Misplaced Pages

#880119

65-677: The Saalian succeeded the Holstein interglacial and was followed by the Eemian interglacial (which began around 130,000 years ago) Though the start date of the Saalian was historically controversial, recent scholarship has suggested that the start date of the Saalian (and thus the end of the Holstein) is around 400,000 years ago. The Saalian encompasses multiple glacial cycles separated by interglacial periods. The first cold phase (Fuhne glacial) at

130-603: 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

195-522: 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

260-630: A MIS 11 date, spanning approximately 421-395,000 years ago. The Holstein interglacial is defined by marine sedimentation. On the stratigraphic record at the natural monument of de:Sievertsche Tongrube in Hamburg -Hummelsbüttel, its development is traced from the Elster ice age (Lauenburg clay) through the start of the warm period (freshwater depositions) to its flooding by the Holstein Sea (Cardien Sands). Lower Saxony Lower Saxony

325-465: 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

390-507: 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)

455-656: 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

520-759: 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

585-944: The Mindel-Riss interglacial ( Mindel-Riß-Interglazial ) in the Alpine region, is the third to last major interglacial in Europe before the Holocene , the present warm period. It followed directly after the Elster glaciation and came before the Saale glaciation , during the Middle Pleistocene . The more precise timing was historically controversial since Holstein was commonly correlated to two different marine isotope stages , MIS 11 (424–374 thousand years ago ) and MIS 9 (337–300 thousand years ago ). Recent scholarship has supported

650-461: 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

715-688: 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

SECTION 10

#1732765932881

780-917: The Northwest German Plain , but older and exhibiting more surface weathering than the much later Young Drift areas of the Weichselian glaciation in northeast Germany. The areas last covered by the Saale cold period, roughly the Westphalian Bight , a large part of Lower Saxony and Saxony-Anhalt , south Brandenburg , or the Leipzig Bay and Lusatia in Saxony, are called the Old Drift Landscapes ( Altmoränenlandschaften ). They were further shaped and changed during

845-545: 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

910-428: 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

975-432: 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

1040-469: 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

1105-514: 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

1170-640: 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

1235-637: 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

1300-669: 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

1365-614: The Saale complex ( obere Teil des Saale-Komplexes ) is characterised in North Germany by three great glacial advances (possibly even four in Schleswig-Holstein). They are usually called the: There are no indisputable traces in northern Germany of clear thermomers ( interstadials , intervals) between these advances. In the work by Litt et al. (2007) focussed on the southern perimeter of the North German glaciations,

SECTION 20

#1732765932881

1430-544: 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

1495-535: 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

1560-731: 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,

1625-535: 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,

1690-598: 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

1755-597: 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

1820-480: The eastern edge of the Harz eastwards ( Poland , Brandenburg , Saxony and Saxony-Anhalt ) the ice advanced to about 10 to 50 km behind the maximum extent of the Elster glaciation. On the northern edge of the Harz the two ice sheets reached the same line; and west of the Harz the ice of the Saale complex extended over 100 km further south than the ice sheet of the Elster. In front of this line, i.e. in front of

1885-708: 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

1950-457: 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

2015-518: 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

Saale glaciation - Misplaced Pages Continue

2080-519: 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 ),

2145-404: 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

2210-674: The former glaciers, fluviatile and periglacial sediments are widespread. In the Drenthe Stage the present day North Sea basin, Great Britain and Ireland were also affected. Several species were hurt by the glaciation, including the woolly mammoths , which suffered a reduction comparable to the one towards the end of the ice age. The Saale complex may be divided into a lower (also Saale Early Glacial) and an upper section (also Middle and Upper Saale Glacial, or Younger Saale glaciation), with glacial advances into Northern Germany. The Saale Early Glacial includes the: The upper part of

2275-560: 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

2340-529: 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

2405-498: The later Weichselian cold period by periglacial processes such as wind-borne sand and loess . The major urstromtal associated with the Saale glacial stage is the Breslau-Magdeburg-Bremen Urstromtal , which was not subsequently covered by ice. Holstein interglacial The Holstein or Holsteinian interglacial ( German : Holstein-Warmzeit or Holstein-Interglazial ), also called

2470-545: 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,

2535-649: 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

2600-533: 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

2665-439: 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

Saale glaciation - Misplaced Pages Continue

2730-544: 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

2795-696: 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

2860-773: 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

2925-508: 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

2990-437: 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

3055-422: 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

3120-434: The same time as the Wolstonian Stage in the British Isles and the Illinoian Stage in North America . In 1910, the name for "Saale glaciation" was given by German geologists Jacob Stoller and Konrad Keilhack . The maximum advance of the ice sheet in North Germany during the Drenthe Stage is described by a line from Düsseldorf via Paderborn , Hamelin , Goslar , Eisleben , Zeitz and Meissen to Görlitz . From

3185-418: 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

3250-435: The start of the Saale complexes is separated by a warmer period (Dömnitz interglacial) from the actual Saale "ice age". The term "Saale Ice Age" or "Saale Glacial" thus has 2 meanings in the literature – it sometimes refers to the phase in which the glacier advanced into North Germany , but can also refer to the whole Saale complex. The terms are frequently interchanged in the literature. The Saale Glaciation occurred at around

3315-412: 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

SECTION 50

#1732765932881

3380-427: 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

3445-406: 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,

3510-425: 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

3575-451: The upper part of the Saale complex is subdivided as follows: The Drenthe Stage corresponds to the maximum extent of glaciation during the Saale complex. During the last stage, the Warthe Stage, glaciers only covered northeast Lower Saxony (parts of the Lüneburg Heath ), the Altmark , the Elbe valley downstream of Magdeburg and the region east of it (c.f. Südlicher Landrücken ), so that these areas are geomorphologically younger than

3640-437: 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

3705-427: 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

3770-418: 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

3835-456: 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

3900-416: 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

3965-411: 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

SECTION 60

#1732765932881

4030-419: 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

4095-408: 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

4160-416: 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

4225-408: 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 ,

#880119