|
Osterwald (ridge)
The Osterwald is a ridge (up to ) in the Calenberg Uplands and together with the Nesselberg and the Kleiner Deister forms a unified group of three adjacent ranges in the Leine Uplands. It lies between Coppenbrügge, Eldagsen and Elze in the North German state of Lower Saxony. Geography The Osterwald is located in the Calenberg Uplands north of the Leine Uplands that border on the Calenberg Land there. It lies about halfway between Hamelin in the west and Hildesheim in the east and between the villages of Coppenbrügge in the southwest and Eldagsen in the north and Elze in the east. In terms of natural regions it belongs to the Lower Saxon Hills and borders on the Calenberg Loess Börde in the north and east. The districts of Hildesheim and Hameln-Pyrmont and the region of Hanover meet near the Triangular Rock (''Dreieckiger Stein'') not far from the Shepherd's Hut (''Sennhütte''). On the southern rim of the Osterwald is the eponymous village of Osterwald in the municipality ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landesstraße
''Landesstraßen'' (singular: ''Landesstraße'') are roads in Germany and Austria that are, as a rule, the responsibility of the respective German or Austrian federal state. The term may therefore be translated as "state road". They are roads that cross the boundary of a rural or urban district (''Landkreis'' or ''Kreisfreie Stadt''). A ''Landesstraße'' is thus less important than a ''Bundesstraße'' or federal road, but more significant than a ''Kreisstraße'' or district road. The classification of a road as a ''Landesstraße'' is a legal matter (''Widmung''). In the free states of Bavaria and Saxony – but not, however, in the Free State of Thuringia – ''Landesstraßen'' are known as ''Staatsstraßen''. Designation The abbreviation for a ''Landesstraße'' consists of a prefixed capital letter ''L'' and a serial number (e. g. L 1, L 83, L 262 or L 3190). ''Staatsstraßen'' in Saxony are similarly abbreviated using a capital ''S'' (e. g. S 190) and the ''Staatsstraßen' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions. Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually related to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Middle Ages
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 period of 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 period. The medieval period is itself subdivided into the Early, 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 7th century, North Africa and the Middle East—most recently part of the Eastern Ro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Refuge Castle
A refuge castleCreighton, Oliver (2015). ''Early European Castles''. Bloomsbury. or refuge fort (german: Fliehburg, also ''Fluchtburg'', ''Volksburg'', ''Bauernburg'' or ''Vryburg'') is a castle-like defensive location, usually surrounded by ramparts, that is not permanently occupied but acts as a temporary retreat for the local population when threatened by war or attack. In former times such sites were also described as giant castles (German: ''Hünenburgen'') because their origin was ascribed to giants. History In Europe a multitude of large protohistoric sites surrounded by earthworks has been uncovered by archaeological excavations, many over 100 metres in diameter, that are understood to be refuge castles. Amongst ancient historical references to them are the refuge castles of the Gauls described by Caesar as ''oppida'', although they could also be permanent settlements. Similar ringwork (''Ringwall'') systems were built by the various Germanic and Slavic tribes, th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 applied to Iron Age Europe and the Ancient Near East, but also, by analogy, to other parts of the Old World. The duration of the Iron Age varies depending on the region under consideration. It is defined by archaeological convention. The "Iron Age" begins locally when the production of iron or steel has advanced to the point where iron tools and weapons replace their bronze equivalents in common use. In the Ancient Near East, this transition took place in the wake of the Bronze Age collapse, in the 12th century BC. The technology soon spread throughout the Mediterranean Basin region and to South Asia (Iron Age in India) between the 12th and 11th century BC. Its further spread to Central Asia, Eastern Europe, and Central Europe is somewhat dela ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hillfort
A hillfort is a type of earthwork used as a fortified refuge or defended settlement, located to exploit a rise in elevation for defensive advantage. They are typically European and of the Bronze Age or Iron Age. Some were used in the post-Roman period. The fortification usually follows the contours of a hill and consists of one or more lines of earthworks, with stockades or defensive walls, and external ditches. Hillforts developed in the Late Bronze and Early Iron Age, roughly the start of the first millennium BC, and were used in many Celtic areas of central and western Europe until the Roman conquest. Nomenclature The spellings "hill fort", "hill-fort" and "hillfort" are all used in the archaeological literature. The ''Monument Type Thesaurus'' published by the Forum on Information Standards in Heritage lists ''hillfort'' as the preferred term. They all refer to an elevated site with one or more ramparts made of earth, stone and/or wood, with an external ditch. Many ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Barenburg (Osterwald)
Barenburg is a municipality in the district of Diepholz, in Lower Saxony, Germany Germany,, officially the Federal Republic of Germany, is a country in Central Europe. It is the second most populous country in Europe after Russia, and the most populous member state of the European Union. Germany is situated betwe .... References Diepholz (district) {{Diepholz-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Barenburg Berg
Barenburg is a municipality in the district of Diepholz, in Lower Saxony, Germany Germany,, officially the Federal Republic of Germany, is a country in Central Europe. It is the second most populous country in Europe after Russia, and the most populous member state of the European Union. Germany is situated betwe .... References Diepholz (district) {{Diepholz-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Weser
The Weser () is a river of Lower Saxony in north-west Germany. It begins at Hannoversch Münden through the confluence of the Werra and Fulda. It passes through the Hanseatic city of Bremen. Its mouth is further north against the ports of Bremerhaven and Nordenham. The latter is on the Butjadingen Peninsula. It then merges into the North Sea via two highly saline, estuarine mouths. It connects to the canal network running east-west across the North German Plain. The river, when combined with the Werra (a dialectal form of "Weser"), is long and thus, the longest river entirely situated within Germany (the Main, however, is the longest if the Weser and Werra are not combined). The Weser itself is long. The Werra rises in Thuringia, the German state south of the main projection (tongue) of Lower Saxony. Etymology "Weser" and "Werra" are the same words in different dialects. The difference reflects the old linguistic border between Central and Low German, passing through Ha ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hamel (river)
Hamel (in its lower course: Fluthamel) is a river of Lower Saxony, Germany. It flows into the Weser in Hameln. See also *List of rivers of Lower Saxony All rivers in the German state of Lower Saxony flow directly or indirectly into the North Sea. A–Z A B D E F G H I J K L M N O P * Purrmühlenbach R S T *Tiefenbeek *Trillkebach *Trutenbeek * Twiste U * Uffe *Ulrichswas ... References Rivers of Lower Saxony Rivers of Germany {{LowerSaxony-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saunders_Quarry-1.jpg "Click for more on -> Sandstone")
