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Dirmstein
Dirmstein ( pfl, Dermschdää) is an ''Ortsgemeinde'' – a municipality belonging to a ''Verbandsgemeinde'', a kind of collective municipality – in the Bad Dürkheim district in Rhineland-Palatinate, Germany. With its roughly 3,000 inhabitants, it is the third largest ''Ortsgemeinde'' in the ''Verbandsgemeinde'' of Leiningerland, whose seat is in Grünstadt, although that town is itself not in the ''Verbandsgemeinde''. Dirmstein lies in the outermost northeast of the district and the northwest of the Rhine-Neckar urban agglomeration. In the 8th century, Dirmstein had its first documentary mention, although this was undated. The first dated documentary mention came in 842. Although it never belonged to the Counts of Leiningen, it is today counted as part of the ''Leiningerland'', the name used for those noblemen's old domain. The historical and well restored village centre has been raised to a monumental zone by the monument protection authority.Georg Peter Karn, Ulrike Weber: ...
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Heritage Sites In Rhineland-Palatinate
Heritage may refer to: History and society * A heritage asset is a preexisting thing of value today ** Cultural heritage is created by humans ** Natural heritage is not * Heritage language Biology * Heredity, biological inheritance of physical characteristics * Kinship, the relationship between entities that share a genealogical origin Arts and media Music * ''Heritage'' (Earth, Wind & Fire album), 1990 * ''Heritage'' (Eddie Henderson album), 1976 * ''Heritage'' (Opeth album), 2011, and the title song * Heritage Records (England), a British independent record label * Heritage (song), a 1990 song by Earth, Wind & Fire Other uses in arts and media * ''Heritage'' (1935 film), a 1935 Australian film directed by Charles Chauvel * ''Heritage'' (1984 film), a 1984 Slovenian film directed by Matjaž Klopčič * ''Heritage'' (2019 film), a 2019 Cameroonian film by Yolande Welimoum * ''Heritage'' (novel), a ''Doctor Who'' novel Organizations Political parties * Heritage ( ...
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Water Wells
A well is an excavation or structure created in the ground by digging, driving, or drilling to access liquid resources, usually water. The oldest and most common kind of well is a water well, to access groundwater in underground aquifers. The well water is drawn up by a pump, or using containers, such as buckets or large water bags that are raised mechanically or by hand. Water can also be Aquifer storage and recovery, injected back into the aquifer through the well. Wells were first constructed at least eight thousand years ago and historically vary in construction from a simple scoop in the sediment of a dry watercourse to the qanats of Iran, and the stepwells and Sakia, sakiehs of India. Placing a lining in the well shaft helps create stability, and linings of wood or wickerwork date back at least as far as the Iron Age. Wells have traditionally been sunk by hand digging, as is still the case in rural areas of the developing world. These wells are inexpensive and low-tech a ...
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Counts Of Leiningen
The House of Leiningen is the name of an old German noble family whose lands lay principally in Alsace, Lorraine, Saarland, Rhineland, and the Palatinate. Various branches of this family developed over the centuries and ruled counties with Imperial immediacy. Origins The first count of Leiningen about whom anything definite is known was a certain Emich II (d. before 1138). He (and perhaps his father Emich I) built Leiningen Castle, which is now known as "Old Leiningen Castle" (German: ''Burg Altleiningen''), around 1100 to 1110. Nearby Höningen Abbey was built around 1120 as the family's burial place. This family became extinct in the male line when Count Frederick I died about 1220. Frederick I's sister, Liutgarde, married Simon II, Count of Saarbrücken. One of Liutgarde's sons, also named Frederick, inherited the lands of the counts of Leiningen, and he took their arms and their name as Frederick II (d. 1237). He became known as a ''Minnesinger'', and one of his songs w ...
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Cultural Monument
A national heritage site is a heritage site having a value that has been registered by a governmental agency as being of national importance to the cultural heritage or history of that country. Usually such sites are listed in a heritage register that is open to the public, and many are advertised by national visitor bureaus as tourist attractions. Usually such a heritage register list is split by type of feature (natural wonder, ruin, engineering marvel, etc.). In many cases a country may maintain more than one register; there are also registers for entities that span more than one country. History of national heritage listing Each country has its own national heritage list and naming conventions. Sites can be added to a list, and are occasionally removed and even destroyed for economic or other reasons. The concept of protecting and taking pride in cultural heritage is something that goes back to the Seven Wonders of the World, but usually it is only after destruction, espec ...
