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The geography of the European Netherlands is unusual in that much of its land has been reclaimed from the sea and is below sea level, protected by dikes. It is a small country with a total area of 41,545 km 2 (16,041 sq mi) [ 1 ] and ranked 131st .
The Dutch Waterline [1] [2] (Dutch: Hollandsche Waterlinie, modern spelling: Hollandse Waterlinie) was a series of water-based defences conceived by Maurice of Nassau in the early 17th century, and realised by his half brother Frederick Henry.
The Dutch Water Defence lines (Dutch: Hollandse Waterlinies) [1] is a UNESCO World Heritage Site in the Netherlands comprising the New Dutch Waterline and Stelling van Amsterdam. The Stelling van Amsterdam was added as a World Heritage Site in 1996, and was extended in 2021 with the New Dutch Waterline in 2021. [2]
The countries that comprise the region called the Low Countries (Netherlands, Belgium, and Luxembourg) all have comparatively the same toponymy.Place names with Neder, Nieder, Nedre, Nether, Lage(r) or Low(er) (in Germanic languages) and Bas or Inferior (in Romance languages) are in use in low-lying places all over Europe.
Southern Bight, also known as the Flanders Bight, and (in Dutch) the Hoofden, is the southern bight of the North Sea bounded by the coasts of the Netherlands, Belgium, France and Great Britain. The Southern Bight is south west of the German Bight and the Wadden Sea.
The coastline paradox states that a coastline does not have a well-defined length. Measurements of the length of a coastline behave like a fractal, being different at different scale intervals (distance between points on the coastline at which measurements are taken). The smaller the scale interval (meaning the more detailed the measurement ...
The Royal Netherlands Navy Hydrographic Service was founded in 1874 as Bureau Hydrografie. [3] It was led by a Chef der Hydrografie, with the first chef being A.R. Blommendal. [ 3 ] Since its creation the Hydrographic service has been responsible for chartering the waters of the Netherlands and tasked with reporting any changes of the fairways ...
The recent Netherlands is formed by Pleistocene and Holocene age sediments as result of -fluvial, eolian and marine sedimentation. Eolian dunes characterise the North Sea coast, a horseshoe-shaped moraine forms the Utrecht Hill Ridge (Dutch: Utrechtse Heuvelrug) and the river influence is still visible all over the Netherlands.