De Peel is a region in the southeast of the Netherlands that straddles the border between the provinces of North Brabant and Limburg.
The region is best known for the extraction of peat for fuel[citation needed], which had been going on since the Middle Ages but is no longer done. For this purpose many canals were dug to remove the water and for ships to move out the peat.
An area that has remained partly untouched by the peat-cutting was turned into a National Park, the Groote Peel. It has a size of 13.4km².
It is one of the most bird-rich areas in Western Europe, with resident black-necked grebes and sometimes migrating common cranes in October/November. The terrain is varied with inaccessible peat swamps, lakes, heath land and sand ridges. The present swamp and some of the lakes were created by the cutting of peat.
There are very many villages in the Peel, the most of them founded by bosses of peat companies. For example: Helenaveen and Griendtsveen, founded by Jan van de Griendt (1804–1882)
Trivia
The Northern Limburgish band Rowwen Hèze made a well-known song about the area named: De Peel in brand (The Peel on fire).
Holland is a geographical region and former province on the western coast of the Netherlands. From the 10th to the 16th century, Holland proper was a unified political region within the Holy Roman Empire as a county ruled by the counts of Holland. By the 17th century, the province of Holland had risen to become a maritime and economic power, dominating the other provinces of the newly independent Dutch Republic.
Limburg is the southernmost of the 12 provinces of the Netherlands. The province is bordered by the province of Gelderland to the north and by North Brabant to its west. Its long eastern boundary forms the international border with the state of North Rhine-Westphalia in Germany. To the west is the international border with the similarly named Belgian province of Limburg, part of which is delineated by the river Meuse. The Vaalserberg is on the extreme south-eastern point, marking the tripoint of the Netherlands, Germany and Belgium.
A polder is a low-lying tract of land that forms an artificial hydrological entity, enclosed by embankments known as dikes. The three types of polder are:
Land reclaimed from a body of water, such as a lake or the seabed
Flood plains separated from the sea or river by a dyke
Marshes separated from the surrounding water by a dike and subsequently drained; these are also known as koogs, especially in Germany
A swamp is a forested wetland. Swamps are considered to be transition zones because both land and water play a role in creating this environment. Swamps vary in size and are located all around the world. The water of a swamp may be fresh water, brackish water, or seawater. Freshwater swamps form along large rivers or lakes where they are critically dependent upon rainwater and seasonal flooding to maintain natural water level fluctuations. Saltwater swamps are found along tropical and subtropical coastlines. Some swamps have hammocks, or dry-land protrusions, covered by aquatic vegetation, or vegetation that tolerates periodic inundation or soil saturation. The two main types of swamp are "true" or swamp forests and "transitional" or shrub swamps. In the boreal regions of Canada, the word swamp is colloquially used for what is more formally termed a bog, fen, or muskeg. Some of the world's largest swamps are found along major rivers such as the Amazon, the Mississippi, and the Congo.
America is a parish village in the Dutch province of Limburg, known historically for its peat extraction.
Peat, also known as turf, is an accumulation of partially decayed vegetation or organic matter. It is unique to natural areas called peatlands, bogs, mires, moors, or muskegs. The peatland ecosystem covers 3.7 million square kilometres (1.4 million square miles) and is the most efficient carbon sink on the planet, because peatland plants capture carbon dioxide (CO2) naturally released from the peat, maintaining an equilibrium. In natural peatlands, the "annual rate of biomass production is greater than the rate of decomposition", but it takes "thousands of years for peatlands to develop the deposits of 1.5 to 2.3 m [4.9 to 7.5 ft], which is the average depth of the boreal [northern] peatlands", which store around 415 gigatonnes (Gt) of carbon (about 46 times 2019 global CO2 emissions). Globally, peat stores up to 550 Gt of carbon, 42% of all soil carbon, which exceeds the carbon stored in all other vegetation types, including the world's forests, although it covers just 3% of the land's surface. Sphagnum moss, also called peat moss, is one of the most common components in peat, although many other plants can contribute. The biological features of sphagnum mosses act to create a habitat aiding peat formation, a phenomenon termed 'habitat manipulation'. Soils consisting primarily of peat are known as histosols. Peat forms in wetland conditions, where flooding or stagnant water obstructs the flow of oxygen from the atmosphere, slowing the rate of decomposition. Peat properties such as organic matter content and saturated hydraulic conductivity can exhibit high spatial heterogeneity.
A bog or bogland is a wetland that accumulates peat as a deposit of dead plant materials – often mosses, typically sphagnum moss. It is one of the four main types of wetlands. Other names for bogs include mire, mosses, quagmire, and muskeg; alkaline mires are called fens. A baygall is another type of bog found in the forest of the Gulf Coast states in the United States. They are often covered in heath or heather shrubs rooted in the sphagnum moss and peat. The gradual accumulation of decayed plant material in a bog functions as a carbon sink.
