the prefix Hannoversch , or " Hanoverian ", was added in the 19th century to help distinguish the town from its similarly-named Prussian neighbour, Minden . City rights might have been granted during the latter half of the 12th century. The French inventor Denis Papin built

803-497: The Altes Land near Hamburg , which is characterised by relatively mild temperatures year round due to the proximity of the North Sea and lower Elbe river, providing excellent conditions for fruit production. Azonal vegetation complexes of moors, riparian forests, fens and water bodies originally stretched along the rivers Ems , Weser , Elbe , Havel and Spree . Distinctive salt marshes , tideflats and tidal reed beds in

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876-759: The British Zone of Occupation . On 23 August 1946, the British Military Government issued Ordinance No. 46 "Concerning the dissolution of the provinces of the former state of Prussia in the British Zone and their reconstitution as independent states" , which initially established the State of Hanover on the territory of the former Prussian Province of Hanover. Its minister president, Hinrich Wilhelm Kopf , had already suggested in June 1945

949-461: The Nazi Party seized power in 1933, they quickly transformed Germany into a highly centralized state and divided the entire Third Reich into Gaue which largely superseded (but did not outright replace) Germany's traditional federal system. Nevertheless, some changes to the old state and provincial borders were made in 1937, notably including the city of Cuxhaven being fully integrated into

1022-632: The North Sea , the states of Schleswig-Holstein , Hamburg , Mecklenburg-Vorpommern , Brandenburg , Saxony-Anhalt , Thuringia , Hesse and North Rhine-Westphalia , and the Netherlands . Furthermore, the state of Bremen forms two enclaves within Lower Saxony, one being the city of Bremen , the other its seaport , Bremerhaven (which is a semi-exclave , as it has a coastline). Lower Saxony thus borders more neighbours than any other single Bundesland . The state's largest cities are

1095-977: The Weser Hills and the Lower Saxon Börde, which partly separate it from that area of the Plain known as the Westphalian Lowland . Elements of the Rhenish Massif also act a part of the southern boundary of the plain: the Eifel , Bergisches Land and the Sauerland . In the east the North German Plain spreads out beyond the Harz Mountains and Kyffhäuser further to the south as far as the Central Saxon hill country and

1168-545: The district of Tecklenburg and the state of Lippe . Kopf's plan was ultimately based on a draft for the reform of the German Empire from the late 1920s by Georg Schnath and Kurt Brüning. The strong Welf connotations of this draft, according to Thomas Vogtherr, did not simplify the development of a Lower Saxon identity after 1946. An alternative model, proposed by politicians in Oldenburg and Brunswick, envisaged

1241-531: The estuaries existed permanently in the tidal zone of the North Sea coast. The natural vegetation of the North German Plain is thought to have been forest formed mainly by the dominant species European Beech (Fagetalia). According to Germany's Federal Agency for Nature Conservation, the BfN , the North German Plain consists of the natural regions listed below. Where possible, their names have been derived from authoritative English-language source(s), as indicated by

1314-428: The north temperate zone of central Europe that is affected by prevailing Westerlies and is located in a transition zone between the maritime climate of Western Europe and the continental climate of Eastern Europe . This transition is clearly noticeable within the state: whilst the northwest experiences an Atlantic (North Sea coastal) to Sub-Atlantic climate, with comparatively low variations in temperature during

1387-432: The "Constituency Association of Lower Saxony" in 1920. In a lecture on 14 September 2007, Dietmar von Reeken described the emergence of a "Lower Saxony consciousness" in the 19th century, the geographical basis of which was used to invent a territorial construct: the resulting local heritage societies ( Heimatvereine ) and their associated magazines routinely used the terms "Lower Saxony" or "Lower Saxon" in their names. At

1460-469: The 1930s, a real Lower Saxony did not yet exist, but there were a plethora of institutions that would have called themselves "Lower Saxon". The motives and arguments in the disputes between "Lower Saxony" and "Westphalia" were very similar on both sides: economic interests, political aims, cultural interests and historical aspects. After the Second World War most of Northwest Germany lay within

1533-570: The Börde areas (Hildesheim Börde, Magdeburg Börde, with their fertile, loess soils). High-level bog peat can be found in the poorest soils, e.g. in the Teufelsmoor . In the loess areas of the lowland are found the oldest settlement locations in Germany ( Linear Pottery culture ). The northeastern part of the plain (Young Drift) is geomorphologically distinct and contains a multitude of lakes (e.g.

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1606-514: The Elbe downstream Hamburg are known as the Altes Land (Old Country). Due to its gentle local climate and fertile soil, it is the state's largest area of fruit farming, its chief produce being apples . Most of the state's territory was part of the historic Kingdom of Hanover , and the state of Lower Saxony has adopted the coat of arms and other symbols of the former kingdom. It was created by

1679-544: The Fulda Gap option was seen as the most likely invasion route because of easier and closer access to tactical and strategic goals important for an invasion of Western Europe. Of the two North German plain invasion options, the southern route of the attack, which had the better strategic opportunities, would have been led by the Soviet Third Shock Army . The plain's geography, which makes it suitable for

1752-650: The Mueritz lake in the Mecklenburg Lake Plateau ) which are vestiges of the last ice age. The retreating glaciers left this landscape behind around 16,000 to 13,000 years ago. In comparison, the dry plains of northwestern Germany (Lower Saxony, western Schleswig-Holstein, and the Bochum area of North Rhine Westphalia) are more heavily weathered and levelled ( Old Drift ) as the last large scale glaciations here occurred at least 130,000 years ago. The region

1825-640: The Principality of Schaumburg-Lippe) around the towns of Rinteln and Hessisch Oldendorf did indeed belong to the Prussian province of Hesse-Nassau until 1932, a province that also included large parts of the present state of Hesse, including the cities of Kassel , Wiesbaden and Frankfurt am Main ; but in 1932 the County of Schaumburg became part of the Prussian Province of Hanover. When

1898-637: The Prussian Province of Hanover under the Greater Hamburg Act . The effect of this Nazi-era change was that in 1946, after the Third Reich had collapsed and when state of Lower Saxony was founded, only four states needed to be merged. With the exception of Bremen and the areas that were ceded to the Soviet Occupation Zone in 1945, all those areas allocated to the new state of Lower Saxony in 1946, had already been merged into

1971-669: The River Hunte a "de-Westphalianising process" began in 1815. After the Congress of Vienna the territories of the later administrative regions ( Regierungsbezirke ) of Osnabrück and Aurich transferred to the Kingdom of Hanover. The Grand Duchy of Oldenburg and the Principality of Schaumburg-Lippe retained state autonomy. Nevertheless, the entire Weser-Ems region (including the city of Bremen ) were grouped in 1920 into

2044-599: The Saxon peoples left their homeland in Holstein about the 3rd century and pushed southwards over the Elbe , where they expanded into the sparsely populated regions in the rest of the lowlands, in present-day Northwest Germany and the northeastern part of what is now the Netherlands . From about the 7th century the Saxons had occupied a settlement area that roughly corresponds to the present state of Lower Saxony, of Westphalia and

2117-535: The Weser-Ems region was placed under the rule of Brunswick-Lüneburg. The word Niedersachsen was first used before 1300 in a Dutch rhyming chronicle ( Reimchronik ). From the 14th century it referred to the Duchy of Saxe-Lauenburg (as opposed to Saxe-Wittenberg ). On the creation of the imperial circles in 1500, a Lower Saxon Circle was distinguished from a Lower Rhenish–Westphalian Circle . The latter included

2190-731: The area of Helmstedt. The highest levels of precipitation are experienced in the Harz because the Lower Saxon part forms the windward side of this mountain range against which orographic rain falls. The average annual temperature is 8 °C (46 °F); 7.5 °C (45.5 °F) in the Altes Land and 8.5 °C (47.3 °F) in the district of Cloppenburg . Lower Saxony is divided into 37 districts ( Landkreise or simply Kreise ): Furthermore, there are eight urban districts and two cities with special status: Between 1946 and 2004,

2263-568: The catchment area of the Oder and Neiße rivers which drain into the Baltic. The North Sea coast and the adjacent coastal areas of the facing East and North Frisian Islands are characterised by a maritime climate . South of the coast, a broad band of maritime and sub-maritime climate stretches from the east coast of Schleswig-Holstein to the western edges of the Central Uplands . To

