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Hondsrug
image:Hoogstraatje RA.JPG, 300px, The Hoogstraatje in Groningen (province), Groningen, the northernmost hill of the Hondsrug The Hondsrug () is a Dutch ridge of sand that is mainly located in the province Drenthe and partly in the province Groningen (province), Groningen. The spur of the Hondsrug in Groningen has led to the creation of various villages build on artificial dwelling hills: Adorp, Sauwerd, Wetsinge, Winsum, Baflo, Rasquert, Warffum, Usquert, Rottum (Groningen), Rottum. The name "''Hondsrug''" would appear to be taken from the Dutch word for "dog" or "hound" (''hond'') and the word for a "back" or "ridge" (''rug''). However, it is more likely a bastardization of the older name ''Hunze-rug'', coming from the name of the Hunze River, which flows through Drenthe and Groningen. Up until the 19th century the ''Hondsrug'' was also known as the ''Bisschopsrug'', meaning "Bishop's Ridge". The ridge has northwest–southeast orientation, which it shares with some less pronou ...
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Hunze
The Hunze (also Oostermoerse Vaart, Oostermoersche Vaart, Drentsche Diep and Schuyten diep) is a river located in the border area of Drenthe and Groningen, east of the Hondsrug, in the Netherlands. The Hunze used to run through to the Wadden Sea, first at Pieterburen and later at Zoutkamp, via the Lauwerszee. The name means "marsh or mud (stream)". The name of the area, Hunsingo, refers to this river, which originally flowed into the Wadden Sea. Origin The Hunze valley probably formed in the Saale glaciation, Saale Glaciation (the penultimate ice age; 236,000 to 124,000 B.C.) during the last phase of the hif period, when the ice flow of the Glacier, land ice changed direction from northeast-southwest to northwest-southeast. Possibly the cutout was caused by an ice lobe. It was previously thought that this occurred later and that the valley was created by meltwater runoff. However, the presence of Depression (geology), depressions and the steep straight boundary on the west side ...
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Regions Of The Netherlands
The regions of the Netherlands provides links to both regions and subregions of the Netherlands. Regions The regions of the Netherlands are divided into the North, South, West and East Netherlands. Official regions Many regions in the Netherlands are officially defined by certain regulations of organizations. First level NUTS of the European Union First level NUTS of the European Union, NUTS-1 Regional divisions as used by the European Union: * Region NL1 (North Netherlands): Groningen, Friesland, Drenthe * Region NL2 (East Netherlands): Overijssel, Gelderland, Flevoland * Region NL3 (West Netherlands): Utrecht, North Holland, South Holland, Zeeland * Region NL4 (South Netherlands): North Brabant, Limburg Unofficial multi-country regions *De Duffelt *EUREGIO, Euregio Enschede-Gronau *Euregio Benelux Middengebied *Ems Dollart Region *Frisia *Kempen (streek), Kempen *Maasland (Limburg), Maasland *Meuse-Rhine Euroregion *Rhine-Meuse-North Euroregion *Rhine-Waal Euroregion *Sc ...
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King Willem-Alexander Canal
The King Willem-Alexander Canal (), named after King Willem-Alexander of the Netherlands, is a 6 km long canal in the northeastern Netherlands. The new canal through the Hondsrug is part of the larger ''Veenvaart'' project to draw more recreational boaters and tourists to the Veenkoloniën region in the provinces of Drenthe and Groningen Groningen ( , ; ; or ) is the capital city and main municipality of Groningen (province), Groningen province in the Netherlands. Dubbed the "capital of the north", Groningen is the largest place as well as the economic and cultural centre of .... The canal was originally to be called the ''Veenkanaal'' but was renamed on 8 June 2013 in honor of recently enthroned King Willem-Alexander. References {{Reflist Canals in the Netherlands Canals opened in 2013 ...
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Rottum (Groningen)
Rottum (or Röppen) is a small village on an artificial dwelling hill between Kantens and Usquert in the municipality of Het Hogeland, falling under the province Groningen in the Netherlands. It had a population of around 85 in January 2017.Kerncijfers wijken en buurten 2017
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History


Heathen chapel

The village was founded on a clay bank of the Fivel and the . Since high tides were threatening the early inhabitants they raised its height with manu ...
