Kinderdijk Travel Blog› entry 10 of 11 › view all entries
WOO HOO WELCOME TO THE LAND OF WINDMILLS
Kinderdijk is situated in a polder at the confluence of the Lek and Noord rivers. To drain the polder, a system of 19 windmills was built around 1740. This group of mills is the largest concentration of old windmills in the Netherlands.
The windmills of Kinderdijk are one of the best known Dutch tourist sites.
Origin of the name
The name Kinderdijk is Dutch for "Child's Dike". In 1421 during the Saint Elizabeth flood of 1421, the Grote Hollandse Waard flooded, but the Alblasserwaard polder stayed unflooded. It is said that when the terrible storm had subsided, someone went on to the dike between these two areas, to see what could be saved. He saw in the distance a wooden cradle floating. There was no hope that anything would be living in it, but when it approached, movement was seen. When the cradle came nearer, someone saw that a cat was in the cradle trying to keep it in balance by jumping back and forth so that no water could come into it. When the cradle eventually came near the dike, someone fished the cradle out and saw that in it a baby slept quiet and dry.
In the Netherlands, the drainage system is an important matter. The Dutch need a well developed water control system in order to keep large areas from being flooded, because some parts of the Netherlands are below sea level. In Alblasserwaard, problems with water became more and more apparent in the 13th century. Large canals, called 'weteringen', were dug to get rid of the excess water in the polders. However, the drained soil started setting, while the level of the river rose due to the river's sand deposits. After a few centuries, an additional way to keep the polders dry was required. It was decided to build a series of windmills, with a limited capacity to bridge water level differences, but just able to pump water into a reservoir at an intermediate level between the soil in the polder and the river; the reservoir could be pumped out into the river by other windmills whenever the river level was low enough; the river level has both seasonal and tidal variations.
Full control over the water level was never achieved. Throughout the centuries, the residents of the western part of the Netherlands suffered inundations, especially because of dyke ruptures; this is reflected the legend of the floating cradle at Kinderdijk and the figure of Hans Brinker with his finger in a ruptured dyke.