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Uppsalaåsen
Uppsalaåsen is an esker ridge that winds its way across Uppland in Sweden. The ridge disappears and reappears, typically locally named. In the south it begins on southernmost Södertörn and runs north-east, crossing Mälaren via Ekerö and Munsö and reaches the mainland at Bålsta. It then continues across the Uppland landscape and past Uppsala, eventually in the form of Billudden disappearing into the Gävle Bay. The ridge continues on the seafloor and curves northwest, appearing at Sandarna on the Hälsinge coast. The ridge is estimated to be 250 kilometers long, with maximum width about 1 km, and height about 75 m. Names Within Uppsala County the ridge has several names. At its southern extremity at Sunnersta it is called Sunnerstaåsen and is used among other things as a ski slope. Between Ultuna and Ulleråker lies Ultunaåsen.Ultunaåsen http://kartor.uppsala.se/scripts/hsrun.exe/extwebb/dynamiskt2/MapXtreme.htx;start=HS_naturomrade?beteckning=BON007 Nor ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Billudden
Billudden is a nature reserve in Uppsala County, Sweden. Billudden is the outermost part of Uppsalaåsen; here the esker forms a promontory into the sea before disappearing from sight underwater. The nature reserve is characterised by the hilly form of the esker, which is still rising with as much as per century due to post-glacial rebound. Areas of windblown sand and sparse Scots pine woods can also be found in the nature reserve. The nature reserve furthermore contains the largest concentration of common sea buckthorn in Europe and several unusual fungi. There are two nature trails with information about the nature of the reserve intended for the educational use of both grown ups and children in the reserve. There is a former fishing hamlet called Billhamn on the promontory. It lies next to a natural harbour which formed during the last 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 expans ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Uppsala
Uppsala (, or all ending in , ; archaically spelled ''Upsala'') is the county seat of Uppsala County and the List of urban areas in Sweden by population, fourth-largest city in Sweden, after Stockholm, Gothenburg, and Malmö. It had 177,074 inhabitants in 2019. Located north of the capital Stockholm it is also the seat of Uppsala Municipality. Since 1164, Uppsala has been the ecclesiology, ecclesiastical centre of Sweden, being the seat of the Archbishop of Uppsala, Archbishop of the Church of Sweden. Uppsala is home to Scandinavia's largest cathedral – Uppsala Cathedral, which was the frequent site of the coronation of the Swedish monarch until the late 19th century. Uppsala Castle, built by King Gustav I of Sweden, Gustav Vasa, served as one of the royal residences of the Swedish monarchs, and was expanded several times over its history, making Uppsala the secondary capital of Sweden during its Swedish Empire, greatest extent. Today it serves as the residence of the Gover ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Esker
An esker, eskar, eschar, or os, sometimes called an ''asar'', ''osar'', or ''serpent kame'', is a long, winding ridge of stratified sand and gravel, examples of which occur in glaciated and formerly glaciated regions of Europe and North America. Eskers are frequently several kilometres long and, because of their uniform shape, look like railway embankments. Etymology The term ''esker'' is derived from the Irish word ''eiscir'' (Old Irish: ''escir''), which means "ridge or elevation, especially one separating two plains or depressed surfaces". The Irish word was and is used particularly to describe long sinuous ridges, which are now known to be deposits of fluvio-glacial material. The best-known example of such an ''eiscir'' is the '' Eiscir Riada'', which runs nearly the whole width of Ireland from Dublin to Galway, a distance of , and is still closely followed by the main Dublin-Galway road The synonym ''os'' comes from the Swedish word ''ås'', "ridge". Geology Most eske ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sten Sture The Elder
Sten Sture the Elder ( sv, Sten Sture den äldre; 1440 – 14 December 1503) was a Swedish statesman and regent of Sweden from 1470–1497 and 1501–1503. As the leader of the victorious Swedish separatist forces against the royal unionist forces during the Battle of Brunkeberg in 1471, he weakened the Kalmar Union considerably and became the effective ruler of Sweden as Lord Regent for most of his remaining life. Background In contemporary sources he is alternatively referred to as ''Sten Gustavsson'' or ''Herr Sten'' ''(Lord Sten)''; the practice of using noble family names as part of a personal name was not yet in use in Sweden at the time. He was born around 1440, the son of Gustav Anundsson of the Sture family and Birgitta Stensdotter Bielke, half-sister of the future Charles VIII. The Sture family was one of the high-ranking noble families of the time, though only distantly related to the royal house; his closest royal ancestor was King Sverker II of Sweden (both through ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Brunkebergsåsen
Brunkebergsåsen was an esker that once reached over much of Stockholm's Norrmalm district. Geologically, it is a part of the much larger Stockholmsåsen. It formed a considerable obstacle to traffic, effectively dividing Norrmalm into a western and an eastern part. Consequently, most of it has been dug away over the centuries to make room for the development of that district. The pedestrian tunnel Brunkebergstunneln and, since the 1910s, the eastern part of Kungsgatan cut through Brunkebergsåsen's southern part. Conspicuous remnants of the esker can be seen in the vicinity of Johannes kyrka, at Observatorielunden, and Vanadislunden. See also *Battle of Brunkeberg Further reading Essay, with several maps, on the city's development in Stockholm City Museum The Stockholm City Museum ( sv, Stadsmuseet i Stockholm) is a museum documenting, preserving and exhibiting the history of Stockholm. The museum is housed in Södra Stadshuset at Slussen on Södermalm. The building was ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stockholmsåsen
