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Leiningen Land
The Leiningerland is an historic landscape in the Palatinate region in the German federal state of Rhineland-Palatinate. It is named after an aristocratic family that used to be the most important in the region, the House of Leiningen. Geography The Leiningerland lies in northeast Palatinate, mostly in the county of Bad Dürkheim. Its area coincides with large parts of the collective municipalities of Hettenleidelheim and Grünstadt-Land as well as the town of Grünstadt. Also a part of the historic Leiningerland is the region around the town of Eisenberg, which is in the county of Donnersbergkreis today. Its total area is just under 200 km2. The region does not have a uniform topography, but shares in three geological features: the Central Uplands, the Rhine Rift Valley and the Rhine Plain. the Leiningerland extends from the northeastern foothills of the Palatine Forest in the west across the northern part of the German Wine Road near Grünstadt to Dirmstein ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
German Wine Road
The German Wine RouteScheunemann J., Stewart J., Walker N. and Williams C. (2011), ''Back Roads Germany'', Dorling Kindersley, London. . or Wine Road (german: Deutsche Weinstraße) is the oldest of Germany's tourist wine routes. Located in the Palatinate region of the federal state of Rhineland-Palatinate, the route was established in 1935. Geography The German Wine Gate (''Deutsches Weintor'') in Schweigen-Rechtenbach on the French border adjacent to Wissembourg (Weißenburg) in France marks the start of the route. Built in 1936, the gate is an imposing ceremonial gatehouse made of sandstone. , the route traverses the Palatinate wine region (''Pfalz'', formerly ''Rheinpfalz'') which lies in the lee of the Haardt Mountains, an area known as Anterior Palatinate (''Vorderpfalz''). The route runs northward, beside the path of Bundesstraßen B 38 and B 271 for 85 km, passing through towns like Bad Bergzabern, Edenkoben, Neustadt an der Weinstraße, Deidesheim, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eisbach (Rhine)
The Eisbach, locally known as , is a long river and left or western tributary of the Rhine in the northeastern Palatinate and southeastern Rhenish Hesse, in the German state of Rhineland-Palatinate. Course The largest of the seven springs of the Eisbach is at an elevation of about above sea level on the northern slope of the Hohe Bühl mountain, , in the northern Palatinate Forest, southwest of Ramsen. After about two kilometres, the seven streams unite in the Eiswoog reservoir. At the hamlet of ''Kleehof'', the long Bockbach flows in from the right. Here, the direction of the river changes from straight north to northeast. The direction remains northeast until the confluence with the Rhine. The river then flows past Ramsen and Eisenberg. Below Ebertsheim, it receives the long Seltenbach from the right and a few metres further, its largest tributary, the Rodenbach from the left. At Asselheim, a ward of Grünstadt, the Eisbach reaches the Upper Rhine Valley. It then fl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eckbach (Rhine)
The Eckbach (locally known as the Eck and in the lower reaches also as Neugraben or Leiniger Graben) is a small river in the northeastern Palatinate and the southeastern Rhenish Hesse. It is slightly over long. Name Linguistic Research into the old name of ''die Eck'' shows that it is related to the Upper German word ''Ache'', which means "river" or "creek" and is derived from the Old High German ''aha''. In the Middle Ages, the river was known as ''Leinbach''. This name refers to the ''Leinbaum'', that is, the Lime tree (''Tilia × europaea'' L., not related to the ''Citrus aurantifolia'', the tree that produces the lime (fruit)). In those days, both the Norway Maple (''Acer platanoides'') and the Large-leaved Linden (''Tilia platyphyllos'') were called ''Leinbaum'' in German. Both species were common on the banks of the Eckbach. One difference between the species is the shape of the leaves: maple leaves are five lobed, lime leaves are undivided. The coat of arms of t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rhine
), Surselva, Graubünden, Switzerland , source1_coordinates= , source1_elevation = , source2 = Rein Posteriur/Hinterrhein , source2_location = Paradies Glacier, Graubünden, Switzerland , source2_coordinates= , source2_elevation = , source_confluence = Reichenau , source_confluence_location = Tamins, Graubünden, Switzerland , source_confluence_coordinates= , source_confluence_elevation = , mouth = North Sea , mouth_location = Netherlands , mouth_coordinates = , mouth_elevation = , progression = , river_system = , basin_size = , tributaries_left = , tributaries_right = , custom_label = , custom_data = , extra = The Rhine ; french: Rhin ; nl, Rijn ; wa, Rén ; li, Rien; rm, label= Sursilvan, Rein, rm, label= Sutsilvan and Surmiran, Ragn, rm, label=Rumantsch Grischun, Vallader and Puter, Rain; it, Reno ; gsw, Rhi(n), inclu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tributaries
A tributary, or affluent, is a stream or river that flows into a larger stream or main stem (or parent) river or a lake. A tributary does not flow directly into a sea or ocean. Tributaries and the main stem river drain the surrounding drainage basin of its surface water and groundwater, leading the water out into an ocean. The Irtysh is a chief tributary of the Ob river and is also the longest tributary river in the world with a length of . The Madeira River is the largest tributary river by volume in the world with an average discharge of . A confluence, where two or more bodies of water meet, usually refers to the joining of tributaries. The opposite to a tributary is a distributary, a river or stream that branches off from and flows away from the main stream. PhysicalGeography.net, Michael Pidwirny & Scott ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Orographic
