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Osenberge
The Osenberge is a dune region up to high in the district of Oldenburg, Lower Saxony (Germany). Geographical location The rolling dunes of the Osenberge are located in the northwest of the Wildeshausen Geest Nature Park, on average about 14 km (as the crow flies) south of Oldenburg, directly south of Sandkrug and immediately northwest of Sandhatten, both of which lie within the municipality of Hatten. To the west the Osenberge are passed by a section of the River Hunte in a south–north direction; to the northwest lies Wardenburg. The Osenberge are the highest elevations in the region, for example the town of Oldenburg is only about 5 to 7 m above sea level. Its two highest peaks, both high, are the Kistenberg south of Sandkrug and the Gierenberg northwest of Sandhatten. From the latter so-called hill there is a good view of the valley of the Hunte. Within the forested or wooded area of ''Barneführerholz'' the Osenberge are mainly covered by old pines. History ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hatten
Hatten is a municipality in Oldenburg, in Lower Saxony, Germany. It is situated southeast of Oldenburg, on the North-West edge of the Wildeshausen Geest Nature Park. Activities Tourism endeavours emphasise the recreational and sporting opportunities available in the area. This includes, adjoining Kirchhatten, a large recreational centre, with swimming pool, exhibition and other facilities. Many visitors enjoy canoeing on the region's major river, the Hunte. The Hatten Airfield, ''Flugplatz Oldenburg-Hatten'', is suitable for small aircraft. It also comprises a flight training school, and sightseeing flights can be booked there as well. The region is serviced through an extensive public transport system, connecting with regional centres, with regular bus and trainNordWestBahn schedules. These provide access to prominent tourist attractions, which in Sandkrug includes Blacksmith and Printing Museums. Moreover, Sandhatten features the workshop of well-known European artist Martin M ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cladonia Foliacea 1 Osenberge
''Cladonia'' is a genus of moss-like lichens in the family Cladoniaceae. They are the primary food source for reindeer/caribou. ''Cladonia'' species are of economic importance to reindeer-herders, such as the Sami in Scandinavia or the Nenets in Russia. Antibiotic compounds are extracted from some species to create antibiotic cream. The light green species ''Cladonia stellaris'' is used in flower decorations. Although the phylogeny of the genus ''Cladonia'' is still under investigation, two main morphological groups are commonly differentiated by taxonomists: the ''Cladonia'' morpho-type and the ''Cladina'' morpho-type. The ''Cladonia'' morpho-type has many more species, and is generally described as a group of squamulose (grow from squamules), cup-bearing lichens. The ''Cladina'' morpho-types are often referred to as forage lichens, mat-forming lichens, or reindeer lichens (due to their importance as caribou winter forage). ''Cladonia perforata'' ("perforate cladonia") is one ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ice Age
An ice age is a long period of reduction in the temperature of Earth's surface and atmosphere, resulting in the presence or expansion of continental and polar ice sheets and alpine glaciers. Earth's climate alternates between ice ages and greenhouse periods, during which there are no glaciers on the planet. Earth is currently in the Quaternary glaciation. Individual pulses of cold climate within an ice age are termed ''glacial periods'' (or, alternatively, ''glacials, glaciations, glacial stages, stadials, stades'', or colloquially, ''ice ages''), and intermittent warm periods within an ice age are called '' interglacials'' or ''interstadials''. In glaciology, ''ice age'' implies the presence of extensive ice sheets in both northern and southern hemispheres. By this definition, Earth is currently in an interglacial period—the Holocene. The amount of anthropogenic greenhouse gases emitted into Earth's oceans and atmosphere is predicted to prevent the next glacial period for th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Oldenburg (district)
The district of Oldenburg (German: ''Landkreis Oldenburg'', not to be confused with the cities of Oldenburg and Oldenburg in Holstein) is a district in the state of Lower Saxony, Germany. It is bounded by (from the east and clockwise) the districts of Diepholz, Vechta, Cloppenburg and Ammerland, the city of Oldenburg, the district of Wesermarsch and the city of Delmenhorst. History The district of Oldenburg was established in 1933. Until 1988 the administrative seat was in the city of Oldenburg. Since then the capital has been in Wildeshausen. Geography The district is located between the metropolitan areas of Oldenburg and Bremen. The Hunte Hunte is a long river in north-western Germany (Lower Saxony), a left tributary of the Weser. The Hunte rises in the Wiehen Hills. In the North German Plain it flows through lake Dümmer. It flows generally northwards through the towns Bad Es ... River runs through the district from south to north. Coat of arms Towns and municipa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of Lower Saxony
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Medieval
