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Neeroeteren
Maaseik (; li, Mezeik) is a city and municipality in the Belgian province of Limburg. Both in size (close to 77 km2) and in population (approx. 25,000 inhabitants, of whom some 3,000 non-Belgian), it is the 8th largest municipality in Limburg. The town is the seat of the administrative arrondissement of Maaseik (''kieskanton''). Internationally, Maaseik is known as the assumed birthplace of the famous Flemish painters Jan and Hubert van Eyck. Geography The town of Maaseik is located on the left bank of the Meuse ( nl, Maas), bordering the Netherlands. For this reason the river is called ''Grensmaas'' (for "border Meuse") here. Two smaller rivers, the Bosbeek (or Oeterbeek) and the Zanderbeek (or Diepbeek), flow into the Meuse near Maaseik. Because of its location in the Meuse valley, Maaseik has mostly fertile soils. The northwestern part of the municipality is situated on the plain of Bocholt and has less fertile soils. The Meuse valley at Maaseik is about 4 kilometres wid ...
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Opoeteren
Maaseik (; li, Mezeik) is a City status in Belgium, city and Municipalities in Belgium, municipality in the Belgium, Belgian Provinces of Belgium, province of Limburg (Belgium), Limburg. Both in size (close to 77 km2) and in population (approx. 25,000 inhabitants, of whom some 3,000 non-Belgian), it is the 8th largest municipality in Limburg (Belgium), Limburg. The town is the seat of the Arrondissement of Maaseik, administrative arrondissement of Maaseik (''kieskanton''). Internationally, Maaseik is known as the assumed birthplace of the famous Flemish painters Jan van Eyck, Jan and Hubert van Eyck. Geography The town of Maaseik is located on the left bank of the Meuse ( nl, Maas), bordering the Netherlands. For this reason the river is called ''Grensmaas'' (for "border Meuse") here. Two smaller rivers, the Bosbeek (or Oeterbeek) and the Zanderbeek (or Diepbeek), flow into the Meuse near Maaseik. Because of its location in the Meuse valley, Maaseik has mostly fertile soils. T ...
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Neeroeteren
Maaseik (; li, Mezeik) is a city and municipality in the Belgian province of Limburg. Both in size (close to 77 km2) and in population (approx. 25,000 inhabitants, of whom some 3,000 non-Belgian), it is the 8th largest municipality in Limburg. The town is the seat of the administrative arrondissement of Maaseik (''kieskanton''). Internationally, Maaseik is known as the assumed birthplace of the famous Flemish painters Jan and Hubert van Eyck. Geography The town of Maaseik is located on the left bank of the Meuse ( nl, Maas), bordering the Netherlands. For this reason the river is called ''Grensmaas'' (for "border Meuse") here. Two smaller rivers, the Bosbeek (or Oeterbeek) and the Zanderbeek (or Diepbeek), flow into the Meuse near Maaseik. Because of its location in the Meuse valley, Maaseik has mostly fertile soils. The northwestern part of the municipality is situated on the plain of Bocholt and has less fertile soils. The Meuse valley at Maaseik is about 4 kilometres wid ...
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Meuse
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 ...
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Anabranch
An anabranch is a section of a river or stream that diverts from the main channel or stem of the watercourse and rejoins the main stem downstream. Local anabranches can be the result of small islands in the watercourse. In larger anabranches, the flow can diverge for a distance of several kilometers before rejoining the main channel. Word usage and related terms The term ''anabranch'', in its hydrological meaning, is used more frequently in Australia than in the rest of the English-speaking world. The term ''anabranching river'' describes a river with many anabranches, whilst an anastomosing river is an organic-rich subset of this river type. The term braided river describes watercourses which are divided by small islands into multiple channel threads within a single main channel, but the term does not describe the multiple channels of an anabranching river. A distributary is a branch of a river that does not rejoin the main channel; these are common on and near river d ...
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Toponymy
Toponymy, toponymics, or toponomastics is the study of ''toponyms'' (proper names of places, also known as place names and geographic names), including their origins, meanings, usage and types. Toponym is the general term for a proper name of any geographical feature, and full scope of the term also includes proper names of all cosmographical features. In a more specific sense, the term ''toponymy'' refers to an inventory of toponyms, while the discipline researching such names is referred to as ''toponymics'' or ''toponomastics''. Toponymy is a branch of onomastics, the study of proper names of all kinds. A person who studies toponymy is called ''toponymist''. Etymology The term toponymy come from grc, τόπος / , 'place', and / , 'name'. The ''Oxford English Dictionary'' records ''toponymy'' (meaning "place name") first appearing in English in 1876. Since then, ''toponym'' has come to replace the term ''place-name'' in professional discourse among geographers. Toponym ...
