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Ferschweiler Plateau
The Ferschweiler Plateau, which is home to the villages of Ferschweiler and Ernzen among others, is an extensive highland area made from sandstone and is located in the collective municipality of Irrel in the county of Bitburg-Prüm in the German state of Rhineland-Palatinate. From a landscape perspective the Ferschweiler Plateau lies within the South Eifel, a region in the Eifel Mountains. The Ferschweiler Plateau is well known for its many Neolithic (New Stone Age) sites. Important sites include the Fraubillen cross which was originally from the megalithic culture and, according to the missionary, Willibrord, was re-fashioned by hand from a menhir over 4.50 metres high, but is now only 3.50 metres high. Also noteworthy are the Langstein ("Long Stone") and the ''Druidenstein'' ("Druid Rock"). At the back of the plateau is the Devil's Gorge as well as Neolithic and a Gallo-Roman grave field. The Ferschweiler Plateau is an escarpment (like the smaller neighbouring pl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Missionary
A missionary is a member of a Religious denomination, religious group which is sent into an area in order to promote its faith or provide services to people, such as education, literacy, social justice, health care, and economic development.Thomas Hale 'On Being a Missionary' 2003, William Carey Library Pub, . In the Bible translations into Latin, Latin translation of the Bible, Jesus, Jesus Christ says the word when he sends the disciples into areas and commands them to preach the gospel in his name. The term is most commonly used in reference to Christian missions, but it can also be used in reference to any creed or ideology. The word ''mission'' originated in 1598 when Jesuits, the members of the Society of Jesus sent members abroad, derived from the Latin (nominative case, nom. ), meaning 'act of sending' or , meaning 'to send'. By religion Buddhist missions The first Buddhist missionaries were called "Dharma Bhanaks", and some see a missionary charge in the symbolis ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landscapes Of Rhineland-Palatinate
A landscape is the visible features of an area of land, its landforms, and how they integrate with natural or man-made features, often considered in terms of their aesthetic appeal.''New Oxford American Dictionary''. A landscape includes the physical elements of geophysically defined landforms such as (ice-capped) mountains, hills, water bodies such as rivers, lakes, ponds and the sea, living elements of land cover including indigenous vegetation, human elements including different forms of land use, buildings, and structures, and transitory elements such as lighting and weather conditions. Combining both their physical origins and the cultural overlay of human presence, often created over millennia, landscapes reflect a living synthesis of people and place that is vital to local and national identity. The character of a landscape helps define the self-image of the people who inhabit it and a sense of place that differentiates one region from other regions. It is the dynamic b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Keuper
The Keuper is a lithostratigraphic unit (a sequence of rock strata) in the subsurface of large parts of west and central Europe. The Keuper consists of dolomite, shales or claystones and evaporites that were deposited during the Middle and Late Triassic epochs (about ). The Keuper lies on top of the Muschelkalk and under the predominantly Lower Jurassic Lias or other Early Jurassic strata. The Keuper together with the Muschelkalk and the Buntsandstein form the Germanic Trias Group, a characteristic sequence of rock strata that gave the Triassic its name. "Muschelkalk (geology)", Britannica Online Encyclopedia, October 2010, webpage: EB-39 Exposure The Upper Triassic is well exposed in Swabia, Franconia, Alsace and Lorraine and Luxembourg; it extends from Basel on the east side of the Rhine into Hanover, and through England into Scotland and north-east Ireland; it appears flanking the central plateau of France and in the Pyrenees and Sardinia. The Keuper sequence is li ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Upper Triassic
The Late Triassic is the third and final epoch of the Triassic Period in the geologic time scale, spanning the time between Ma and Ma (million years ago). It is preceded by the Middle Triassic Epoch and followed by the Early Jurassic Epoch. The corresponding series of rock beds is known as the Upper Triassic. The Late Triassic is divided into the Carnian, Norian and Rhaetian Ages. Many of the first dinosaurs evolved during the Late Triassic, including ''Plateosaurus'', ''Coelophysis'', and ''Eoraptor''. The Triassic–Jurassic extinction event began during this epoch and is one of the five major mass extinction events of the Earth. Etymology The Triassic was named in 1834 by Friedrich von Alberti, after a succession of three distinct rock layers (Greek meaning 'triad') that are widespread in southern Germany: the lower Buntsandstein (colourful sandstone'')'', the middle Muschelkalk (shell-bearing limestone) and the upper Keuper (coloured clay). The Late Triassic Series co ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jurassic
The Jurassic ( ) is a Geological period, geologic period and System (stratigraphy), stratigraphic system that spanned from the end of the Triassic Period million years ago (Mya) to the beginning of the Cretaceous Period, approximately Mya. The Jurassic constitutes the middle period of the Mesozoic, Mesozoic Era and is named after the Jura Mountains, where limestone strata from the period were first identified. The start of the Jurassic was marked by the major Triassic–Jurassic extinction event, associated with the eruption of the Central Atlantic magmatic province, Central Atlantic Magmatic Province. The beginning of the Toarcian Stage started around 183 million years ago and is marked by an extinction event associated with widespread Anoxic event, oceanic anoxia, ocean acidification, and elevated temperatures likely caused by the eruption of the Karoo-Ferrar, Karoo-Ferrar large igneous provinces. The end of the Jurassic, however, has no clear boundary with the Cretaceous and i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Grave Field
A grave field is a prehistoric cemetery, typically of Bronze Age and Iron Age Europe. Grave fields are distinguished from necropoleis by the former's lack of remaining above-ground structures, buildings, or grave markers. Types Grave fields can be classified by type of burial custom: *tumulus (kurgan) fields *flat graves *row graves: grave fields arranged in rows *ossuaries *shaft tombs *urnfields Celtic grave fields ;Hallstatt culture *Kinding-Ilbling, Eichstätt district, Germany ;La Tène culture *Münsingen-Rain, Berne, Switzerland Northern Europe Scandinavia ;Nordic Bronze Age * Jordbro Grave Field, Jordbro, Sweden *Sammallahdenmäki, Finland * Ekornavallen, Falköping Municipality, Sweden *Gettlinge, Öland, Sweden *Itzehoe tumulus, Germany ;Vendel period *Vendel, Uppland, Sweden *Greby, Bohuslän, Sweden *Smålandsstenar, Gislaved Municipality, Sweden *Trullhalsar, Gotland, Sweden *Blomsholm, Bohuslän, Sweden *Högom, Medelpad, Sweden * Vätteryd, Skåne County, Sweden ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gallo-Roman Culture
Gallo-Roman culture was a consequence of the Romanization of Gauls under the rule of the Roman Empire. It was characterized by the Gaulish adoption or adaptation of Roman culture, language, morals and way of life in a uniquely Gaulish context. The well-studied meld of cultures in Gaul gives historians a model against which to compare and contrast parallel developments of Romanization in other, less-studied Roman provinces. ''Interpretatio romana'' offered Roman names for Gaulish deities such as the smith-god Gobannus, but of Celtic deities only the horse-patroness Epona penetrated Romanized cultures beyond the confines of Gaul. The barbarian invasions beginning in the late third century forced upon Gallo-Roman culture fundamental changes in politics, in the economic underpinning, in military organization. The Gothic settlement of 418 offered a double loyalty, as Western Roman authority disintegrated at Rome. The plight of the highly Romanized governing class is examined by ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Devil's Gorge (Eifel)
The Devil's Gorge or Teufelsschlucht is located on the eastern edge of the Ferschweiler Plateau within the South Eifel Nature Park in the vicinity of Irrel. It was formed towards the end of the last ice age, about 10,000 years ago as the result of one or more rock collapses. The cause of this event was probably a combination of the geological and climatic circumstances. The heavily fissured, more or less porous, rock strata of the so-called Luxembourg Sandstone (geologically part of the Lower Jurassic or German Lias) are laid over keuper beds that tend towards being impervious. As weathering progresses, the structure becomes unstable as a result of the undercutting of the sandstone base. Towards the end of the last glaciation period this undercutting, in combination with extensive frost shattering Frost weathering is a collective term for several mechanical weathering processes induced by stresses created by the freezing of water into ice. The term serves as an umbrella t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Druidenstein
The Druidenstein is a cone-shaped basalt rock in the northern Heller Upland above the town of Kirchen on the Sieg in the parish of Herkersdorf, Altenkirchen, Germany. The basalt cone stands at a height and is about 20 metres high. Formation The Druidenstein is about 25 million years old (Young Tertiary) and covers an area of about 100 m². Its unusual shape was caused when lava forced itself through the Devonian greywacke of the basement and then solidified. As a result, prismatic basalt columns formed at right angles to the cooling surface. By erosion on the hard basalt core has remained, but this continues to shrink. Other processes have also reduced the size of the basalt cone. History The Druidenstein was probably used by the Celts as a religious site and gathering place. The highest tip was probably broken off for tactical reasons during the Thirty Years’ War, so that enemy troops could not orient themselves by it. At that time the tip w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Menhir
A menhir (from Brittonic languages: ''maen'' or ''men'', "stone" and ''hir'' or ''hîr'', "long"), standing stone, orthostat, or lith is a large human-made upright stone, typically dating from the European middle Bronze Age. They can be found individually as monoliths, or as part of a group of similar stones. Menhirs' size can vary considerably, but they often taper toward the top. They are widely distributed across Europe, Africa and Asia, but are most numerous in Western Europe; particularly in Ireland, Great Britain, and Brittany, where there are about 50,000 examples, and northwestern France, where there are some 1,200 further examples. Standing stones are usually difficult to date. They were constructed during many different periods across pre-history as part of the larger megalithic cultures in Europe and near areas. Some menhirs stand next to buildings that have an early or current religious significance. One example is the South Zeal Menhir in Devon, which formed th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Willibrord
Willibrord (; 658 – 7 November AD 739) was an Anglo-Saxon missionary and saint, known as the "Apostle to the Frisians" in the modern Netherlands. He became the first bishop of Utrecht and died at Echternach, Luxembourg. Early life His father, named Wilgils or Hilgis, was styled by Alcuin as a Saxon of Northumbria. Newly converted to Christianity, Wilgils entrusted his son as an oblate to the Abbey of Ripon, and withdrew from the world, constructing a small oratory, near the mouth of the Humber, dedicated to Saint Andrew. The king and nobles of the district endowed him with estates until he was at last able to build a church, over which Alcuin afterwards ruled. Willibrord grew up under the influence of Wilfrid, Bishop of York. Later he joined the Benedictines. He spent the years between the ages of 20 and 32 in the Abbey of Rath Melsigi, in County Carlow, Ireland, which was a centre of European learning in the 7th century. Frisia During this time he studied under Ecgberht of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
