Lone (river)
The Lone is a river in Baden-Württemberg, Germany. It flows into the Hürbe river, a tributary of the Brenz, which in turn discharges into the Danube. Course The Lone rises from a Karst spring with a large discharge near Urpsring, in the municipality of Lonsee, Baden-Württemberg. It flows southeast and then turns northeast. After around 37 km it flows into the Hürbe, which in turn is a tributary of the Brenz. The valley of the Lone is fairly shallow, with rises of only around 50 m on both sides. The valley's width is up to 200 m. The flat valley floor is covered by meadows and fields, the slopes of reef limestone are mostly wooded. The karst on the slopes contains various caves and protuberances which were repeatedly visited by prehistoric hunter/gatherer groups as long ago as the Paleolithic and post-Ice Age Mesolithic. Among these are the Bocksteinhöhle, Hohlenstein-Stadel and Vogelherd Cave, locations of important pre-historic findings. See also *List of river ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Lonsee
Lonsee is a town in the Alb-Donau district in Baden-Württemberg in Germany. The population of Lonsee in 2019 is 5010; the town consists of 7 villages – Ettlenschieß, Halzhausen, Lonsee, Luizhausen, Radelstetten, Sinabronn, and Urspring. The village has a town hall, two railway stations on the Fils Valley Railway, and two schools. Various clubs and groups provide for an active social life. Lonsee was first mentioned in the year 888, but the remains of a Roman fort in nearby Urspring tell of an even older history. Lonsee has been twinned with the English town of Kingskerswell Kingskerswell (formerly Kings Carswell, or Kings Kerswell) is a village and civil parish within Teignbridge local government district in the south of Devon, England. The village grew up where an ancient track took the narrowest point across a ... since 1989. References Alb-Donau-Kreis Württemberg {{AlbDonau-geo-stub ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Hürbe
Hürbe is a 7 km long river of Baden-Württemberg, Germany. It flows into the Brenz near Hermaringen. See also *List of rivers of Baden-Württemberg A list of rivers of Baden-Württemberg, Germany: A * Aal * Aalbach *Aalenbach * Ablach * Ach * Acher *Adelbach * Aich * Aid * Aischbach, tributary of the Kinzig * Aischbach, tributary of the Körsch * Aitrach, tributary of the Danube * Aitrach, ... References Rivers of Baden-Württemberg Rivers of Germany {{BadenWürttemberg-river-stub ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Germany
Germany, officially the Federal Republic of Germany (FRG),, is a country in Central Europe. It is the most populous member state of the European Union. Germany lies between the Baltic and North Sea to the north and the Alps to the south. Its 16 constituent states have a total population of over 84 million in an area of . It borders Denmark to the north, Poland and Czechia to the east, Austria and Switzerland to the south, and France, Luxembourg, Belgium, and the Netherlands to the west. The nation's capital and most populous city is Berlin and its main financial centre is Frankfurt; the largest urban area is the Ruhr. Settlement in what is now Germany began in the Lower Paleolithic, with various tribes inhabiting it from the Neolithic onward, chiefly the Celts. Various Germanic tribes have inhabited the northern parts of modern Germany since classical antiquity. A region named Germania was documented before AD 100. In 962, the Kingdom of Germany formed the ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Baden-Württemberg
Baden-Württemberg (; ), commonly shortened to BW or BaWü, is a German state () in Southwest Germany, east of the Rhine, which forms the southern part of Germany's western border with France. With more than 11.07 million inhabitants across a total area of nearly , it is the third-largest German state by both area (behind Bavaria and Lower Saxony) and population (behind North Rhine-Westphalia and Bavaria). As a federated state, Baden-Württemberg is a partly-sovereign parliamentary republic. The largest city in Baden-Württemberg is the state capital of Stuttgart, followed by Mannheim and Karlsruhe. Other major cities are Freiburg im Breisgau, Heidelberg, Heilbronn, Pforzheim, Reutlingen, Tübingen, and Ulm. What is now Baden-Württemberg was formerly the historical territories of Baden, Prussian Hohenzollern, and Württemberg. Baden-Württemberg became a state of West Germany in April 1952 by the merger of Württemberg-Baden, South Baden, and Württemberg-Hohe ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Brenz (river)
The Brenz () is a river in Baden-Württemberg and Bavaria, Germany. It is a left tributary of the Danube. Its source is at a spring in the town of Königsbronn and it flows for 52 kilometers before meeting the Danube at Lauingen, a few kilometers west of Dillingen. It flows through the towns of Königsbronn, Heidenheim an der Brenz, Giengen and Lauingen. See also *List of rivers of Baden-Württemberg *List of rivers of Bavaria A list of rivers of Bavaria, Germany: A * Aalbach * Abens * Ach *Afferbach * Affinger Bach *Ailsbach * Aisch * Aiterach * Alpbach * Alster * Altmühl * Alz * Amper *Anlauter *Arbach * Arbachgraben *Aschaff * Aschbach * Attel * Aubach, tributary o ... References Rivers of Baden-Württemberg Rivers of Bavaria Rivers of Germany {{BadenWürttemberg-river-stub ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Danube