Stockholmsåsen, is a long esker stretching from southern Uppland to northeastern Södermanland, in Stockholm County, Sweden. The esker extends from Arlanda to Jordbro and Västerhaninge, passing through Stockholm where it is known as Brunkebergsåsen. See also * Brunkebergsåsen Brunkebergsåsen was an esker that once reached over much of Stockholm's Norrmalm district. Geologically, it is a part of the much larger Stockholmsåsen. It formed a considerable obstacle to traffic, effectively dividing Norrmalm into a western ... {{DEFAULTSORT:Stockholmsasen Uppland Södermanland Eskers of Sweden ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Post-glacial Rebound
Post-glacial rebound (also called isostatic rebound or crustal rebound) is the rise of land masses after the removal of the huge weight of ice sheets during the last glacial period, which had caused isostatic depression. Post-glacial rebound and isostatic depression are phases of glacial isostasy (glacial isostatic adjustment, glacioisostasy), the deformation of the Earth's crust in response to changes in ice mass distribution. The direct raising effects of post-glacial rebound are readily apparent in parts of Northern Eurasia, Northern America, Patagonia, and Antarctica. However, through the processes of ''ocean siphoning'' and ''continental levering'', the effects of post-glacial rebound on sea level are felt globally far from the locations of current and former ice sheets.Milne, G.A., and J.X. Mitrovica (2008) ''Searching for eustasy in deglacial sea-level histories.'' Quaternary Science Reviews. 27:2292–2302. Overview During the last glacial period, much of northern Eu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shingle Beach
A shingle beach (also referred to as rocky beach or pebble beach) is a beach which is armoured with pebbles or small- to medium-sized cobbles (as opposed to fine sand). Typically, the stone composition may grade from characteristic sizes ranging from diameter. While this beach landform is most commonly found in Europe, examples are found in Bahrain, North America, and a number of other world regions, such as the west coast of New Zealand's South Island, where they are associated with the shingle fans of braided rivers. Though created at shorelines, post-glacial rebound can raise shingle beaches as high as above sea level, as on the High Coast in Sweden. The ecosystems formed by this unique association of rock and sand allow colonization by a variety of rare and endangered species. Formation Shingle beaches are typically steep, because the waves easily flow through the coarse, porous surface of the beach, decreasing the effect of backwash erosion and increasing the formati ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lövstalöt
Lövstalöt is a locality situated in Uppsala Municipality, Uppsala County, Sweden with 1,046 inhabitants in 2010. Lövstalöt is situated 12 km north of the city of Uppsala, in the flat country that surrounds the city. Until the end of the 1930s, the village consisted of a few houses and a school, built in 1892. In 1938, a woodworking factory, ''Bälinge Snickerifabrik'', was built. Most of the houses in Lövstalöt were built during the 1960s and 1980s. Detached houses dominate, but there are also some terraced houses. In the centre of Lövstalöt there is a gravefield from the Iron Age The Iron Age is the final epoch of the three-age division of the prehistory and protohistory of humanity. It was preceded by the Stone Age (Paleolithic, Mesolithic, Neolithic) and the Bronze Age (Chalcolithic). The concept has been mostly appl .... References Populated places in Uppsala County Populated places in Uppsala Municipality {{Uppsala-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ekoln
Ekoln constitutes the northernmost gulf of Lake Mälaren, Sweden. On its northern shore are the southern suburbs of Uppsala and the mouth of River Fyris Fyrisån (, "the Fyris river") is a river in the Swedish province of Uppland, which passes through the city of Uppsala and ends in Lake Mälaren. The "Sala" river in Uppland was changed in the 17th century in memory of the Fyrisvellir battle, m .... In 2019, Ikea named a toilet brush after it. References {{coord, 59, 45, N, 17, 37, E, display=title, region:SE_type:waterbody_source:GNS-enwiki Uppsala Mälaren Landforms of Uppsala County Gulfs of Sweden ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gamla Uppsala
Gamla, alt. sp. Gamala ( he, גַּמְלָא, The Camel) was an ancient Jewish city on the Golan Heights. It is believed to have been founded as a Seleucid fort during the Syrian Wars which was turned into a city under Hasmonean rule in 81 BCE. During the Great Revolt, it became an important stronghold for rebels and because of this Gamla is a symbol for the modern state of Israel and an important historical and archaeological site. It lies within the current Gamla nature reserve and is a prominent tourist attraction. History Situated at the southern part of the Golan, overlooking the Sea of Galilee, Gamla was built on a steep hill shaped like a camel's hump, from which it derives its name (''Gamla'' meaning 'the camel' in Aramaic). Early history Archaeological excavations have shown that in the place of Gamla there was already a settlement in the Early Bronze Age. The settlement was probably agricultural, as archaeologists have found evidence of long-term use of flint s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
