Zuiderzee in the context of "Markermeer"

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⭐ Core Definition: Zuiderzee

The Zuiderzee or Zuider Zee (Dutch: [ˌzœydərˈzeː] ; old spelling Zuyderzee or Zuyder Zee), historically called Lake Almere and Lake Flevo, was a shallow bay of the North Sea in the northwest of the Netherlands. It extended about 100 km (62 mi) inland and at most 50 km (31 mi) wide, with an overall depth of about 4 to 5 m (13 to 16 ft) and a coastline of about 300 km (190 mi). It covered 5,000 km (1,900 sq mi). Its name is Dutch for "southern sea", indicating that the name originates in Friesland, to the north of the Zuiderzee (cf. North Sea).

It is generally acknowledged that the Zuiderzee existed from roughly 1170, following the devastating All Saints' Flood, until 1932, when the Afsluitdijk was completed. The majority of the Zuiderzee was closed off from the North Sea, leaving the mouth of the inlet to become part of the Wadden Sea. The salt water inlet changed into a fresh water lake now called the IJsselmeer (IJssel Lake) after the river that drains into it, and by means of drainage and polders, an area of some 1,500 km (580 sq mi) was reclaimed as land. This land eventually became the province of Flevoland. Part of the IJsselmeer was also divided into the Markermeer.

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👉 Zuiderzee in the context of Markermeer

The Markermeer (Dutch pronunciation: [ˌmɑrkərˈmeːr]) is a 700 km (270 sq mi) lake in the central Netherlands in between North Holland, Flevoland, and its smaller and larger neighbors, the IJmeer and IJsselmeer. A shallow lake at 3 to 5 m in depth, matching the reclaimed land to its west, north-west and east it is named after the small former island, now peninsula, of Marken on its west shore.

The Markermeer was not originally intended to remain a lake. It was formerly part of the Zuiderzee, a saltwater inlet of the North Sea, that was dammed off by the Afsluitdijk (Closure Dike) in 1932, turning the Zuiderzee into the freshwater IJsselmeer. The following years saw the reclamation of extensive tracts of land as large polders in an enormous project known as the Zuiderzee Works. One of these, the Markerwaard, was to occupy the area of the current Markermeer. Part of the construction of this polder was building the Houtribdijk, also called Markerwaarddijk, finished in 1976, which hydrologically splits the IJsselmeer in two, the southern section being the Markermeer.

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Zuiderzee in the context of Funnelbeaker culture

The Funnel(-neck-)beaker culture, in short TRB or TBK (German: Trichter(-rand-)becherkultur, Dutch: Trechterbekercultuur; Danish: Tragtbægerkultur; c. 4300–2800 BCE), was an archaeological culture in north-central Europe. It developed as a technological merger of local neolithic and mesolithic techno-complexes between the lower Elbe and middle Vistula rivers. These predecessors were the (Danubian) Lengyel-influenced Stroke-ornamented ware culture (STK) groups/Late Lengyel and Baden-Boleráz in the southeast, Rössen groups in the southwest and the Ertebølle-Ellerbek groups in the north. The TRB introduced farming and husbandry as major food sources to the pottery-using hunter-gatherers north of this line.

The TRB techno-complex is divided into a northern group including Northern Germany and southern Scandinavia (TRB-N, roughly the area that previously belonged to the Ertebølle-Ellerbek complex), a western group in the Netherlands between the Zuiderzee and lower Elbe that originated in the Swifterbant culture, an eastern group centered on the Vistula catchment, roughly ranging from Oder to Bug, and south-central groups (TRB-MES, Altmark) around the middle and upper Elbe and Saale. Especially in the southern and eastern groups, local sequences of variants emerged. In the late 4th millennium BCE, the Globular Amphora culture (GAC) replaced most of the eastern and subsequently also the southern TRB groups, reducing the TRB area to modern northern Germany and southern Scandinavia.

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Zuiderzee in the context of Flevoland

Flevoland (Dutch pronunciation: [ˈfleːvoːlɑnt] ) is the twelfth and newest province of the Netherlands, established in 1986, when the southern and eastern Flevopolders, together with the Noordoostpolder, were merged into one provincial entity. It is in the centre of the country in the former Zuiderzee, which was turned into the freshwater IJsselmeer by the closure of the Afsluitdijk in 1932. Almost all of the land belonging to Flevoland was reclaimed in the 1950s and 1960s while splitting the Markermeer and bordering lakes from the IJsselmeer. As to dry land, it is the smallest province of the Netherlands at 1,410 km (540 sq mi), but not gross land as that includes much of the waters of the fresh water lakes (meres) mentioned.

The province had a population of about 445,000 as of January 2023 and consists of six municipalities. Its capital is Lelystad and its most populous city is Almere, which forms part of the Randstad and has grown to become the seventh largest city of the country. Flevoland is bordered in the extreme north by Friesland, in the northeast by Overijssel, and in the northwest by the lakes Markermeer and IJsselmeer. In the southeast, the province borders on Gelderland; in the southwest on Utrecht and North Holland. Outside urban areas, the land in Flevoland is predominantly used for agriculture.