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Regions Of Groningen (province)
In geography, regions, otherwise referred to as areas, zones, lands or territories, are portions of the Earth's surface that are broadly divided by physical characteristics (physical geography), human impact characteristics (human geography), and the interaction of humanity and the environment ( environmental geography). Geographic regions and sub-regions are mostly described by their imprecisely defined, and sometimes transitory boundaries, except in human geography, where jurisdiction areas such as national borders are defined in law. More confined or well bounded portions are called ''locations'' or ''places''. Apart from the global continental regions, there are also hydrospheric and atmospheric regions that cover the oceans, and discrete climates above the land and water masses of the planet. The land and water global regions are divided into subregions geographically bounded by large geological features that influence large-scale ecologies, such as plains and features. As a ...
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Hausruckviertel
The Hausruckviertel is one of the four traditional "quarters" () of the Austrian province of Upper Austria Upper Austria ( ; ; ) is one of the nine States of Austria, states of Austria. Its capital is Linz. Upper Austria borders Germany and the Czech Republic, as well as the other Austrian states of Lower Austria, Styria, and Salzburg (state), Salzbur .... The region is named after a range of hills, the Hausruck. Cities in the Hausruckviertel include Wels, Eferding, Grieskirchen, and Vöcklabruck. Notes References * * Geography of Upper Austria {{UpperAustria-geo-stub ...
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Hunsrück
The Hunsrück () is a long, triangular, pronounced mountain range, upland in Rhineland-Palatinate, Germany. It is bounded by the valleys of the Moselle (river), Moselle-Saar (north-to-west), the Nahe (south), and the Rhine (east). It is continued by the Taunus mountains, past the Rhine and by the Eifel past the Moselle. To the south of the Nahe is a lower, hilly country forming the near bulk of the Palatinate (region), Palatinate region and all of the, smaller, Saarland. Below its north-east corner is Koblenz. As the Hunsrück proceeds east it acquires north-south width and three notable gaps in its southern ridges. In this zone are dendritic drainage, multi-branch headwaters including the Simmerbach ending at Simmertal on the southern edge. This interior is therefore rarely higher than above sea level. Peaks and escarpments are principally: the Schwarzwälder Hochwald, (Black Forest) Hochwald, the Idar Forest, the Soonwald, and the Bingen Forest. The highest mountain is the Erb ...
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Moraines
A moraine is any accumulation of unconsolidated debris ( regolith and rock), sometimes referred to as glacial till, that occurs in both currently and formerly glaciated regions, and that has been previously carried along by a glacier or ice sheet. It may consist of partly rounded particles ranging in size from boulders (in which case it is often referred to as boulder clay) down to gravel and sand, in a groundmass of finely-divided clayey material sometimes called glacial flour. Lateral moraines are those formed at the side of the ice flow, and terminal moraines are those formed at the foot, marking the maximum advance of the glacier. Other types of moraine include ground moraines (till-covered areas forming sheets on flat or irregular topography) and medial moraines (moraines formed where two glaciers meet). Etymology The word ''moraine'' is borrowed from French , which in turn is derived from the Savoyard Italian ('mound of earth'). in this case was derived from Proven ...
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Glacial Landforms
Glacial landforms are landforms created by the action of glaciers. Most of today's glacial landforms were created by the movement of large ice sheets during the Quaternary glaciations. Some areas, like Fennoscandia and the southern Andes, have extensive occurrences of glacial landforms; other areas, such as the Sahara, display rare and very old fossil glacial landforms. Erosional landforms As the glaciers expand, due to their accumulating weight of snow and ice they crush, abrade, ''and'' scour surfaces such as rocks and bedrock. The resulting erosional landforms include striations, cirques, glacial horns, arêtes, trim lines, U-shaped valleys, roches moutonnées, overdeepenings and hanging valleys. * Striations: grooves and indentations in rock outcrops, formed by the scraping of small sediments on the bottom of a glacier across the Earth's surface. The direction of striations display the direction the glacier was moving. * Cirque: Starting location for mountain gl ...
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Usquert
Usquert is a village in the Dutch province of Groningen. It is located in the municipality of Het Hogeland Het Hogeland is a municipality in the north of the province of Groningen (province), Groningen in the northeast of the Netherlands. History The municipality of Het Hogeland was established on 1 January 2019 by merging the municipalities of Bedu .... It had a population of around 1,415 in January 2017. History Usquert was a separate municipality until 1990, when it became part of Hefshuizen. After that, the name of the municipality was changed to Eemsmond in 1992. Image:Usquert.JPG, The church on the wierde File:Oude gemeentehuis Usquert.jpg, Former Usquert town hall File:Raadhuisstraat 5 Usquert.JPG, Villa in Usquert File:Gaykema Heerd Usquert 2.JPG, Farm in Usquert References External links * Het Hogeland Populated places in Groningen (province) Former municipalities of Groningen (province) {{Groningen-geo-stub ...
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