Netherlands: Difference between revisions
→Geography
Dutch-ODST (talk | contribs) No edit summary |
Dutch-ODST (talk | contribs) |
||
Line 124:
The European Netherlands is geographically very low relative to sea level and is a mostly flat country, with roughly 31% of its area and 39% of its population located below sea level and only about 50% of its land exceeding one meter above sea level. The European mainland is for the most part flat, with the exception of foothills in the far southeast that stretch to a height of no more than 321 meters; additionally there are some low hill ranges in the central region of the country. Most regions below sea level are man-made, caused by peat extraction or achieved through land reclamation. Since the late 16th century, through elaborate drainage systems that include dikes, canals and pumping stations, large areas of coastal land were reclaimed from the sea (known as polders). Today nearly 23% of the country's land area is reclaimed from the sea and from lakes.
Much of the country was originally formed by the estuaries of three large European rivers: the Rhine (''Rijn''), the Meuse (''Maas'') and the Scheldt (''Schelde''), as well as their tributaries. These three rivers create the largest river delta in the country which also creates the whole south-western geographic region of the Netherlands, the Rhine-Meuse-Scheldt delta. The European Netherlands is divided into north and south by the Rhine, the Waal, its main tributary branch, and the Meuse. In the past, these rivers functioned as a natural barrier between fiefdoms and have historically created a cultural divide, this is evident in some phonetic traits that are
== Government and politics ==
| |||