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Zuiderzee in the context of Cornelis Lely

Cornelis Lely (Dutch pronunciation: [kɔrˈneːlɪs ˈleːli]; 23 September 1854 – 22 January 1929) was a Dutch politician of the Liberal Union and civil engineer who was Minister of Water Management and Governor of Suriname. The designer of Afsluitdijk, the largest dam and causeway at its time of construction, in 1932, he oversaw the Zuiderzee Works as Minister, turning the Zuiderzee into a lake and making possible the conversion of a vast area of former seabed into dry land. His plan deeply transposed and influenced the current geography of the Netherlands. Lelystad, the capital of the province of Flevoland, is named after him.

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Zuiderzee in the context of Terp

A terp, also known as a wierde, woerd, warf, warft, werf, werve, wurt or værft, is an artificial dwelling mound found on the North European Plain that has been created to provide safe ground during storm surges, high tides and sea or river flooding. The various terms used reflect the regional dialects of the North European region.

Terps are found in the coastal regions of the Netherlands, particularly in the provinces of Zeeland, Friesland and Groningen, as well as in southern Denmark and northwestern Germany. Before the construction of dykes, these mounds provided protection against floodwaters that regularly disrupted daily life. They are especially common in East Frisia (Ostfriesland) and Nordfriesland in Germany. On the Halligen islands in Kries Norfriesland, people continue to live on terps without the protection of dykes. Terps are also present in the Rhine and Meuse river plains in central Netherlands. Further examples occur in North Holland, such as Avendorp near Schagen, and in the towns of Bredene and Leffinge near Oostende in Belgium. Additional terps are located at mouth of the IJssel River, including at Kampereiland in the province of Overijssel, as well as on the former island of Schokland in the Zuiderzee, now part of the reclaimed Noordoostpolder. An old terp, known as Het Torp is also located beneath the town of Den Helder in North Holland.

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Zuiderzee in the context of Doornspijk

Doornspijk is a village in the Dutch province of Gelderland. It is located in the municipality of Elburg.

The village was first mentioned in 796 as Thornspiiic, and is a combination of thorn and tapering land. The original village was flooded by the former Zuiderzee in 1825, and current village formed around the church after 1829.

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Zuiderzee in the context of Chauci

The Chauci were an ancient Germanic tribe living in the low-lying region between the Rivers Ems and Elbe, on both sides of the Weser and ranging as far inland as the upper Weser. Along the coast they lived on artificial mounds called terpen, built high enough to remain dry during the highest tide. A dense population of Chauci lived further inland, and they are presumed to have lived in a manner similar to the lives of the other Germanic peoples of the region.

Their ultimate origins are not well understood. In the Germanic pre-Migration Period (i.e., before c. 300 AD) the Chauci and the related Frisians, Saxons, and Angles inhabited the Continental European coast from the Zuyder Zee to south Jutland. All of these peoples shared a common material culture, and so cannot be defined archaeologically. The Chauci originally centered on the Weser and Elbe, but in c. AD 58 they expanded to the River Ems by expelling the neighboring Ampsivarii, whereby they gained a border with the Frisians to the west. The Romans referred to the Chauci living between the Weser and Elbe as the 'Greater Chauci' and those living between the Ems and Weser as the 'Lesser Chauci'.

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Zuiderzee in the context of Zuiderzee Works

The Zuiderzee Works (Dutch: Zuiderzeewerken) is a system of dams and dikes, land reclamation and water drainage work, which was the largest hydraulic engineering project undertaken by the Netherlands during the twentieth century. The project involved the damming of the Zuiderzee, a large, shallow inlet of the North Sea, and the reclamation of land in the newly enclosed water using polders. Its main purposes are to improve flood protection and create additional land for agriculture.

The enormous scale of the works required the creation of a joint venture company comprising several large dredging contractors, known as the Maatschappij tot Uitvoering van Zuiderzeewerken. The American Society of Civil Engineers declared the works, together with the Delta Works in the South-West of the Netherlands, as among the Seven Wonders of the Modern World.

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Zuiderzee in the context of IJssel

The IJssel (Dutch: [ˈɛisəl] ; Dutch Low Saxon: Iessel(t) [ˈisəl(t)]) is a Dutch distributary of the river Rhine that flows northward and ultimately discharges into the IJsselmeer (before the 1932 completion of the Afsluitdijk known as the Zuiderzee), a North Sea natural harbour. It more immediately flows into the east-south channel around the Flevopolder, Flevoland which is kept at 3 metres below sea level. This body of water is then pumped up into the IJsselmeer.

It is sometimes called the Gelderse IJssel (IPA: [ˌɣɛldərsə ˈʔɛisəl] ; "Gueldern IJssel") to distinguish it from the Hollandse IJssel. It is in the provinces of Gelderland and Overijssel, the latter of which was named after this river. The Romans knew the river as Isala. It flows from Westervoort, on the east side of the city of Arnhem.

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