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2336-535: The coast East Frisia . The state is dominated by several large northwards-flowing rivers, including the Ems , Weser , Aller , and the Elbe. The highest point in Lower Saxony is the Wurmberg (971 metres or 3,186 feet) in the Harz. Most of the significant hills and mountains are found in the southeastern part of the state. The lowest point in the state, at about 2.5 metres or 8 feet 2 inches below sea level,

2409-598: The course of the year and a surplus water budget, the climate towards the southeast is increasingly affected by the Continent. This is clearly shown by greater temperature variations between the summer and winter halves of the year and in lower and more variable amounts of precipitation across the year. This sub-continental effect is most sharply seen in the Wendland, in the Weser Uplands (Hamelin to Göttingen) and in

2482-597: The division of the British occupation zone into three large states proved to be capable of gaining a majority. Because this division of their occupation zone into relatively large states also met the interests of the British, on 8 November 1946 Regulation No. 55 of the British military government was issued, by which the State of Lower Saxony with its capital Hanover were founded, backdated to 1 November 1946. The state

2555-639: The enclave area. To the southeast, the state border runs through the Harz, low mountains that are part of the German Central Uplands . The northeast and west of the state, which form roughly three-quarters of its land area, belong to the North German Plain, while the south is in the Lower Saxon Hills , including the Weser Uplands , Leine Uplands , Schaumburg Land , Brunswick Land , Untereichsfeld , Elm , and Lappwald . In

2628-653: The end of 2023, there were almost 1,085,315 non-German citizens in Lower Saxony. The following table illustrates the largest minority groups in Lower Saxony: Religion in Lower Saxony (Census 2011): North German Plain In the west, the southern boundary of the North German Plain is formed by the Lower Saxon Hills : specifically the ridge of the Teutoburg Forest , the Wiehen Hills ,

2701-457: The end of the 1920s in the context of discussions about a reform of the Reich, and promoted by the expanding local heritage movement ( Heimatbewegung ), a 25-year conflict started between "Lower Saxony" and "Westphalia". The supporters of this dispute were administrative officials and politicians, but regionally focussed scientists of various disciplines were supposed to have fuelled the arguments. In

2774-518: The following territories that, in whole or in part, belong today to the state of Lower Saxony: the Bishopric of Osnabrück , the Bishopric of Münster , the County of Bentheim , the County of Hoya , the Principality of East Frisia , the Principality of Verden , the County of Diepholz , the County of Oldenburg , the County of Schaumburg and the County of Spiegelberg . At the same time a distinction

2847-570: The foothills of the Ore Mountains . It is known that the North German Plain was formed during the Pleistocene era as a result of the various glacial advances of terrestrial Scandinavian ice sheets as well as by periglacial geomorphologic processes. The terrain may be considered as part of the Old or Young Drift ( Alt- or Jungmoräne ), depending on whether or not it was formed by

2920-519: The formation of a state of Lower Saxony, that was to include the largest possible region in the middle of the British Zone. In addition to the regions that actually became Lower Saxony subsequently, Kopf asked, in a memorandum dated April 1946, for the inclusion of the former Prussian district of Minden-Ravensberg (i.e. the Westphalian city of Bielefeld as well as the Westphalian districts of Minden , Lübbecke , Bielefeld , Herford and Halle ),

2993-404: The former Hanoverian president ( Regierungspräsident ) as their first minister-president. Kopf led a five-party coalition, whose basic task was to rebuild a state afflicted by the war's rigours. Kopf's cabinet had to organise an improvement of food supplies and the reconstruction of the cities and towns destroyed by Allied air raids during the war years. Hinrich Wilhelm Kopf remained – interrupted by

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3066-560: The foundation of the independent state of "Weser-Ems", that would be formed from the state of Oldenburg, the Hanseatic City of Bremen and the administrative regions of Aurich and Osnabrück. Several representatives of the state of Oldenburg even demanded the inclusion of the Hanoverian districts of Diepholz , Syke , Osterholz-Scharmbeck and Wesermünde in the proposed state of "Weser-Ems". Likewise an enlarged State of Brunswick