In the history of Europe, the Middle Ages or medieval period lasted approximately from the late 5th to the late 15th centuries, similar to the Post-classical, post-classical period of World history (field), global history. It began with the fall of the Western Roman Empire and transitioned into the Renaissance and the Age of Discovery. The Middle Ages is the middle period of the three traditional divisions of Western history: classical antiquity, the medieval period, and the modern history, modern period. The medieval period is itself subdivided into the Early Middle Ages, Early, High Middle Ages, High, and Late Middle Ages. Population decline, counterurbanisation, the collapse of centralized authority, invasions, and mass migrations of tribes, which had begun in late antiquity, continued into the Early Middle Ages. The large-scale movements of the Migration Period, including various Germanic peoples, formed new kingdoms in what remained of the Western Roman Empire. In the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dwarf (mythology)
A dwarf () is a type of supernatural being in Germanic folklore, including mythology. Accounts of dwarfs vary significantly throughout history however they are commonly, but not exclusively, presented as living in mountains or stones and being skilled craftsmen. In early literary sources, only males are explicitly referred to as dwarfs, although they are described as having sisters and daughters, while both male and female dwarfs feature in later saga literature and folklore. Dwarfs are sometimes described as short, however, scholars have noted that this is neither explicit nor of relevance to their roles in the earliest sources. Dwarfs continue to feature in modern popular culture such as in the works of J.R.R. Tolkien and Terry Pratchett, where they are often, but not exclusively, presented as distinct from elves. Etymology The modern English noun ''dwarf'' descends from ang, dweorg. It has a variety of cognates in other Germanic languages, including non, dvergr and goh, tw ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Legend
A legend is a Folklore genre, genre of folklore that consists of a narrative featuring human actions, believed or perceived, both by teller and listeners, to have taken place in human history. Narratives in this genre may demonstrate human values, and possess certain qualities that give the tale verisimilitude (literature), verisimilitude. Legend, for its active and passive participants may include miracles. Legends may be transformed over time to keep them fresh and vital. Many legends operate within the realm of uncertainty, never being entirely believed by the participants, but also never being resolutely doubted. Legends are sometimes distinguished from myths in that they concern human beings as the main characters rather than gods, and sometimes in that they have some sort of historical basis whereas myths generally do not. The Brothers Grimm defined ''legend'' as "Folklore, folktale historically grounded". A by-product of the "concern with human beings" is the long list o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Weichselian Glaciation
The Weichselian glaciation was the last glacial period and its associated glaciation in northern parts of Europe. In the Alpine region it corresponds to the Würm glaciation. It was characterized by a large ice sheet (the Fenno-Scandian ice sheet) that spread out from the Scandinavian Mountains and extended as far as the east coast of Schleswig-Holstein, northern Poland and Northwest Russia. This glaciation is also known as the Weichselian ice age (german: Weichsel-Eiszeit), Vistulian glaciation, Weichsel or, less commonly, the Weichsel glaciation, Weichselian cold period (''Weichsel-Kaltzeit''), Weichselian glacial (''Weichsel-Glazial''), ''Weichselian Stage'' or, rarely, the Weichselian complex (''Weichsel-Komplex''). In Northern Europe it was the youngest of the glacials of the Pleistocene ice age. The preceding warm period in this region was the Eemian interglacial. The last cold period began about 115,000 years ago and ended 11,700 years ago. Its end corresponds with the end o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pine
A pine is any conifer tree or shrub in the genus ''Pinus'' () of the family Pinaceae. ''Pinus'' is the sole genus in the subfamily Pinoideae. The World Flora Online created by the Royal Botanic Gardens, Kew and Missouri Botanical Garden accepts 187 species names of pines as current, together with more synonyms. The American Conifer Society (ACS) and the Royal Horticultural Society accept 121 species. Pines are commonly found in the Northern Hemisphere. ''Pine'' may also refer to the lumber derived from pine trees; it is one of the more extensively used types of lumber. The pine family is the largest conifer family and there are currently 818 named cultivars (or trinomials) recognized by the ACS. Description Pine trees are evergreen, coniferous resinous trees (or, rarely, shrubs) growing tall, with the majority of species reaching tall. The smallest are Siberian dwarf pine and Potosi pinyon, and the tallest is an tall ponderosa pine located in southern Oregon's Rogue Riv ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sand
Sand is a granular material composed of finely divided mineral particles. Sand has various compositions but is defined by its grain size. Sand grains are smaller than gravel and coarser than silt. Sand can also refer to a textural class of soil or soil type; i.e., a soil containing more than 85 percent sand-sized particles by mass. The composition of sand varies, depending on the local rock sources and conditions, but the most common constituent of sand in inland continental settings and non-tropical coastal settings is silica (silicon dioxide, or SiO2), usually in the form of quartz. Calcium carbonate is the second most common type of sand, for example, aragonite, which has mostly been created, over the past 500million years, by various forms of life, like coral and shellfish. For example, it is the primary form of sand apparent in areas where reefs have dominated the ecosystem for millions of years like the Caribbean. Somewhat more rarely, sand may be composed of calciu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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