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Gender (stream)
The Gender () is a stream in the Dutch province of North Brabant. It originates in originally marshy flatlands near Steensel and flows through Veldhoven and its eastern district Meerveldhoven in a general east-northeast direction towards Eindhoven. The Gender is one of many small streams that drain what once was the marshy heath and moorland of eastern North Brabant and the Kempen plateau. Similar streams include the Dommel, Kleine Dommel, Keersop, Tongelreep, Aa, Binnendieze and Run. All of these streams at one point or other merge to finally form River Dieze in Den Bosch, which in turn flows into River Maas. Near Eindhoven, the Gender originally flowed just north of the medieval city walls, serving as the north part of the city moat, to end in confluence with the Dommel stream. As early as the fifteenth century, its course was diverted southward through the city centre, to provide the city with freshwater supplies and fire-extinguishing means. By the 19th century, the stretc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Netherlands
) , anthem = ( en, "William of Nassau") , image_map = , map_caption = , subdivision_type = Sovereign state , subdivision_name = Kingdom of the Netherlands , established_title = Before independence , established_date = Spanish Netherlands , established_title2 = Act of Abjuration , established_date2 = 26 July 1581 , established_title3 = Peace of Münster , established_date3 = 30 January 1648 , established_title4 = Kingdom established , established_date4 = 16 March 1815 , established_title5 = Liberation Day (Netherlands), Liberation Day , established_date5 = 5 May 1945 , established_title6 = Charter for the Kingdom of the Netherlands, Kingdom Charter , established_date6 = 15 December 1954 , established_title7 = Dissolution of the Netherlands Antilles, Caribbean reorganisation , established_date7 = 10 October 2010 , official_languages = Dutch language, Dutch , languages_type = Regional languages , languages_sub = yes , languages = , languages2_type = Reco ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Plateau
In geology and physical geography, a plateau (; ; ), also called a high plain or a tableland, is an area of a highland consisting of flat terrain that is raised sharply above the surrounding area on at least one side. Often one or more sides have deep hills or escarpments. Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, and erosion by water and glaciers. Plateaus are classified according to their surrounding environment as intermontane, piedmont, or continental. A few plateaus may have a small flat top while others have wide ones. Formation Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, Plate tectonics movements and erosion by water and glaciers. Volcanic Volcanic plateaus are produced by volcanic activity. The Columbia Plateau in the north-western United States is an example. They may be formed by upwelling of volcanic magma or extrusion of lava. The un ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Archaeology
Archaeology or archeology is the scientific study of human activity through the recovery and analysis of material culture. The archaeological record consists of artifacts, architecture, biofacts or ecofacts, sites, and cultural landscapes. Archaeology can be considered both a social science and a branch of the humanities. It is usually considered an independent academic discipline, but may also be classified as part of anthropology (in North America – the four-field approach), history or geography. Archaeologists study human prehistory and history, from the development of the first stone tools at Lomekwi in East Africa 3.3 million years ago up until recent decades. Archaeology is distinct from palaeontology, which is the study of fossil remains. Archaeology is particularly important for learning about prehistoric societies, for which, by definition, there are no written records. Prehistory includes over 99% of the human past, from the Paleolithic until the adven ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Confluence
In geography, a confluence (also: ''conflux'') occurs where two or more flowing bodies of water join to form a single channel. A confluence can occur in several configurations: at the point where a tributary joins a larger river (main stem); or where two streams meet to become the source of a river of a new name (such as the confluence of the Monongahela and Allegheny rivers at Pittsburgh, forming the Ohio); or where two separated channels of a river (forming a river island) rejoin at the downstream end. Scientific study of confluences Confluences are studied in a variety of sciences. Hydrology studies the characteristic flow patterns of confluences and how they give rise to patterns of erosion, bars, and scour pools. The water flows and their consequences are often studied with mathematical models. Confluences are relevant to the distribution of living organisms (i.e., ecology) as well; "the general pattern ownstream of confluencesof increasing stream flow and decreasing s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Moat
A moat is a deep, broad ditch, either dry or filled with water, that is dug and surrounds a castle, fortification, building or town, historically to provide it with a preliminary line of defence. In some places moats evolved into more extensive water defences, including natural or artificial lakes, dams and sluices. In older fortifications, such as hillforts, they are usually referred to simply as ditches, although the function is similar. In later periods, moats or water defences may be largely ornamental. They could also act as a sewer. Historical use Ancient Some of the earliest evidence of moats has been uncovered around ancient Egyptian castles. One example is at Buhen, a castle excavated in Nubia. Other evidence of ancient moats is found in the ruins of Babylon, and in reliefs from ancient Egypt, Assyria, and other cultures in the region. Evidence of early moats around settlements has been discovered in many archaeological sites throughout Southeast Asia, including ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
City Walls