3139-422: The four administrative regions or governorates ( Regierungsbezirke ), into which Lower Saxony had been hitherto divided, were dissolved. These were the governorates of Braunschweig, Hanover, Lüneburg and Weser-Ems. The largest towns in Lower Saxony as of 31 December 2017: The name of Saxony derives from that of the Germanic confederation of tribes called the Saxons . Before the late medieval period, there

3212-630: The ice age which formed them) – e.g., on the Fläming Heath (200 m (660 ft) above sea level) and the Helpt Hills 179 m (587 ft)). Following the ice ages, rain-fed, raised bogs originated in western and northern Lower Saxony during warm periods of high precipitation (as influenced by Medieval Warm Period). These bogs were formerly widespread but much of this terrain has now been drained or otherwise superseded. The coastal areas consist of Holocene lake and river marshes and lagoons connected to Pleistocene Old and Young Drift terrain in various stages of formation and weathering. After or during

3285-501: The ice sheets of the last glacial period, the Weichselian Ice Age . The surface relief varies from level to undulating. The lowest points are low moorlands and old marshland on the edge of the ridge of dry land in the west of Schleswig-Holstein (the Wilster Marsh is 3.5 m (11 ft) below sea level) and in the northwest of Lower Saxony (Freepsum, 2.3 m (7.5 ft) below sea level). The highest points may be referred to as Vistula and Hall glaciation terminal moraines (depending on

3358-488: The main transport artery to West Berlin and, from 1945 to 1990 was the busiest European border crossing point. Of economic significance for the state was the Volkswagen concern, that restarted the production of civilian vehicles in 1945, initially under British management, and in 1949 transferred into the ownership of the newly founded country of West Germany and state of Lower Saxony. Overall, Lower Saxony, with its large tracts of rural countryside and few urban centres,

3431-427: The medieval, Welf estates of the Duchy of Brunswick-Lüneburg . All the Welf princes called themselves dukes "of Brunswick and Lüneburg" despite often ruling parts of a duchy that was forever being divided and reunited as various Welf lines multiplied or died out. Two major principalities survived east of the Weser after the Napoleonic Wars: the Kingdom of Hanover and the Duchy of Brunswick (after 1866 Hanover became

3504-418: The merger of the State of Hanover with three smaller states on 1 November 1946. Lower Saxony has a natural boundary in the north in the North Sea and the lower and middle reaches of the River Elbe , although parts of the city of Hamburg lie south of the Elbe. The state and city of Bremen is an enclave entirely surrounded by Lower Saxony. The Bremen/Oldenburg Metropolitan Region is a cooperative body for

3577-439: The new Lower Saxon constitution entered force, replacing the "Provisional Lower Saxon Constitution" of 1951. It enables referendums and plebiscites and establishes environmental protection as a fundamental state principle. The former Hanoverian Amt Neuhaus with its parishes of Dellien, Haar, Kaarßen, Neuhaus (Elbe), Stapel, Sückau, Sumte and Tripkau as well as the villages of Neu Bleckede, Neu Wendischthun and Stiepelse in

3650-480: The northeast of Lower Saxony is the Lüneburg Heath. The heath is dominated by the poor, sandy soils of the geest , whilst in the central-east and southeast in the loess börde zone , productive soils with high natural fertility occur. Under these conditions—with loam and sand -containing soils—the land is well-developed agriculturally . In the west lie the County of Bentheim , Osnabrück Land , Emsland , Oldenburg Land , Ammerland , Oldenburg Münsterland , and on

3723-439: The northern and eastern border of North Rhine-Westphalia has largely been identical with that of the Prussian Province of Westphalia . Only the Free State of Lippe was not incorporated into North Rhine-Westphalia until January 1947. With that the majority of the regions left of the Upper Weser became North Rhine-Westphalian. In the end, at the meeting of the Zone Advisory Board on 20 September 1946, Kopf's proposal with regard to

