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recognizable by the paved sections of the dike between the asphalted road sections after the dike reinforcements. Waiting for all the water to be drained through the de-inundation lock would take too long. Sheet pile walls have been installed in the dike to prevent the holes from wearing too far. They are covered with concrete beams, visible on the outside of the dike.
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flowing water that rapidly washes away the ground on the inside of the dike to great depths. Depths of 20 meters are not uncommon. Even after almost three centuries, the Wheels still bear witness to the calamity of drowned people and animals and the loss of homes and possessions, with all its consequences. The dike residents were generally not very wealthy.
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The overflow areas have been preserved and were even adapted to the new standards with the dike reinforcements of 1996. The level difference with Tiel is approximately 7.20 meters. In 1995, after the near-flood disaster, a water board official deemed it irresponsible to build large-scale houses here.
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A separate book could be written about the phenomenon of dike breaches in the entire
Tielerwaard region. For Dalem, the consequences of the dike breaches in 1726, 1728, and 1729 are still visible, and the wheels formed at that time are integral parts of the landscape. A wheel is formed by the inward
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The history of the Dalem lock dates back to 1284 when the Lords of the Vijf
Heerenlanden decided to build a dike ring around their area (the Diefdijk) and also to have the option to drain the excess water through an outlet lock at Dalem. As was customary at the time, this lock would be entirely made
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r (dutch: Maas Rivier) fail. After a flood, this water can be drained again into the lower course of the river through excavations of the overflow areas and through the Dalem de-inundation lock. It is also possible to excavate three dike sections at Dalem to accelerate the drainage of water. This is
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In 1254, Floris van Dalem was enfeoffed with the lordship of Dalem by Jan van der Leede and Hugo van Arkel. In 1423, his descendant Lord Floris van Dalem sold the lordships of Dalem, Schuvenoord, and Staden for 2260 crowns to the
Gelderland Duke Arnoud. From him, the ownership passed to Charles of
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The natural location of Dalem, in the lowest part of the
Tielerwaard, has regularly caused flooding over the centuries. Together with the entire Betuwe region, the Tielerwaard served as a water catchment area during times of extremely high water, protecting the even lower-lying
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and stayed at the (old) Doelen (Molenstraat). When he visited the threatened areas and was on the
Dalemsedijk with his carriage, a part of the dike broke. The king had to be taken away by boat. When the formwork collapsed on the Kortendijk on January 30, the water from the
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of wood. The first stone for the lock in its approximately current form was laid in 1661. Dike construction began in the 13th century, before which there were no dike breaches because there were no dikes.
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Dike breaches at that time were usually caused by ice dams in the river, blocking the flow of water. Sometimes the dams became so high that houses on the outside of the dike were destroyed.
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area, and work began on
January 18 to create outlets in the Dalem overflow areas. By January 25, 1809, so much water had flowed down through the Betuwe region that the city of
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flowed into the lower city through the
Hoogstraat and the alleys. Soldiers and citizens managed to close the gaps with great effort and prevented the city from being flooded.
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On June 16, 1518, other sources mention 1517, Duke
Charles granted the lordship of Dalem for life to Christoffel, Count of Meurs. This warrior was favored by both
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Lower Dalem is the lowest-lying area of the
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128:(it was during the French period) unexpectedly arrived in the city with his entourage from
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32:. Until January 1, 1818, Dalem was the name of the municipality, which was then renamed
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In the year 1809, on the night of
January 14 to 15, there was a dike breach in the
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Egmont, Duke of Guelders, who first pawned Dalem to Willem van Rossum for 300
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Dalem is a village in the Tielerwaard region in the municipality of
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Location in the province of South Holland in the Netherlands
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until 1986 and was part of the former municipality of
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476:"Kerncijfers wijken en buurten 2021"
598:Former municipalities of Gelderland
330:1.50 km (0.58 sq mi)
546:. You can help Knowledge (XXG) by
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593:Populated places in South Holland
93:In the event of a dike breach in
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24:. The village belonged to the
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608:South Holland geography stubs
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480:Central Bureau of Statistics
242:Location in the Netherlands
20:, in the Dutch province of
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501:"Postcodetool for 4213CD"
359:590/km (1,500/sq mi)
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212:Show map of South Holland
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338:0.3 m (1.0 ft)
245:Show map of Netherlands
542:location article is a
101:The de-inundation lock
26:province of Gelderland
451:Dutch Reformed church
382: • Summer (
148:region was submerged.
356: • Density
274:51.82778°N 5.00944°E
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135:Linge River
118:Over-Betuwe
587:Categories
457:References
343:Population
265:05°00′34″E
262:51°49′40″N
86:Meuse Rive
603:Gorinchem
365:Time zone
335:Elevation
316:Gorinchem
122:Gorinchem
18:Gorinchem
302:Province
142:Kedichem
426:Gallery
291:Country
165:Village
40:History
130:Vianen
538:This
511:3 May
485:3 May
391:UTC+2
370:UTC+1
236:Dalem
203:Dalem
158:Dalem
34:Vuren
30:Vuren
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513:2022
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322:Area
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