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Ground Water
Groundwater is the water present beneath Earth's surface in rock and soil pore spaces and in the fractures of rock formations. About 30 percent of all readily available freshwater in the world is groundwater. A unit of rock or an unconsolidated deposit is called an aquifer when it can yield a usable quantity of water. The depth at which soil pore spaces or fractures and voids in rock become completely saturated with water is called the water table. Groundwater is recharged from the surface; it may discharge from the surface naturally at springs and seeps, and can form oases or wetlands. Groundwater is also often withdrawn for agricultural, municipal, and industrial use by constructing and operating extraction wells. The study of the distribution and movement of groundwater is hydrogeology, also called groundwater hydrology. Typically, groundwater is thought of as water flowing through shallow aquifers, but, in the technical sense, it can also contain soil moisture, permafro ...
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Fracture (geology)
A fracture is any separation in a geologic formation, such as a Joint (geology), joint or a Fault (geology), fault that divides the Rock (geology), rock into two or more pieces. A fracture will sometimes form a deep fissure or crevice in the rock. Fractures are commonly caused by Stress (physics), stress exceeding the rock strength, causing the rock to lose cohesion along its weakest plane. Fractures can provide Permeability (fluid), permeability for fluid movement, such as water or hydrocarbons. Highly fractured rocks can make good aquifers or Oil reservoir, hydrocarbon reservoirs, since they may possess both significant Permeability (fluid), permeability and fracture porosity. Brittle deformation Fractures are forms of brittle deformation. There are two types of primary brittle deformation processes. Tensile fracturing results in ''joints''. ''Shear fractures'' are the first initial breaks resulting from shear forces exceeding the cohesive strength in that plane. After those ...
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Palatinate (region)
The Palatinate (german: Pfalz; Palatine German: ''Palz'') is a region of Germany. In the Middle Ages it was known as the Rhenish Palatinate (''Rheinpfalz'') and Lower Palatinate (''Unterpfalz''), which strictly speaking designated only the western part of the Electorate of the Palatinate (''Kurfürstentum Pfalz''), as opposed to the Upper Palatinate (''Oberpfalz''). It occupies roughly the southernmost quarter of the German federal state of Rhineland-Palatinate (''Rheinland-Pfalz''), covering an area of with about 1.4 million inhabitants. Its residents are known as Palatines (''Pfälzer''). Geography The Palatinate borders Saarland in the west, historically also comprising the state's Saarpfalz District. In the northwest, the Hunsrück mountain range forms the border with the Rhineland region. The eastern border with Hesse and the Baden region runs along the Upper Rhine river, while the left bank, with Mainz and Worms as well as the Selz basin around Alzey, belong to th ...
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Upper Rhine Plain
The Upper Rhine Plain, Rhine Rift Valley or Upper Rhine Graben (German: ''Oberrheinische Tiefebene'', ''Oberrheinisches Tiefland'' or ''Oberrheingraben'', French: ''Vallée du Rhin'') is a major rift, about and on average , between Basel in the south and the cities of Frankfurt/Wiesbaden in the north. Its southern section straddles the France–Germany border. It forms part of the European Cenozoic Rift System, which extends across Central Europe. The Upper Rhine Graben formed during the Oligocene, as a response to the evolution of the Alps to the south. It remains active to the present day. Today, the Rhine Rift Valley forms a downfaulted trough through which the river Rhine flows. Formation The Upper Rhine Plain was formed during the Early Cenozoic era, during the Late Eocene epoch. At this time, the Alpine Orogeny, the major mountain building event that was to produce the Alps, was in its early stages. The Alps were formed because the continents of Europe and Africa colli ...
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Water Well
A well is an excavation or structure created in the ground by digging, driving, or drilling to access liquid resources, usually water. The oldest and most common kind of well is a water well, to access groundwater in underground aquifers. The well water is drawn up by a pump, or using containers, such as buckets or large water bags that are raised mechanically or by hand. Water can also be injected back into the aquifer through the well. Wells were first constructed at least eight thousand years ago and historically vary in construction from a simple scoop in the sediment of a dry watercourse to the qanats of Iran, and the stepwells and sakiehs of India. Placing a lining in the well shaft helps create stability, and linings of wood or wickerwork date back at least as far as the Iron Age. Wells have traditionally been sunk by hand digging, as is still the case in rural areas of the developing world. These wells are inexpensive and low-tech as they use mostly manual labour, ...
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