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3796-523: The northern parts of the Central Uplands : the Weser Uplands and the Harz Mountains. Between these two lie the Lower Saxon Hills , a range of low ridges. The region in the northeast, the Lüneburg Heath ( Lüneburger Heide ), is the largest heathland area of Germany. In the Middle Ages, the town of Lüneburg was wealthy due to salt-mining and the salt trade. To the north the Elbe valley separates Lower Saxony from Hamburg, Schleswig-Holstein, Mecklenburg-Vorpommern , and Brandenburg. The left banks of

3869-508: The parish of Teldau and the historic Hanoverian region in the forest district of Bohldamm in the parish of Garlitz transferred with effect from 30 June 1993 from Mecklenburg-Vorpommern to Lower Saxony ( Lüneburg district ). From these parishes the new municipality of Amt Neuhaus was created on 1 October 1993. In 1998 Gerhard Glogowski succeeded Gerhard Schröder who became Federal Chancellor. Because he had been linked with various scandals in his home city of Brunswick, he resigned in 1999 and

3942-421: The references. During the Cold War , in the event of war between NATO and the Warsaw Pact , NATO military strategists identified the North German plain as an area that could have been used for two of three major invasion routes into Western Europe by Warsaw Pact forces. The third route was the Fulda Gap further south. The North German plain routes were the best attack options for an attacking army. However,

4015-437: The regions listed here are part of other, larger regions, that are also included in the list. Just under 20% of the land area of Lower Saxony is designated as nature parks, i.e.: Dümmer , Elbhöhen-Wendland , Elm-Lappwald , Harz , Lüneburger Heide , Münden , Terra.vita , Solling-Vogler , Lake Steinhude , Südheide , Weser Uplands , Wildeshausen Geest , Bourtanger Moor-Bargerveen . Lower Saxony falls climatically into

4088-422: The regions that used to be independent, especially the heartlands of the former states of Brunswick , Hanover , Oldenburg and Schaumburg-Lippe , a marked local regional awareness exists. By contrast, the areas surrounding the Hanseatic cities of Bremen and Hamburg are much more oriented towards those centres. Sometimes, overlaps and transition areas happen between the various regions of Lower Saxony. Several of

4161-431: The retreat of the glaciers, wind-borne sand often formed dunes, which were later fixed by vegetation. Human intervention caused the emergence of open heath such as the Lüneburg Heath , and measures such as deforestation and the so-called Plaggenhieb (removal of the topsoil for use as fertilizer elsewhere) caused a wide impoverishment of the soil ( Podsol ). The most fertile soils are the young marshes ( Auen-Vegen ) and

4234-418: The seven East Frisian Islands offshore are popular with tourists. In the extreme west of Lower Saxony is the Emsland , an economically emerging but rather sparsely populated area, once dominated by inaccessible swamps. The northern half of Lower Saxony, also known as the North German Plain , is almost invariably flat except for the gentle hills around the Bremen geestland . Towards the south and southwest lie

4307-451: The south east and east, the climate becomes increasingly subcontinental: characterised by temperature differences between summer and winter which progressively increase away from the tempering effect of the ocean. Locally, a drier continental climate can be found in the rain shadow of the Harz and some smaller areas of upland like the Drawehn and the Fläming . Special microclimates occur in bogs and heathlands and, for example, in

4380-412: The state capital Hanover , Braunschweig (Brunswick), Oldenburg , Osnabrück , Wolfsburg , Göttingen , Salzgitter , Hildesheim , mainly situated in its central and southern parts, except Oldenburg and Lüneburg. Lower Saxony is the only Bundesland that encompasses both maritime and mountainous areas. The northwestern area of the state, on the coast of the North Sea, is called East Frisia and

4453-427: The state's districts and independent towns were grouped into eight regions, with a different status for two regions ( Verwaltungsbezirke ), comprising the formerly free states of Brunswick and Oldenburg. In 1978 these regions were merged into four governorates ( Regierungsbezirke ). In 2005 the Bezirksregierungen (regional governments) were again split into separate bodies. 1946–1978: 1978–2004: On 1 January 2005

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4526-406: The successor to Hinrich Wilhelm Kopf. He was replaced in 1970 by Alfred Kubel . The arguments about the Gorleben Nuclear Waste Repository , that began during the time in office of minister president Ernst Albrecht (1976–1990), have played an important role in state and federal politics since the end of the 1970s. In 1990 Gerhard Schröder entered the office of minister-president. On 1 June 1993,

