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The IJsselmeer [a] (Dutch: [ˌɛisəlˈmeːr] ⓘ; West Frisian: Iselmar, Dutch Low Saxon: Iesselmeer), also known as Lake IJssel in English, [3] is a closed-off freshwater lake in the central Netherlands bordering the provinces of Flevoland, North Holland and Friesland.
This body of water is then pumped up into the IJsselmeer. It is sometimes called the Gelderse IJssel (IPA: [ˌɣɛldərsə ˈʔɛisəl] ⓘ; "Gueldern IJssel") to distinguish it from the Hollandse IJssel. It is in the provinces of Gelderland and Overijssel, the latter of which was named after this river. The Romans knew the river as Isala.
All of the Netherlands is drained into the North Sea, partly via the IJsselmeer lake. In the list below, rivers that flow into the sea are sorted following the North Sea coast (including IJsselmeer) from the Belgian border near Knokke to the German border near Emden. Rivers that flow into other rivers are sorted by the proximity of their points ...
The park is in Breitung Township, on the shore of Lake Vermilion in northern Minnesota's Vermilion Range. It has become a popular tourist site, often visited on the way to and from Ely and the Boundary Waters Canoe Area Wilderness. [citation needed] The state park is operated under the Department of Natural Resources.
The salt water inlet changed into a fresh water lake now called the IJsselmeer (IJssel Lake) after the river that drains into it, and by means of drainage and polders, an area of some 1,500 km 2 (580 sq mi) was reclaimed as land. This land eventually became the province of Flevoland. [1] Part of the IJsselmeer was also divided into the Markermeer.
The 1953 flood disaster prompted a new approach to the design of dikes and other water-retaining structures, based on an acceptable probability of overflowing. Risk is defined as the product of probability and consequences. The potential damage in lives, property and rebuilding costs is compared to the potential cost of water defences.
Almost all of the land belonging to Flevoland was reclaimed in the 1950s and 1960s [5] while splitting the Markermeer and Bordering lakes from the IJsselmeer. As to dry land, it is the smallest province of the Netherlands at 1,410 km 2 (540 sq mi), but not gross land as that includes much of the waters of the fresh water lakes (meres) mentioned ...
The inner berm slope toward the future water level of the IJsselmeer (or Amstelmeer) was designed to be steeper than the outer slope, with a ratio of approximately 1:3. The majority of the dam's core consisted of sand, while boulder clay on the exterior provided resistance against water flow, limiting seepage and enhancing dike breach protection.