Gooi
Gooi
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Gooi

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Gooi

The Gooi (Dutch: Het Gooi [ət ˈxoːi]) is an area around Hilversum, in the centre of the Netherlands. It is a slightly hilly area characterised by its green landscape, its historical charm, the wealth of its inhabitants and its villas. The Gooi is known in the country as the home of the rich and famous.

The name Gooi is related to gouw, the Dutch word for "gau", being an old name for a 'region'. The Gooi is conventionally referred to in Dutch as het Gooi[citation needed] or 't Gooi, literally meaning 'the Gooi'. It is also sometimes referred to as "Gooiland". In English, the area is generally referred to as "Het Gooi" (capital "H") or "the Gooi area".

The Gooi is the area around Hilversum in the southeastern corner of the province of North Holland. It is located east of Amsterdam and north of Utrecht, between Amersfoort and Amsterdam. The boundaries are not clearly demarcated. It is generally the area between a dry ditch called the Gooyergracht, dug in 1356 to demarcate the border with the province of Utrecht, and the river Vecht. The Gooi refers traditionally to the part of this area that lies in the province of North Holland. Often the term is used to refer just to the higher, sandy, forested part of this area. The towns in the area include (in descending order of size): Hilversum (the centre of the area and the largest municipality), Bussum and Naarden, Huizen, Laren and Blaricum.

To the north of the Gooi there is a body of water called Lake Gooi (in Dutch, Gooimeer), a southern extension of the IJsselmeer. An area called the Vechtstreek lies to the west of the Gooi. Eemland in the province of Utrecht lies to the east. The towns of Weesp and Eemnes are also sometimes thought to be in the Gooi. Their inclusion would mean that the region extends in the west to the Amsterdam–Rhine Canal (not just to the Vecht) and in the east to the river Eem (not just to the Gooyergracht). However, historically and geographically these towns are not really part of the Gooi. Weesp is part of the Vechtstreek and Eemnes part of Eemland.

To the west and southwest there are two lake systems called the Loosdrecht Lakes (Loosdrechtseplassen) and the Ankeveen Lakes (Ankeveenscheplassen). On 1 January 2002 the towns in the area of these lake systems was organised into a municipality called Wijdemeren. This municipality includes Ankeveen, Breukeleveen, 's-Graveland, Kortenhoef, Muyeveld, Nederhorst den Berg, Nieuw-Loosdrecht and Oud-Loosdrecht. Some of this area is fenland. Since then this area has also been considered to be part of the Gooi, although historically not all of it was. Pasture land called the Utrechtse weilanden lies to the south. To the southeast lies a wooded area in the province of Utrecht called the Laagte van Pijnenburg, or Pijnenburg Depression, marking the transition to the central part of the Utrecht Hill Ridge.

Two motorways run through the Gooi: the A1 runs east and west; the A27 runs north and south. The railways running from Amsterdam to Hilversum and Amersfoort (Gooilijn, part of the Amsterdam–Zutphen railway) and from Hilversum to Utrecht (Hilversum–Lunetten railway) run through the area. A line called the "Gooiboog" links the Gooilijn with the Weesp–Lelystad railway (Flevolijn) to Almere and Lelystad.

The Gooi is centred on the northernmost point of a geological formation called the Utrecht Hill Ridge (Utrechtse Heuvelrug). The "hilliness" of this area is relative. It is considered hilly because the rest of the countryside is flat and below sea level. The highest point in the Gooi is the Tafelberg (36.4 m above sea level), which is located halfway between Blaricum and Huizen.

Originally the Gooi area was covered with woods and heath. It was at one time encircled by treacherous high and low fen areas (with peat bogs) that created a natural barrier and isolated it from the Utrecht area to the south. Today there is still a good amount of variation in the landscape in the Gooi area. The landscape is dominated by a dry, sandy ridge. To the east and west of the ridge there is flat wet low-lying pasture land. The changes in land elevation, and the transition from wet to dry, are important for many animals and plants. The bodies of water at the margins of the area are fed by water seeping through the sandy ridge.

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