4599-425: The time in office of Heinrich Hellwege (1955–1959) – as the head of government in Lower Saxony until 1961. The greatest problem facing the first state government in the immediate post-war years was the challenge of integrating hundreds of thousands of refugees from Germany's former territories in the east (such as Silesia and East Prussia ), which had been annexed by Poland and the Soviet Union . Lower Saxony

4672-437: The varieties of language in the Low German dialect group. The establishment of permanent boundaries between what later became Lower Saxony and Westphalia began in the 12th century. In 1260, in a treaty between the Archbishopric of Cologne and the Duchy of Brunswick-Lüneburg the lands claimed by the two territories were separated from each other. The border ran along the Weser to a point north of Nienburg. The northern part of

4745-427: Was a single Duchy of Saxony . The term "Lower Saxony" was used after the dissolution of the stem duchy in the late 13th century to distinguish the parts of the former duchy ruled by the House of Welf from the Electorate of Saxony on one hand, and from the Duchy of Westphalia on the other. The name and coat of arms of the present state go back to the Germanic tribe of Saxons . During the Migration Period some of

4818-418: Was at the western end of the direct escape route from East Prussia and had the longest border with the Soviet Zone. On 3 October 1950 Lower Saxony took over the sponsorship of the very large number of refugees from Silesia . In 1950 there was still a shortage of 730,000 homes according to official figures. During the period when Germany was divided, the Lower Saxon border crossing at Helmstedt found itself on

4891-456: Was formed by a merger of the Free States of Brunswick , of Oldenburg and of Schaumburg-Lippe with the previously formed State of Hanover. But there were exceptions: The demands of Dutch politicians that the Netherlands should be given the German regions east of the Dutch-German border as war reparations , were roundly rejected at the London Conference of 26 March 1949. In fact only about 1.3 km (0.50 sq mi) of west Lower Saxony

4964-416: Was made with the eastern part of the old Saxon lands from the central German principalities later called Upper Saxony for dynastic reasons. The close historical links between the domains of the Lower Saxon Circle now in modern Lower Saxony survived for centuries especially from a dynastic point of view. The majority of historic territories whose land now lies within Lower Saxony were sub-principalities of

5037-411: Was one of the industrially weaker regions of the federal republic for a long time. In 1960, 20% of the working population worked on the land. In the rest of the federal territory the figure was just 14%. Even in economically prosperous times the jobless totals in Lower Saxony are constantly higher than the federal average. In 1961 Georg Diederichs took office as the minister president of Lower Saxony as

5110-419: Was proposed in the southeast to include the Regierungsbezirk of Hildesheim and the district of Gifhorn . Had this plan come to fruition, the territory of the present Lower Saxony would have consisted of three states of roughly equal size. The district council of Vechta protested on 12 June 1946 against being incorporated into the metropolitan area of Hanover ( Großraum Hannover ). If the State of Oldenburg

5183-408: Was replaced by Sigmar Gabriel . From 2003 to his election as Federal President in 2010 Christian Wulff was minister president in Lower Saxony. The Osnabrücker headed a CDU-led coalition with the FDP as does his successor, David McAllister . After the elections on 20 January 2013 McAllister was deselected . At the end of 2014, there were almost 571,000 non-German citizens in Lower Saxony. At

5256-541: Was to be dissolved, Vechta District would much rather be included in the Westphalian region. Particularly in the districts where there was a political Catholicism the notion was widespread, that Oldenburg Münsterland and the Regierungsbezirk of Osnabrück should be part of a newly formed State of Westphalia. Since the foundation of the states of North Rhine-Westphalia and Hanover on 23 August 1946

5329-621: Was transferred to the Netherlands, in 1949. → see main article Dutch annexation of German territory after World War II The first Lower Saxon parliament or Landtag met on 9 December 1946. It was not elected; rather it was established by the British Occupation Administration (a so-called "appointed parliament"). That same day the parliament elected the Social Democrat , Hinrich Wilhelm Kopf ,

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