A defensive wall is a fortification usually used to protect a city, town or other settlement from potential aggressors. The walls can range from simple palisades or earthworks to extensive military fortifications with towers, bastions and gates for access to the city. From ancient to modern times, they were used to enclose settlements. Generally, these are referred to as city walls or town walls, although there were also walls, such as the Great Wall of China, Walls of Benin, Hadrian's Wall, Anastasian Wall, and the Atlantic Wall, which extended far beyond the borders of a city and were used to enclose regions or mark territorial boundaries. In mountainous terrain, defensive walls such as ''letzis'' were used in combination with castles to seal valleys from potential attack. Beyond their defensive utility, many walls also had important symbolic functions representing the status and independence of the communities they embraced. Existing ancient walls are almost always masonry st ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Meuse (river)
The Meuse ( , , , ; wa, Moûze ) or Maas ( , ; li, Maos or ) is a major European river, rising in France and flowing through Belgium and the Netherlands before draining into the North Sea from the Rhine–Meuse–Scheldt delta. It has a total length of . History From 1301 the upper Meuse roughly marked the western border of the Holy Roman Empire with the Kingdom of France, after Count Henry III of Bar had to receive the western part of the County of Bar (''Barrois mouvant'') as a French fief from the hands of King Philip IV. In 1408, a Burgundian army led by John the Fearless went to the aid of John III against the citizens of Liège, who were in open revolt. After the battle which saw the men from Liège defeated, John ordered the drowning in the Meuse of suspicious burghers and noblemen in Liège. The border remained stable until the annexation of the Three Bishoprics Metz, Toul and Verdun by King Henry II in 1552 and the occupation of the Duchy of Lorraine by the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Den Bosch
s-Hertogenbosch (), colloquially known as Den Bosch (), is a city and municipality in the Netherlands with a population of 157,486. It is the capital of the province of North Brabant and its fourth largest by population. The city is south of the Maas river and near the Waal; it is to the north east of the city of Tilburg, north west of Eindhoven, south west of Nijmegen, and a longer distance south of Utrecht and south east of Dordrecht. History The city's official name is a contraction of the (archaic) Dutch ''des Hertogen bosch'' — "the forest of the duke". The duke in question was Henry I of Brabant, whose family had owned a large estate at nearby Orthen for at least four centuries. He founded a new town located on some forested dunes in the middle of a marsh. At age 26, he granted 's-Hertogenbosch city rights and the corresponding trade privileges in 1185. This is, however, the traditional date given by later chroniclers; the first mention in contemporaneous sources is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dieze
The Dieze is a short river in North Brabant, the Netherlands, tributary of the Meuse (). It is formed by the confluence of the rivers Aa and Dommel in 's-Hertogenbosch. The part of the Dieze in the centre of 's-Hertogenbosch is called Binnendieze, a partly covered network of canals. The Dieze flows into the Meuse near Hedel. Dieze and Dommel Of the two rivers that form the Dieze, the Dommel is the main river, and the Aa is her tributary. It is remarkable that after this confluence, the last 5 km of the 125-km stream bed of the Dommel is named 'Dieze'. This has historic reasons. The name 'Dieze' used to refer to a river running from Oisterwijk to the Meuse. It consisted of the Esschestroom, which now runs for only 7 km from Oisterwijk to Halder; the Dommel from Halder to 's-Hertogenbosch; the Binnendieze and Aa in 's-Hertogenbosch, and the current Dieze. All of this (about 25 km) was known as the Dieze, because the Dommel was considered to be her tributary. When the Dommel ca ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Run (stream)
The Run is a stream in the Dutch province of North Brabant. It is a left tributary of the Dommel and part of the Meuse basin. The Run originates near the town of Weebosch and flows in a general northeast direction towards Veldhoven. South of Eersel it flows near the hamlets of Stokkelen, Schadewijk and Stevert. Near the hamlet Stevert used to be a watermill in the Run, which became obsolete in 1969 due to the channelization of the stream. Further downstream the Run passes the hamlet of Heers until it discharges into the Dommel, just south of Veldhoven Veldhoven () is a municipality and town on the Gender in the southern Netherlands, just southwest of Eindhoven. Topography Dutch topographic map of Veldhoven (town), Dec. 2013 Population centres The modern town of Veldhoven is an agglomerat .... References Rivers of North Brabant Rivers of the Netherlands {{Netherlands-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Binnendieze
Binnendieze is the common name for all rivers and canals inside the city walls of 's-Hertogenbosch, the Netherlands. It is a major tourist attraction. Near the north-west tip of the city walls, the confluence of the Binnendieze with the rivers Aa River (Meuse), Aa and Dommel forms the short river Dieze, tributary of the Meuse ( nl, Maas). Dieze and Dommel The Dommel originates in Belgium and flows through Eindhoven and 's-Hertogenbosch to join the Meuse. However, inside 's-Hertogenbosch and further downstream, the Dommel is known as (Binnen)Dieze. This has historic reasons. In the past, locals considered the Esschestroom, or Run, which runs from Oisterwijk to Halder, to be the main stream bed of the Dommel. Therefore they applied the name 'Dieze' to the whole stretch between Oisterwijk and the Meuse. When the Dommel came to be considered the main river, the stretch of the Dieze between Oisterwijk and Halder was renamed Esschestroom, or Run. The stretch between Halder and 's- ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aa River (Meuse)
The Aa () is a small river in the Netherlands. It rises near Nederweert in the southeastern province of Limburg, in the Peel region. It flows northwest through the province of North Brabant towards 's-Hertogenbosch, roughly along the Zuid-Willemsvaart canal. In 's-Hertogenbosch, at the confluence of the Aa and the Dommel, the river Dieze is formed, which flows into the Meuse ( nl, Maas) a few km further. The main cities and towns along the Aa's course are Asten, Helmond, Veghel and 's-Hertogenbosch. History The old Aa was navigable The current Aa is not as important as the former river. This is due to the Zuid-Willemsvaart, which has been dug in the drainage basin of the Aa from 1823 to 1826. The canal absorbs much of the water that would otherwise flow to the Aa. The Zuid-Willemsvaart was initially dug to be much wider than the Aa, but since then its width and depth accelerated, taking ever more water from the Aa. The role of the Aa in history can only be understood by co ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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