|
Westerberg (Lamstedt)
The Westerberg (i.e. western hill) in is a low ridge in Northern Germany in the north of the collective municipality of Börde Lamstedt in the state of Lower Saxony. It is covered with mixed forest and, like the nearby Wingst ridge, it is an end moraine from the Saale glaciation period. Together with the Wingst it forms part of the eastern boundary of Land Hadeln. The ''Georgenhöhe'' ("George's Height") is its highest elevation at . In the middle of the Westerberg woods are ''inter alia'' a megalithic grave or dolmen, the ''Steinofen'' and a "stone garden", a collection of 106 examples of glacial erratics. A nunnery that later moved to Himmelpforten was originally seated on the hill.Georg von Issendorff, ''Kloster und Amt Himmelpforten. Nach Akten und Urkunden dargestellt'', reprint of the edition by "Stader Archiv", 1911/1913, extended by Clemens Förster, Stade and Buxtehude: Krause, 1979, pp. 5seq. No ISBN. The convent owned Westerberg hill with its forest. The erratics ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Northern Germany
Northern Germany (, ) is a linguistic, geographic, socio-cultural and historic region in the northern part of Germany which includes the coastal states of Schleswig-Holstein, Mecklenburg-Vorpommern and Lower Saxony and the two city-states Hamburg and Bremen. It contrasts with Southern Germany, Western Germany, and Eastern Germany. Language Northern Germany generally refers to the ''Sprachraum'' area north of the Uerdingen line, Uerdingen and Benrath line isoglosses, where Low German dialects are spoken. These comprise the West Low German, Low Saxon dialects in the west (including the Westphalian language area up to the Rhineland), the East Low German region along the Baltic Sea, Baltic coast with Western Pomerania, the Altmark and northern Brandenburg, as well as the North Low German dialects. Although from the 19th century onwards, the use of Standard German was strongly promoted especially by the Kingdom of Prussia, Prussian administration, Low German dialects are still prese ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Börde Lamstedt
Börde Lamstedt is a ''Samtgemeinde'' ("collective municipality") in the Cuxhaven (district), district of Cuxhaven, in Lower Saxony, Germany. It is situated approximately 35 km east of Bremerhaven, and 15 km north of Bremervörde. Its seat is in the village Lamstedt. The ''Samtgemeinde'' Börde Lamstedt consists of the following municipalities: # Armstorf # Hollnseth # Lamstedt # Mittelstenahe # Stinstedt References Samtgemeinden in Lower Saxony {{Cuxhaven-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lower Saxony
Lower Saxony is a States of Germany, German state (') in Northern Germany, northwestern Germany. It is the second-largest state by land area, with , and fourth-largest in population (8 million in 2021) among the 16 ' of the Germany, Federal Republic of Germany. In rural areas, Northern Low Saxon and Saterland Frisian language, Saterland Frisian are still spoken, though by declining numbers of people. Lower Saxony borders on (from north and clockwise) the North Sea, the states of Schleswig-Holstein, Hamburg, , Brandenburg, Saxony-Anhalt, Thuringia, Hesse and North Rhine-Westphalia, and the Netherlands. Furthermore, the Bremen (state), state of Bremen forms two enclaves within Lower Saxony, one being the city of Bremen, the other its seaport, Bremerhaven (which is a semi-exclave, as it has a coastline). Lower Saxony thus borders more neighbours than any other single '. The state's largest cities are the state capital Hanover, Braunschweig (Brunswick), Oldenburg (city), Oldenburg, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mixed Forest
Temperate broadleaf and mixed forest is a temperate climate terrestrial habitat type defined by the World Wide Fund for Nature, with broadleaf tree ecoregions, and with conifer and broadleaf tree mixed coniferous forest ecoregions. These forests are richest and most distinctive in central China and eastern North America, with some other globally distinctive ecoregions in the Himalayas, Western and Central Europe, the southern coast of the Black Sea, Australasia, Southwestern South America and the Russian Far East. Ecology The typical structure of these forests includes four layers. * The uppermost layer is the canopy composed of tall mature trees ranging from high. Below the canopy is the three-layered, shade-tolerant understory that is roughly shorter than the canopy. * The top layer of the understory is the sub-canopy composed of smaller mature trees, saplings, and suppressed juvenile canopy layer trees awaiting an opening in the canopy. * Below the sub-canopy is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wingst (ridge)
The Wingst is a ridge, up to 74 metres high, in northern Lower Saxony, Germany. Geography The ridge is located in northeast part of the district of Cuxhaven, just a few kilometres south of the mouth of the River Elbe on the North Sea coast, and west of the lower reaches of the Oste between Cadenberge to the north and Hemmoor to the south. It is surrounded by villages in the borough of Wingst. Some distance to the south-southwest of the Wingst is the lake of Balksee; south of which is the ''Varrel Moor''. Geology and history The Wingst is a small geest ridge, covered by mixed woods, that was formed by an ice age moraine. It is surrounded by flat, divided marsh and bog landscapes, that are sometimes only 1 metre above sea level. Dolmens situated within the Wingst indicate that there were early settlements in the local area. Infrastructure The Wingst may be reached via the B 73 federal highway, that grazes the area to the east, as well as its side roads, and also via ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
End Moraine
