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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 chain of the Frisian Islands, and W., S., and E. by the provinces of
See also: North Holland, See also: Utrecht, Gelderland, See also: Overysel, and See also: Friesland
.
It is about 85 m. 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 early centuries of the Christian era the Zuider (i.e
.
See also: Southern) Zee was a small inland lake situated in the southern See also: part of the See also: present gulf, and called Flevo by 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 West Frisians. in See also: time, however, and especially during the 12th 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 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 character of its bottom, promising fertile See also: soil, occasioned various projects of drainage
.
The scheme recommended by the Zuider Zee Vereeniging (1886) formed the subject of a report in 1894 by a See also: state commission
.
The See also: principal feature in the scheme was the See also: building of a dike from the island of Wieringen to the coast of Friesland
.
The area south of this would be divided into four polders, with 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 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) 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 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 stage of 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 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 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 spring
.
Several of the islands were once the See also: property of religious houses on the mainland
.
The See also: British See also: Foreign 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)
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