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Pelm
Pelm is an ''Ortsgemeinde'' – a municipality belonging to a ''Verbandsgemeinde'', a kind of collective municipality – in the Vulkaneifel district in Rhineland-Palatinate, Germany. It belongs to the ''Verbandsgemeinde'' of Gerolstein, whose seat is in the like-named town. Geography Location The municipality lies on the river Kyll in the Vulkaneifel, a part of the Eifel known for its volcanic history, geographical and geological features, and even ongoing activity today, including gases that sometimes well up from the earth. Neighbouring municipalities Pelm's neighbours are Gerolstein, Rockeskyll, Berlingen, Dohm-Lammersdorf and Hohenfels-Essingen. History Pelm is notable for its connection with ancient history. Unearthed to the west of the village was a Gallo-Roman sanctuary. It had already been widely destroyed by graverobbers by the time a systematic investigation was done in 1928. More recently, newer information was brought to light by a dig undertaken in 198 ...
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Gerolstein
Gerolstein () is a town in the Vulkaneifel district of Rhineland-Palatinate, Germany. Gerolstein is a local municipality of the ''Verbandsgemeinde Gerolstein''. It has been approved as a '' Luftkurort'' (spa town). History As early as the Stone Age, there is evidence of human habitation in the ''Buchenloch'', a nearby cave. In the Bronze Age the Dietzenley was used by the Celts as a refuge castle. In Roman times a temple and dwellings were known to have existed, and remnants of them have been preserved. One form of the name Gerolstein first appeared in connection with the building of the Löwenburg in 1115, which was then named the ''Burg Gerhardstein''. Town rights were granted to Gerolstein in 1336. In 1691, the town was almost completely destroyed when it was liberated from French occupation by troops from the Duchy of Jülich. After reconstruction, a devastating fire burnt down the town in 1708, and again in 1784. In the 1801 Treaty of Lunéville, Gerolstein, along with ...
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Gerolstein Kasselburg Axb01
Gerolstein () is a town in the Vulkaneifel district of Rhineland-Palatinate, Germany. Gerolstein is a local municipality of the ''Verbandsgemeinde Gerolstein''. It has been approved as a ''Luftkurort'' (spa town). History As early as the Stone Age, there is evidence of human habitation in the ''Buchenloch'', a nearby cave. In the Bronze Age the Dietzenley was used by the Celts as a refuge castle. In Roman times a temple and dwellings were known to have existed, and remnants of them have been preserved. One form of the name Gerolstein first appeared in connection with the building of the Löwenburg in 1115, which was then named the ''Burg Gerhardstein''. Town rights were granted to Gerolstein in 1336. In 1691, the town was almost completely destroyed when it was liberated from French occupation by troops from the Duchy of Jülich. After reconstruction, a devastating fire burnt down the town in 1708, and again in 1784. In the 1801 Treaty of Lunéville, Gerolstein, along with al ...
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Rockeskyll
Rockeskyll is an ''Ortsgemeinde'' – a municipality belonging to a ''Verbandsgemeinde'', a kind of collective municipality – in the Vulkaneifel district in Rhineland-Palatinate, Germany. It belongs to the ''Verbandsgemeinde'' of Gerolstein, whose seat is in the like-named town. Geography The municipality lies in the Vulkaneifel, a part of the Eifel known for its volcanic history, geographical and geological features, and even ongoing activity today, including gases that sometimes well up from the earth. The municipality’s landmark is the Rockeskyller Kopf, a stratovolcano in the heart of the Vulkaneifel, which stretches from the Belgian border to the Moselle. Southwest of Rockeskyll flows the river Kyll, a tributary to the Moselle and the longest river in the Eifel. History In 1098, ''Kila'' had its first documentary mention in a donation document. In 1511, a Gothic church with columnar supports was built. This church is a highly ranked cultural monument and stands as ...
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Vulkaneifel
Vulkaneifel () is a district (''Kreis'') in the northwest of the state Rhineland-Palatinate, Germany. It is the least densely populated district in the state and the fourth most sparsely populated district in Germany. The administrative centre of the district is in Daun. Neighboring districts are Euskirchen (North Rhine-Westphalia), Ahrweiler, Mayen-Koblenz, Cochem-Zell, Bernkastel-Wittlich, and Bitburg-Prüm. Location The county of Vulkaneifel lies in the western part of the eponymous region which lies at heights between 150 and 700 metres above sea level. As a result of former volcanism numerous mineral springs (''Sauerbrunnen'') have formed. The Kyll flows through the county from north to south. The German Wildlife Route and the German Volcano Route also cross the county as does the Eifelsteig hiking trail. History The district was created in 1815 when the Eifel became part of Prussia. As most of the local industries had their traditional markets in France, the distri ...
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Berlingen, Germany
Berlingen is an ''Ortsgemeinde'' – a municipality belonging to a ''Verbandsgemeinde'', a kind of collective municipality – in the Vulkaneifel district in Rhineland-Palatinate, Germany. It belongs to the ''Verbandsgemeinde'' of Gerolstein, whose seat is in the like-named town. Geography Location The municipality lies in the Vulkaneifel, a part of the Eifel known for its volcanic history, geographical and geological features, and even ongoing activity today, including gases that sometimes well up from the earth. Neighbouring municipalities Berlingen’s neighbours are Kirchweiler and Pelm. History In 1201, Berlingen had its first documentary mention. Politics Municipal council The council is made up of 6 council members, who were elected by majority vote at the municipal election held on 7 June 2009, and the honorary mayor as chairman. Coat of arms The German blazon reads: ''In Silber eine eingeschobene rote Spitze, darin über einer erniedrigten silbernen ...
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Gerolstein (Verbandsgemeinde)
Gerolstein is a ''Verbandsgemeinde'' ("collective municipality") in the district Vulkaneifel, in Rhineland-Palatinate, Germany. The seat of the ''Verbandsgemeinde'' is in Gerolstein. On 1 January 2019 it was expanded with the municipalities of the former ''Verbandsgemeinden'' Hillesheim and Obere Kyll. The ''Verbandsgemeinde'' Gerolstein consists of the following ''Ortsgemeinden'' ("local municipalities"): # Basberg # Berlingen # Berndorf #Birgel #Birresborn #Densborn # Dohm-Lammersdorf #Duppach # Esch # Feusdorf #Gerolstein #Gönnersdorf #Hallschlag #Hillesheim #Hohenfels-Essingen #Jünkerath # Kalenborn-Scheuern #Kerpen #Kerschenbach # Kopp #Lissendorf # Mürlenbach # Neroth #Nohn # Oberbettingen # Oberehe-Stroheich #Ormont #Pelm # Reuth #Rockeskyll #Salm #Scheid #Schüller #Stadtkyll #Steffeln # Üxheim # Walsdorf #Wiesbaum Wiesbaum is an '' Ortsgemeinde'' – a municipality belonging to a ''Verbandsgemeinde'', a kind of collective municipality †...
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Rheinisches Landesmuseum Trier
The ''Rheinische Landesmuseum Trier'' is an archaeological museum in Trier, Germany. The collection stretches from prehistory through the Roman period, the Middle Ages to the Baroque era with a strong emphasis on the Roman past of Augusta Treverorum, Germany's oldest city. Its collections of (local) Roman sculptures, Roman mosaics and frescos are among the best in Germany (along with those of the Römisch-Germanisches Museum in Cologne, the Rheinisches Landesmuseum Bonn and the Römisch-Germanisches Zentralmuseum in Mainz). History The museum was founded in 1877 as the Provincial Museum of the Prussian Rhine Province (''Provinzialmuseum der preußischen Rheinprovinz''), of which the Rheinisches Landesmuseum Bonn was also part. The first director was the archaeologist Felix Hettner (1877–1902). In 1885–89 a proper museum building was built at the edge of the palace garden of the Electoral Palace, just outside the Roman wall. The architect of the building, rectangular and ...
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Limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limes ...
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Cella
A cella (from Latin for small chamber) or naos (from the Ancient Greek, Greek ναός, "temple") is the inner chamber of an ancient Greek temple, Greek or Roman temple in classical antiquity. Its enclosure within walls has given rise to extended meanings, of a Monastery, hermit's or monk's cell, and since the 17th century, of a Cell (biology), biological cell in plants or animals. Greek and Roman temples In ancient Greek temple, Greek and Roman temples the cella was a room at the center of the building, usually containing a cult image or statue representing the particular deity venerated in the temple. In addition, the cella may contain a table to receive supplementary votive offerings such as votive statues of associated deities, precious and semi-precious stones, helmets, spear and arrow heads, swords, and war trophy, war trophies. No gatherings or sacrifices took place in the cella as the altar for sacrifices was always located outside the building along the axis and tempora ...
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Sestertius
The ''sestertius'' (plural ''sestertii''), or sesterce (plural sesterces), was an Ancient Rome, ancient Roman Roman currency, coin. During the Roman Republic it was a small, silver coin issued only on rare occasions. During the Roman Empire it was a large brass coin. The name ''sestertius'' means "two and one half", referring to its nominal value of two and a half ''as (Roman coin), asses'' (a bronze Roman coin, singular ''as''), a value that was useful for commerce because it was one quarter of a denarius, a coin worth ten ''asses''. The name is derived from ''semis'', "half" and "tertius", "third", in which "third" refers to the third ''as'': the sestertius was worth two full ''asses'' and half of a third. English-language sources routinely use the original Latin form ''sestertius'', plural ''sestertii''; but older literature frequently uses ''sesterce'', plural ''sesterces'', ''terce'' being the English equivalent of ''tertius''. A modern shorthand for values in sestertii i ...
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Hercules
Hercules (, ) is the Roman equivalent of the Greek divine hero Heracles, son of Jupiter and the mortal Alcmena. In classical mythology, Hercules is famous for his strength and for his numerous far-ranging adventures. The Romans adapted the Greek hero's iconography and myths for their literature and art under the name ''Hercules''. In later Western art and literature and in popular culture, ''Hercules'' is more commonly used than ''Heracles'' as the name of the hero. Hercules is a multifaceted figure with contradictory characteristics, which enabled later artists and writers to pick and choose how to represent him. This article provides an introduction to representations of Hercules in the later tradition. Mythology Birth and early life In Roman mythology, although Hercules was seen as the champion of the weak and a great protector, his personal problems started at birth. Juno sent two witches to prevent the birth, but they were tricked by one of Alcmene's servants and sent ...
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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 ...
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