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ZUIDER ZEE, or ZUYDER ZEE

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Originally appearing in Volume V28, Page 1049 of the 1911 Encyclopedia Britannica.
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ZUIDER ZEE, or ZUYDER ZEE  , a See also:

land-locked inlet on the See also:coast of See also:Holland, bounded N. by the See also:chain of the Frisian Islands, and W., S., and E. by the provinces of See also:North Holland, See also:Utrecht, See also:Gelderland, See also:Overysel, and See also:Friesland . It is about 85 m. See also:long N. to S., and from lo to 45 M. broad, with an See also:area of 2027 sq. m., and contains the islands of Marken, Schokland, Urk, Wieringen, and Griend . In the See also:early centuries of the See also:Christian era the Zuider (i.e . See also:Southern) Zee was a small inland See also:lake situated in the southern See also:part of the See also:present gulf, and called Flevo by See also:Tacitus, See also:Pliny, and other early writers . It was separated from the See also:sea by a See also:belt of See also:marsh and fen uniting Friesland and North Holland, the See also:original coast-See also:line being still indicated by the line of the Frisian Islands . Numerous streams, including the Vecht, Eem, and Ysel, discharged their See also:waters into this lake and issued thence as the Vlie (Latin Flevus), which reached the North Sea by the Vliegat between the islands of Vlieland and Terschelling . In the Lex Frisonum the Vlie (Fli, or Flehi) is accepted as the boundary between the territory of the See also:East and See also:West See also:Frisians. in See also:time, however, and especially during the 12th See also:century, high tides and north-west storms swept away the western See also:banks of the Vlie and submerged See also:great tracts of land . In 1170 the land between Stavoren, Texel, and See also:Medemblik was washed away, and a century later the Zuider Zee was formed . The open waterway between Stavoren and See also:Enkhuizen, however, as it now exists, See also:dates from 1400 . In the See also:south and east the destruction was arrested by the high sandy shores of Gooi, Veluwe, Voorst, and Gasterland in the provinces of Utrecht, Gelderland, Overysel, and Friesland respectively . The mean See also:depth of the Zuider Zee is 11.48 ft.; depth in the southern See also:basin of the former lake, 19 ft.; at Val See also:van Urk (deep See also:water to the west of the See also:island of Urk), 14; ft . If a line be See also:drawn from the island of Urk to Marken, and thence westwards to See also:Hoorn (North Holland) and N.N.E. to Lemmer (Friesland), these lines will connect parts of the Zuider Zee having a See also:uniform depth of 8 ft .

The other parts on the coast are only 3 ft. deep or less . This shallowness of its waters served to protect the Zuider Zee from the invasion of large See also:

ships of See also:war . It also explains how many once flourishing commercial towns, such as Stavoren, Medemblik, Enkhuizen, Hoorn, See also:Monnikendam, declined to the See also:rank of provincial trading and fishing ports . The See also:fisheries of the Zuider Zee are of considerable importance . Eighty per cent. of the bottom consists of sea See also:clay and .the more See also:recent silt of the Ysel ; 20 per cent. of See also:sand, partly in the north about Urk and Enkhuizen, partly in the south along the high shores of Gooi, Veluwe, &c . The shallowness of the sea and the See also:character of its bottom, promising fertile See also:soil, occasioned various projects of drainage . The See also:scheme recommended by the Zuider Zee Vereeniging (1886) formed the subject of a See also:report in 1894 by a See also:state See also:commission . The See also:principal feature in the scheme was the See also:building of a See also:dike from the island of Wieringen to the coast of Friesland . The area south of this would be divided into four polders, with See also:reservation, however, of a lake, Yselmeer, in the centre, whence branches would run to Ysel and the Zwolsche Diep, to See also:Amsterdam, and, by sluices near Wieringen, to the See also:northern part of the sea . The four polders with their areas of fertile soil would be: (I) North-west See also:polder, area 53,599 acres; fertile soil, 46,189 acres . (2) South-west ,, ,, 77,854 ,, " ,, 68,715 „ (3) South-east „ „ 266,167 „ „ 222,275 „ (4) North-east ,, 125,599 „ „ 120,783 „ The Lake Yselmeer would have an area of 56o sq. m . The gain would be the addition to the See also:kingdom of a new and fertile See also:province of the area of North See also:Brabant, a saving of expenses on dikes, diminution of inundations, improvement of communication between the south and the north of the kingdom, See also:protection of isles of the sea, &c .

The See also:

costs were calculated as follows: (1) enclosing dike, sluices, and regulation of Zwolsche Diep, £1,760,000; (2) reclamation of four polders, £5,200,000; (3) defensive See also:works, £400,000; (4) See also:indemnity to fishermen, £180,000; See also:total, £7,540,000 . In 1901 the See also:government introduced a See also:bill in the States See also:General, based on the recommendations of the commission, providing for enclosing the Zuider Zee by building a dike from the North Holland coast, through the Amsteldiep to Wieringen and from that island to the Friesland coast at Piaam; and further providing for the draining of two portions of the enclosed area, namely the N.W. and the S.W. polders shown in the table . The entire See also:work was to be completed in 18 years at an estimated cost of £7,916,000 . The bill failed to become See also:law and in consequence of See also:financial difficulties the project had not, up to 1910, advanced beyond the See also:stage of See also:consideration . With the exception of Griend and Schokland, the islands of the Zuider Zee are inhabited by small fishing communities, who retain some archaic customs and a picturesque See also:dress . Urk is already mentioned as an island in 966 . The inhabitants of Schokland were compelled to leave the island by See also:order of the state in 1859, it being considered insecure from inundation . The island of Griend (or Grind) once boasted a walled See also:town, which was destroyed by See also:flood at the end of the 13th century . But the island continued for some centuries to serve as a pasturage for See also:cattle, giving its name to a well-known description of See also:cheese . Like some of the other islands, See also:sheep are still brought to graze upon it in summer, and a large number of birds' eggs are collected upon it in See also:spring . Several of the islands were once the See also:property of religious houses on the mainland . The See also:British See also:Foreign See also:Office report, Draining of the Zuiderzee (1901), gives full particulars of the Dutch government's scheme and a retrospect of all former proposals .

See also De economische beteekens van de afsluiting en drooglegging der Zuiderzee vom Zuiderzee-Verein (2nd ed., 1901), and D . Bellet, " Le dessechement du Zuiderzee,” Rev . Geog . (1902) and W . J . Tuyn, Oude I-Iollandsche Dorpen aan de Zuiderzee (See also:

Haarlem, 1900) .

End of Article: ZUIDER ZEE, or ZUYDER ZEE
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