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North Brabant topographic map
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North Brabant
The historical region of Kempen occupies the southern part of the province of Noord-Brabant and extends south of Eindhoven far into northern Belgium. To the east it reaches as far as the Meuse valley. The surface topography of De Kempen is very uniform. Most of it lies between 5 m (15 ft) and 35 m (115 ft) above sea level. The basement rocks are Cretaceous and Tertiary sediments, which are overlaid by Ice Age gravels and sands carried here by rivers of melt-water from the retreating glaciers. It is a typical area of sandy heathland. The infertile soil is suitable only for undemanding crops such as rye, oats, potatoes and fodder plants; this limits the profitability of agriculture. Until a few decades ago Kempen was a region of heathland and sand drifts with a sparse growth of pines, a few scattered villages subsisting on the poor soil and some small towns; and this is still the pattern in much of the region. In recent years, however, the rapid advance of industry has brought about profound changes in this agricultural region. The origins of this industrial development go back 70–100 years. The main concentrations of industry are along the southern frontier of the Netherlands, e.g., at Eindhoven, Helmond, Tilburg, Breda, 's-Hertogenbosch.
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About this map
Name: North Brabant topographic map, elevation, terrain.
Location: North Brabant, Netherlands (49.00177 2.84414 54.20177 8.04414)
Average elevation: 325 ft
Minimum elevation: -23 ft
Maximum elevation: 2,743 ft
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Other topographic maps
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The construction of the tower and the church was started in 1444. The church was destroyed by an explosion in 1787, but the tower survived, and the layout of the church still can be discerned today through the use of different types of stone in the pavement of the open space that was created. It is now the…
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Amersfoort
The construction of the tower and the church was started in 1444. The church was destroyed by an explosion in 1787, but the tower survived, and the layout of the church still can be discerned today through the use of different types of stone in the pavement of the open space that was created. It is now the…
Average elevation: 23 ft
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Etten-Leur
Dutch topographic map of Etten-Leur (town), March 2014
Average elevation: 16 ft
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Groesbeek
Due to this, the topography is much more varied here than in other higher grounds with similar origins in the Netherlands. Finally, during the Younger Dryas stadial, large amounts of loess were deposited in the valley, making it extremely fertile, while the hills around it are composed to this day of sandy…
Average elevation: 135 ft
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Renswoude
Dutch Topographic map of the municipality of Renswoude, June 2015
Average elevation: 26 ft
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Wageningen
Topographic map of the municipality of Wageningen, July 2013 (click to enlarge)
Average elevation: 43 ft
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Someren
Dutch Topographic map of the municipality of Someren, June 2015
Average elevation: 85 ft
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Breda
Topographic map image of the city of Breda, March 2014. Click to enlarge.
Average elevation: 23 ft
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Den Helder
Netherlands > North Holland > Den Helder
Dutch Topographic map of Den Helder (town), March 2014.
Average elevation: 0 ft
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The villages and city that make up modern Eindhoven were originally built on sandy elevations between the Dommel, Gender and Tongelreep rivers. Beginning in the 19th century, the basins of the rivers themselves have also been used as housing land, resulting in occasional flooding in the city centre. Partly to…
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Goes
Netherlands > Zeeland > Goes
Dutch Topographic map of Goes (town), Sept. 2014.
Average elevation: 0 ft
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