A marsh is a wetland that is dominated by herbaceous rather than woody plant species. Marshes can often be found at the edges of lakes and streams, where they form a transition between the aquatic and terrestrial ecosystems. They are often dominated by grasses, rushes or reeds. If woody plants are present they tend to be low-growing shrubs, and then sometimes called carrs. This form of vegetation is what differentiates marshes from other types of wetland such as swamps, which are dominated by trees, and mires, which are wetlands that have accumulated deposits of acidic peat.
Flooded grasslands and savannas is a terrestrial biome of the WWF biogeographical system, consisting of large expanses or complexes of flooded grasslands. These areas support numerous plants and animals adapted to the unique hydrologic regimes and soil conditions. Large congregations of migratory and resident waterbirds may be found in these regions. However, the relative importance of these habitat types for these birds as well as more vagile taxa typically varies as the availability of water and productivity annually and seasonally shifts among complexes of smaller and larger wetlands throughout a region.
Börger is a village and a municipality in the district Emsland in Lower Saxony, Germany. Börger is part of the administrative unit of Sögel.
Waterwolf, or Water-wolf is a Dutch word that comes from the Netherlands, which refers to the tendency of lakes in low lying peaty land, sometimes previously worn-down by men digging peat for fuel, to enlarge or expand by flooding, thus eroding the lake shores, and potentially causing harm to infrastructure, or death. The term waterwolf is an example of zoomorphism, in which a non-living thing is given traits or characteristics of an animal. The traits of a wolf most commonly given to lakes include “something to be feared”, “quick and relentless”,” an enemy of man”.
Peat swamp forests are tropical moist forests where waterlogged soil prevents dead leaves and wood from fully decomposing. Over time, this creates a thick layer of acidic peat. Large areas of these forests are being logged at high rates.
De Groote Peel National Park is a national park in the De Peel, a region in the southeast of the Netherlands on the border between the provinces of Limburg and North Brabant. It has a size of 13.4 km² and preserves a peat bog that has remained partly untouched by peat cutting, which used to be extensive in the area.
Flood control is an important issue for the Netherlands, as due to its low elevation, approximately two thirds of its area is vulnerable to flooding, while the country is densely populated. Natural sand dunes and constructed dikes, dams, and floodgates provide defense against storm surges from the sea. River dikes prevent flooding from water flowing into the country by the major rivers Rhine and Meuse, while a complicated system of drainage ditches, canals, and pumping stations keep the low-lying parts dry for habitation and agriculture. Water control boards are the independent local government bodies responsible for maintaining this system.
The Borneo peat swamp forests ecoregion, within the tropical and subtropical moist broadleaf forests biome, are on the island of Borneo, which is divided between Brunei, Indonesia and Malaysia.
Kaatsheuvel is a village in the province of North Brabant, Netherlands situated along highways N261 and N628. With a population of roughly 16,600, it is the largest village in and the capital of the municipality of Loon op Zand, which also consists of the villages of De Moer and Loon op Zand.
The Vechtstreek is a region in the Dutch provinces of Utrecht and North Holland along the Vecht River between the towns of Utrecht and Amsterdam. Located in the economic heartland of the Netherlands, it is known for its natural environment and history. The Vechtstreek is known for its many vestiges of the Dutch Golden Age, including castles, homes, parks and tea houses. They bear witness to the greatness and wealth of that period, the important commercial role played by the Vecht River and the area's history as a residential area for the nobility and wealthy.
Someren-Eind is a small town, located in the southeast of North Brabant, Netherlands. It is a part of the gemeente Someren, counting 3510 residents by 2007. Someren-Eind is located near the Zuid-Willemsvaart, a canal that connects 's-Hertogenbosch and Maastricht. Someren-Eind is also known under the name D'end.
Negara River is a river of Borneo, Indonesia. It flows in the southeast region of the island, within the Negara District, province of South Kalimantan. It is the second longest river in the province after the Barito River, which Negara River flows into.
A mire, peatland, or quagmire is a wetland area dominated by living peat-forming plants. Mires arise because of incomplete decomposition of organic matter, usually litter from vegetation, due to water-logging and subsequent anoxia. All types of mires share the common characteristic of being saturated with water, at least seasonally with actively forming peat, while having their own ecosystem. Like coral reefs, mires are unusual landforms that derive mostly from biological rather than physical processes, and can take on characteristic shapes and surface patterning.
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![A peat lake near Griendtsveen [nl] Netherlands Peel lake.jpg](http://upload.wikimedia.org/wikipedia/commons/thumb/f/f8/Netherlands_Peel_lake.jpg/220px-Netherlands_Peel_lake.jpg)