A terminal moraine, also called an end moraine, is a type of moraine that forms at the terminal (edge) of a glacier, marking its maximum advance. At this point, debris that has accumulated by plucking and abrasion, has been pushed by the front edge of the ice, is driven no further and instead is deposited in an unsorted pile of sediment. Because the glacier acts very much like a conveyor belt, the longer it stays in one place, the greater the amount of material that will be deposited. The moraine is left as the marking point of the terminal extent of the ice. Formation As a glacier moves along its path, the surrounding area is continuously eroding. Loose rock and pieces of bedrock are constantly being picked up and transported with the glacier. Fine sediment and particles are also incorporated into the glacial ice. The accumulation of these rocks and sediment together form what is called glacial till when deposited. Push moraines are formed when a glacier retreats from a pr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saale Glaciation
The Saale glaciation or Saale Glaciation, sometimes referred to as the Saalian glaciation, Saale cold period (), Saale complex (''Saale-Komplex'') or Saale glacial stage (called the Wolstonian Stage in Britain), covers the middle of the three large glaciations in Northern Europe and the northern parts of Eastern Europe, Central Europe and Western Europe by the Scandinavian Inland Ice Sheet. It follows the Holstein interglacial ( Hoxnian Stage in Britain) and precedes the Eemian interglacial (globally known as the Last Interglacial and the Ipswichian in Britain), spanning from around 400,000 years ago to 130,000 years ago. The Saalian covers multiple glacial cycles punctuated by interglacial periods. In its latter part it is coeval with the global Penultimate Glacial Period. Age and definitions The Saalian succeeded the Holstein interglacial and was followed by the Eemian interglacial (which began around 130,000 years ago) Though the start date of the Saalian was historical ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Land Hadeln
Land Hadeln is a historic landscape and former administrative district in Northern Germany with its seat in Otterndorf on the Lower Elbe, the lower reaches of the River Elbe, in the Elbe-Weser Triangle between the estuaries of the Elbe and Weser. The name goes back to a place named ''Haduloha'' in the Royal Frankish Annals, which must have been in the north of Hohe Lieth moraine range, west of present-day Cuxhaven. Enthusiastic historians of late 19th and early 20th century postulated an Old Saxon '' Gau'' (district) of that name, but there is no evidence for this theory.Hans-Ulrich Hucker: Das Problem von Herrschaft und Freiheit in den Landesgemeinden des Mittelalters im Unterweserraum (Thesis, Münster 1978), available in Staatsarchiv Bremen (n°. 538 U) und in the Library of ''Männer vom Morgenstern'' historical society in Bremerhaven In the Middle Ages, the Land Hadeln was a fairly, but not perfectly, autonomous rural community, applying Saxon Law. Nominally, it bel ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dolmen
A dolmen, () or portal tomb, is a type of single-chamber Megalith#Tombs, megalithic tomb, usually consisting of two or more upright megaliths supporting a large flat horizontal capstone or "table". Most date from the Late Neolithic period (40003000 BCE) and were sometimes covered with earth or smaller stones to form a tumulus (burial mound). Small pad-stones may be wedged between the cap and supporting stones to achieve a level appearance. In many instances, the covering has eroded away, leaving only the stone "skeleton". In Sumba (Indonesia), dolmens are still commonly built (about 100 dolmens each year) for collective graves according to lineage. The traditional village of Wainyapu, Sumba, Wainyapu has some 1,400 dolmens. Etymology Celtic or French The word ''dolmen'' entered archaeology when Théophile Corret de la Tour d'Auvergne used it to describe megalithic tombs in his (1796) using the spelling ''dolmin'' (the current spelling was introduced about a decade later and h ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glacial Erratics
A glacial erratic is a glacially deposited rock (geology), rock differing from the type of country rock (geology), rock native to the area in which it rests. Erratics, which take their name from the Latin word ' ("to wander"), are carried by glacial ice, often over distances of hundreds of kilometres. Erratics can range in size from pebbles to large boulders such as Okotoks Erratic, Big Rock (16,500 metric tons) in Alberta. Geologists identify erratics by studying the rocks surrounding the position of the erratic and the composition of the erratic itself. Erratics are significant because: *They can be transported by glaciers, and are thereby one of a series of indicators which mark the path of prehistoric Glacial motion, glacier movement. Their lithographic origin can be traced to the parent bedrock, allowing for confirmation of the ice flow route. *They can be transported by ice rafting, which allows quantification of the extent of glacial flooding resulting from ice dam failure ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Himmelpforten Convent
Himmelpforten Convent (Low Saxon: ''Klooster Hemelpoorten'', ; ) was founded as a monastery of nuns following the Cistercian Rule during the 13th century in Himmelpforten, in today's Lower Saxony, Germany. During the 16th century, it was converted into use as a Lutheran Damsels' Convent. The Himmelpforten Convent was founded before 1255 and finally dissolved in 1647. The convent complex was built between 1300 and 1330. After 1645 the buildings, including the abbey, increasingly decayed, until they were little by little demolished. The dilapidated abbey was demolished in 1737 and replaced by today's St. Mary's Church which partially covers the foundations of the former abbey. History The convent was founded in the mid-13th century on Westerberg hill in , a location later indicated by St. Andrew's Chapel.Georg von Issendorff, ''Kloster und Amt Himmelpforten. Nach Akten und Urkunden dargestellt'', reprint of the edition by "Stader Archiv", 1911/1913, extended by Clemens Förster, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