The Danube ( ; ) is a river that was once a long-standing frontier of the Roman Empire and today connects 10 European countries, running through their territories or being a border. Originating in Germany, the Danube flows southeast for , passing through or bordering Austria, Slovakia, Hungary, Croatia, Serbia, Romania, Bulgaria, Moldova, and Ukraine before draining into the Black Sea. Its drainage basin extends into nine more countries. The largest cities on the river are Vienna, Budapest, Belgrade and Bratislava, all of which are the capitals of their respective countries; the Danube passes through four capital cities, more than any other river in the world. Five more capital cities lie in the Danube's basin: Bucharest, Sofia, Zagreb, Ljubljana and Sarajevo. The fourth-largest city in its basin is Munich, the capital of Bavaria, standing on the Isar River. The Danube is the second-longest river in Europe, after the Volga in Russia. It flows through much of C ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Karst Spring
A karst spring or karstic spring is a spring (outflow of groundwater) that is part of a karst hydrological system. Description Because of their often conical or inverted bowl shape, karst springs are also known in German-speaking lands as a ''Topf'' ("pot") which is reflected in names such as Aachtopf (the source of the Radolfzeller Aach) or Blautopf (the source of the Blau river in Blaubeuren). Karst springs often have a very high yield or discharge rate, because they are often fed by underground drainage from a large catchment basin. Because the springs are usually the terminus of a cave drainage system at the place where a river cave reaches the Earth's surface, it is often possible to enter the caves from karst springs for exploration. Large karst springs are located in many parts of the world; the largest ones are believed to be in Papua New Guinea, with others located in Mediterranean countries such as Bosnia and Herzegovina, Croatia, Turkey, Slovenia, and Italy. ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Karst
Karst is a topography formed from the dissolution of soluble rocks such as limestone, dolomite, and gypsum. It is characterized by underground drainage systems with sinkholes and caves. It has also been documented for more weathering-resistant rocks, such as quartzite, given the right conditions. Subterranean drainage may limit surface water, with few to no rivers or lakes. However, in regions where the dissolved bedrock is covered (perhaps by debris) or confined by one or more superimposed non-soluble rock strata, distinctive karst features may occur only at subsurface levels and can be totally missing above ground. The study of ''paleokarst'' (buried karst in the stratigraphic column) is important in petroleum geology because as much as 50% of the world's hydrocarbon reserves are hosted in carbonate rock, and much of this is found in porous karst systems. Etymology The English word ''karst'' was borrowed from German in the late 19th century, which entered German ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Paleolithic
The Paleolithic or Palaeolithic (), also called the Old Stone Age (from Greek: παλαιός '' palaios'', "old" and λίθος ''lithos'', "stone"), is a period in human prehistory that is distinguished by the original development of stone tools, and which represents almost the entire period of human prehistoric technology. It extends from the earliest known use of stone tools by hominins, 3.3 million years ago, to the end of the Pleistocene, 11,650 cal BP. The Paleolithic Age in Europe preceded the Mesolithic Age, although the date of the transition varies geographically by several thousand years. During the Paleolithic Age, hominins grouped together in small societies such as bands and subsisted by gathering plants, fishing, and hunting or scavenging wild animals. The Paleolithic Age is characterized by the use of knapped stone tools, although at the time humans also used wood and bone tools. Other organic commodities were adapted for use as tools, i ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Mesolithic
The Mesolithic (Greek: μέσος, ''mesos'' 'middle' + λίθος, ''lithos'' 'stone') or Middle Stone Age is the Old World archaeological period between the Upper Paleolithic and the Neolithic. The term Epipaleolithic is often used synonymously, especially for outside northern Europe, and for the corresponding period in the Levant and Caucasus. The Mesolithic has different time spans in different parts of Eurasia. It refers to the final period of hunter-gatherer cultures in Europe and Western Asia, between the end of the Last Glacial Maximum and the Neolithic Revolution. In Europe it spans roughly 15,000 to 5,000 BP; in Southwest Asia (the Epipalaeolithic Near East) roughly 20,000 to 10,000 BP. The term is less used of areas farther east, and not at all beyond Eurasia and North Africa. The type of culture associated with the Mesolithic varies between areas, but it is associated with a decline in the group hunting of large animals in favour of a broader hunt ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Hohlenstein-Stadel
Hohlenstein-Stadel is a cave located in the Hohlenstein cliff (not to be confused with the Hohle Fels) at the southern rim of the Lonetal (valley of the Lone) in the Swabian Jura in Germany. While first excavations were started after the second half of the 19th century, the significance of some of the findings was not realized until 1969. The most significant finding was a small ivory statue called the ''Löwenmensch'', which is one of the oldest pieces of figurative art ever found. The name of the cliff is derived from a combination of Hohlenstein meaning "hollow rock" and Stadel meaning "barn". The Hohlenstein cliffs are made of limestone which was hollowed out by natural causes to create caves. The Stadel is one of three caves in the area that are of important paleontological and archaeological significance. The other two are (the small barn) and the (Bears' Cave). In 2017 the site became part of the UNESCO World Heritage Site Caves and Ice Age Art in the Swabian Jura. Ex ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |