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De Hoge Veluwe National Park (Dutch pronunciation: [də ˈɦoːɣə ˈveːlyʋə]; "The High Veluwe") is a Dutch national park in the province of Gelderland near the cities of Ede, Wageningen, Arnhem and Apeldoorn. It is approximately 55 km 2 (14,000 acres; 21 sq mi) in area, consisting of heathlands, sand dunes, and woodlands.
Veluwezoom National Park is a national park in the Netherlands located in the province of Gelderland.It is the oldest national park in the Netherlands. [2] It has a surface area of about 50 square kilometers (some 20 square miles) at the southeastern edge of the Veluwe, a complex of terminal push moraines from the Saalian glaciation.
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The Museonder is a Dutch museum in the De Hoge Veluwe National Park The museum focuses on the geology and biology of the Veluwe and calls itself the world's first fully underground museum. [1] The name "Museonder" is a portmanteau of the Dutch words for "museum" and "under", respectively "museum" and "onder".
Helene Müller and Anton Kröller, c. 1888. The Kröller-Müller Museum was founded by Helene Kröller-Müller, an avid art collector who, being advised by H.P. Bremmer, was one of the first to recognize Vincent van Gogh's genius and collect his works.
Areas where the Dutch Christian right Reformed Political Party (SGP) received a significant number of votes in 2010, largely co-extensive with the Dutch Bible Belt. The Bible Belt (Dutch: bijbelgordel, biblebelt) is a strip of land in the Netherlands with the highest concentration of conservative orthodox Reformed Protestants in the country.
NUTS 1 Code NUTS 2 Code NUTS 3 Code North Netherlands NL1 Groningen: NL11 East Groningen NL111 Delfzijl and surroundings NL112 Rest of Groningen NL113 Friesland: NL12 North Friesland NL124 South West Friesland NL125 South East Friesland NL126 Drenthe: NL13 North Drenthe NL131 South East Drenthe NL132 South West Drenthe NL133 East Netherlands NL2
The Veluwe is the largest push moraine complex in the Netherlands, stretching 60 km (40 miles) from north to south, and reaching heights of up to 110 metres (360'). The Veluwe was formed by the Saalian glacial during the Pleistocene epoch, some 200,000 years ago. Glaciers some 200 metres (600') thick pushed the sand deposits in the Rhine and ...