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Aldeneik
Aldeneik, founded in 730, is a suburb of the Belgian town of Maaseik. It lies on the left bank of the river Meuse, close to the border with the Netherlands, close to where the Bosbeek runs off it. According to legend it sprung up around a monastery set up by the Frankish sisters Herlindis and Relindis, who wrote the Gospel book known as the Codex Eyckensis, still in Maaseik. The settlement contains the Romanesque and Gothic Sint-Annakerk. Foundation legends Devil The Devil saw the sisters writing the Codex and could do nothing to stop them, until he had the idea of blowing out their candles. However, an angel came and re-lit them. Gallery Willibrordusput.jpg, 7th century baptistery built by Willibrord on the site of a shrine to Wōden Odin (; from non, Óðinn, ) is a widely revered god in Germanic paganism. Norse mythology, the source of most surviving information about him, associates him with wisdom, healing, death, royalty, the gallows, knowledge, war, battle, ...
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Watersports
Water sports or aquatic sports are sport activities conducted on waterbodies, and can be categorized according to the degree of immersion by the participants. On the water * Boat racing, the use of powerboats to participate in races * Boating, the use of boats for personal recreation * Cable skiing, similar to wake boarding but with cables for artificial maneuvering * Canoe polo combines boating and ball handling skills with a contact team game, where tactics and positional play are as important as the speed and fitness of the individual athletes. * Canoeing is an activity which involves paddling a canoe with a single-bladed paddle. Most present-day canoeing is done as or as a part of a sport or recreational activity. * Dragon boat racing, teams of 20 paddlers racing the ancient dragon boat * Fishing, the recreation and sport of catching fish * Flyboard, a brand of hydroflighting device which supplies propulsion to drive the Flyboard into the air to perform a sport known as ...
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Nature Reserve
A nature reserve (also known as a wildlife refuge, wildlife sanctuary, biosphere reserve or bioreserve, natural or nature preserve, or nature conservation area) is a protected area of importance for flora, fauna, or features of geological or other special interest, which is reserved and managed for purposes of conservation and to provide special opportunities for study or research. They may be designated by government institutions in some countries, or by private landowners, such as charities and research institutions. Nature reserves fall into different IUCN categories depending on the level of protection afforded by local laws. Normally it is more strictly protected than a nature park. Various jurisdictions may use other terminology, such as ecological protection area or private protected area in legislation and in official titles of the reserves. History Cultural practices that roughly equate to the establishment and maintenance of reserved areas for animals date bac ...
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Clay
Clay is a type of fine-grained natural soil material containing clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2 Si2 O5( OH)4). Clays develop plasticity when wet, due to a molecular film of water surrounding the clay particles, but become hard, brittle and non–plastic upon drying or firing. Most pure clay minerals are white or light-coloured, but natural clays show a variety of colours from impurities, such as a reddish or brownish colour from small amounts of iron oxide. Clay is the oldest known ceramic material. Prehistoric humans discovered the useful properties of clay and used it for making pottery. Some of the earliest pottery shards have been dated to around 14,000 BC, and clay tablets were the first known writing medium. Clay is used in many modern industrial processes, such as paper making, cement production, and chemical filtering. Between one-half and two-thirds of the world's population live or work in buildings made with clay, often ...
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Loam
Loam (in geology and soil science) is soil composed mostly of sand (particle size > ), silt (particle size > ), and a smaller amount of clay (particle size < ). By weight, its mineral composition is about 40–40–20% concentration of sand–silt–clay, respectively. These proportions can vary to a degree, however, and result in different types of loam soils: sandy loam, silty loam, clay loam, sandy clay loam, silty clay loam, and loam. In the , textural classification triangle, the only soil that is not predominantly sand, silt, or clay is called "loam". Loam soils generally contain more nutrients, moisture, and

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Gravel
Gravel is a loose aggregation of rock fragments. Gravel occurs naturally throughout the world as a result of sedimentary and erosive geologic processes; it is also produced in large quantities commercially as crushed stone. Gravel is classified by particle size range and includes size classes from granule- to boulder-sized fragments. In the Udden-Wentworth scale gravel is categorized into granular gravel () and pebble gravel (). ISO 14688 grades gravels as fine, medium, and coarse, with ranges 2–6.3 mm to 20–63 mm. One cubic metre of gravel typically weighs about 1,800 kg (or a cubic yard weighs about 3,000 lb). Gravel is an important commercial product, with a number of applications. Almost half of all gravel production is used as aggregate for concrete. Much of the rest is used for road construction, either in the road base or as the road surface (with or without asphalt or other binders.) Naturally occurring porous gravel deposits have a ...
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Sediment
Sediment is a naturally occurring material that is broken down by processes of weathering and erosion, and is subsequently transported by the action of wind, water, or ice or by the force of gravity acting on the particles. For example, sand and silt can be carried in suspension in river water and on reaching the sea bed deposited by sedimentation; if buried, they may eventually become sandstone and siltstone (sedimentary rocks) through lithification. Sediments are most often transported by water (fluvial processes), but also wind (aeolian processes) and glaciers. Beach sands and river channel deposits are examples of fluvial transport and deposition, though sediment also often settles out of slow-moving or standing water in lakes and oceans. Desert sand dunes and loess are examples of aeolian transport and deposition. Glacial moraine deposits and till are ice-transported sediments. Classification Sediment can be classified based on its grain size, grain shape, and c ...
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