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A remarkable aspect of the Netherlands is the flatness of the country. About half of its surface area is less than 1 meter (3.3 ft) above sea level, and large parts of it are actually below sea level. An extensive range of dykes and dunes protects these areas from flooding. Numerous massive pumping stations keep the ground water level in check. The highest point, the Vaalserberg, in the south-eastern most point of the country, is 321 meters (1,053 ft) above sea level. A substantial part of the Netherlands, for example, all of Flevoland (the largest man-made island in the world) and large parts of Holland, has been reclaimed from the sea. These areas are known as polders. This has led to the saying "God created the world, but the Dutch created the Netherlands." In years past, the Dutch coastline has changed considerably due to human intervention and natural disasters. Most notable in terms of land loss are the 1134 storm, which created the archipelago of Zeeland in the south west, and the 1287 storm, which killed 50,000 people and created the Zuyderzee in the northwest, giving Amsterdam direct access to the sea. The St. Elizabeth flood of 1421 and the mismanagement in its aftermath destroyed a newly reclaimed polder, replacing it with the 72 square kilometers (28 sq mi) Biesbosch tidal floodplain's in the south-center. The most recent parts of Zeeland were flooded during the North Sea Flood of 1953 and 1,836 people were killed, after which the Delta Plan was executed. The disasters were partially man-made; the people drained relatively high lying swampland for use as farmland. This drainage caused the fertile peat to compress and the ground level to drop, locking the land users in a vicious circle whereby they would lower the water level to compensate for the drop in ground level, causing the underlying peat to compress even more. The vicious circle is unsolvable and remains to this day. Up until the 19th century peat was dug up, dried, and used for fuel, further adding to the problem. To guard against floods, a series of defenses against the water were contrived. In the first millennium, villages and farmhouses were built on man-made hills called terps. Later, these terps were connected by dikes. In the 12th century, local government agencies called "waterschappen" (English "water bodies") or "hoogheemraadschappen" ("high home councils") started to appear, whose job it was to maintain the water level and to protect a region from floods. (The water bodies are still around today performing the exact same function.) As the ground level dropped, the dikes by necessity grew and merged into an integrated system. In the 13th century, windmills came into use to pump water out of the areas by now below sea level. The windmills were later used to drain lakes, creating the famous polders. In 1932, the Afsluitdijk (English "Closure Dike") was completed, blocking the former Zuyderzee (Southern Sea) off from the North Sea and thus creating the IJsselmeer (IJssel Lake). It became part of the larger Zuiderzee Works in which four polders totaling 1,650 square kilometers (637 sq mi) were reclaimed from the sea. After the 1953 disaster, the Delta project, a vast construction effort designed to end the threat from the sea once and for all, was launched in 1958 and largely completed in 2002. The official goal of the Delta project was to reduce the risk of flooding in Holland to once per 10,000 years. (For the rest of the country, the protection-level is once per 4,000 years.) This was achieved by raising 3,000 kilometers (1,864 mi) of outer sea-dikes and 10,000 kilometers (6,200 mi) of inner, canal, and river dikes to "delta" height, and by closing off the sea estuaries of the Zeeland province. New risk assessments occasionally incur additional Delta project work in the form of dike reinforcements. The Delta project is the single largest construction effort in human history and is considered by the American Society of Civil Engineers as one of the seven wonders of the modern world. Because of the high cost of maintaining the polders some have argued that maybe some of the deepest polders should be given up. Additionally, the Netherlands is one of the countries that may suffer most from climatic change. Not only is the rising sea a problem, but also erratic weather patterns may cause the rivers to overflow. These flooded polders might then be used as water catchments to take part of the blow. The country is divided into two main parts by three rivers Rhine (Rijn), Waal, and Meuse (Maas). The south-western part of the Netherlands is actually one big river delta of these rivers. These rivers not only function as a natural barrier, but also as a cultural divide, as is evident in the different dialects spoken north and south of these great rivers and the (previous) religious dominance of Catholics in the south and Calvinists in the north. The predominant wind direction in the Netherlands is south-west, which causes a moderate maritime climate, with cool summers and mild winters. |
Netherlands Information: Inside
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