Orography is the study of the topographic relief of mountains, and can more broadly include hills, and any part of a region's elevated terrain. Orography (also known as ''oreography'', ''orology'' or ''oreology'') falls within the broader discipline of geomorphology. The term orography comes from the Greek: , hill, , to write. Uses Mountain ranges and elevated land masses have a major impact on global climate. For instance, the elevated areas of East Africa substantially determine the strength of the Indian monsoon.Srinivasan, J., Nanjundiah, Ravi S. and Chakraborty, Arindam (2005Impact of Orography on the Simulation of Monsoon Climate in a General Circulation Model''Indian Institute of Science'' In scientific models, such as general circulation models, orography defines the lower boundary of the model over land. When a river's tributaries or settlements by the river are listed in 'orographic sequence', they are in order from the highest (nearest the source of the river) to the l ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Biotope
A biotope is an area of uniform environmental conditions providing a living place for a specific assemblage of plants and animals. ''Biotope'' is almost synonymous with the term "habitat", which is more commonly used in English-speaking countries. However, in some countries these two terms are distinguished: the subject of a habitat is a population, the subject of a biotope is a ''biocoenosis'' or "biological community". It is an English loanword derived from the German ''Biotop'', which in turn came from the Greek ''bios'' (meaning 'life') and ''topos'' ('place'). (The related word ''geotope'' has made its way into the English language by the same route, from the German '' Geotop''.) Ecology The concept of a biotope was first advocated by Ernst Haeckel (1834–1919), a German zoologist famous for the recapitulation theory. In his book ''General Morphology'' (1866), which defines the term "ecology", he stresses the importance of the concept of habitat as a prerequisite for an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Natural Monument
A natural monument is a natural or natural/cultural feature of outstanding or unique value because of its inherent rarity, representative of aesthetic qualities or cultural significance. Under World Commission on Protected Areas guidelines, natural monuments are level III, described as: :"Areas are set aside to protect a specific natural monument, which can be a landform, sea mount, submarine cavern, geological feature such as a cave or even a living feature such as an ancient grove. They are generally quite small protected areas and often have high visitor value." This is a lower level of protection than level II (national parks) and level I (wilderness areas). The European Environment Agency's guidelines for selection of a natural monument are: * The area should contain one or more features of outstanding significance. Appropriate natural features include waterfalls, caves, craters, fossil beds, sand dunes and marine features, along with unique or representative fauna and flo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Erosion (geology)
Erosion is the action of surface processes (such as water flow or wind) that removes soil, rock, or dissolved material from one location on the Earth's crust, and then transports it to another location where it is deposited. Erosion is distinct from weathering which involves no movement. Removal of rock or soil as clastic sediment is referred to as ''physical'' or ''mechanical'' erosion; this contrasts with ''chemical'' erosion, where soil or rock material is removed from an area by dissolution. Eroded sediment or solutes may be transported just a few millimetres, or for thousands of kilometres. Agents of erosion include rainfall; bedrock wear in rivers; coastal erosion by the sea and waves; glacial plucking, abrasion, and scour; areal flooding; wind abrasion; groundwater processes; and mass movement processes in steep landscapes like landslides and debris flows. The rates at which such processes act control how fast a surface is eroded. Typically, physical erosion proceed ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Loess
Loess (, ; from german: Löss ) is a clastic, predominantly silt-sized sediment that is formed by the accumulation of wind-blown dust. Ten percent of Earth's land area is covered by loess or similar deposits. Loess is a periglacial or aeolian (windborne) sediment, defined as an accumulation of 20% or less of clay and a balance of roughly equal parts sand and silt (with a typical grain size from 20 to 50 micrometers), often loosely cemented by calcium carbonate. It is usually homogeneous and highly porous and is traversed by vertical capillaries that permit the sediment to fracture and form vertical bluffs. Properties Loess is homogeneous, porous, friable, pale yellow or buff, slightly coherent, typically non- stratified and often calcareous. Loess grains are angular, with little polishing or rounding, and composed of crystals of quartz, feldspar, mica and other minerals. Loess can be described as a rich, dust-like soil. Loess deposits may become very thick, more than ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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