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Kalvarienberg
The Kalvarienberg is a Deutsche Grundkarte 1:5,000 calvary hill in the nature reserve of Lampertstal near Alendorf, a village in the municipality of Blankenheim in the county of Euskirchen in the German state of North Rhine-Westphalia. History Count Salentin Ernest of Manderscheid-Blankenheim (born 1630) realised the idea of an ancestor, who wanted the Alendorf countryside and the (originally so-called) hill of Kelberg to recall the original hill of Calvary in Jerusalem. Between 1663 and 1680 Salentin initially had seven stations of the cross - based on ancient tradition - and a chapel built on the hill. In the 19th century seven more stations were added. The chapel that stood on the site of the present-day cross no longer exists. The stations, some of which had been badly weathered, were restored with the aid of NRW Foundation for Conservation, Local History and Culture. Views From the summit of the Kalvarienberg there is an extensive view over the Eifel region. For example, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Calvary Hill
A calvary, also called calvary hill, Sacred Mount, or Sacred Mountain, is a type of Christian sacred place, built on the slopes of a hill, composed by a set of chapels, usually laid out in the form of a pilgrims' way. It is intended to represent the passion of Jesus Christ and takes its name after Calvary, the hill in Jerusalem where, according to tradition, Jesus was crucified. These function as greatly expanded versions of the Stations of the Cross that are usual in Catholic churches, allowing the devout to follow the progress of the stages of the Passion of Christ along the Via Dolorosa in Jerusalem. Each chapel contains a large image of the scene from the Passion it commemorates, sometimes in sculpture, that may be up to life-size. This kind of shrine was especially popular in the Baroque period when the Holy Land was under Turkish rule and it was difficult to make a pilgrimage to the Mount Calvary in Jerusalem. Calvaries were especially popular with the Franc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eifel
The Eifel (; lb, Äifel, ) is a low mountain range in western Germany and eastern Belgium. It occupies parts of southwestern North Rhine-Westphalia, northwestern Rhineland-Palatinate and the southern area of the German-speaking Community of Belgium. The Eifel is part of the Rhenish Massif; within its northern portions lies the Eifel National Park. Geography Location The Eifel lies between the cities of Aachen to the north, Trier to the south and Koblenz to the east. It descends in the northeast along a line from Aachen via Düren to Bonn into the Lower Rhine Bay. In the east and south it is bounded by the valleys of the Rhine and the Moselle. To the west it transitions in Belgium and Luxembourg into the geologically related Ardennes and the Luxembourg Ösling. In the north it is limited by the Jülich-Zülpicher Börde. Within Germany it lies within the states of Rhineland-Palatinate and North Rhine-Westphalia; in the Benelux the area of Eupen, St. Vith and Luxemb ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ahr Hills
The Ahr HillsElkins, T.H. (1972). ''Germany'' (3rd ed.). London: Chatto & Windus, 1972. . (german: Ahrgebirge or ''Ahreifel'' ) are a range of low mountains and hills up to and long in the Eifel region of Germany, which lie roughly southwest of Bonn on the border between the German states of North Rhine-Westphalia and Rhineland-Palatinate. The forested Ahr Hills have numerous tourist destinations (e. g. Aremberg Castle and the Effelsberg Radio Telescope) and the section of a Roman road with its ancient Eifel Aqueduct. Geography Location The Ahr Hills are part of the Eifel, the bulk of which lies to the south and southwest of it. It lies on the left, i.e. northwestern, bank of the river Ahr, roughly 40 km southwest of Bonn. Sometimes the ridge on the right, southeastern, bank of the Ahr in the area of Altenahr is also counted as part of the Ahr Hills. This small range is bordered by a square enclosed by the Grafschaft and Remagen to the east, by Altenahr to the s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains And Hills Of North Rhine-Westphalia
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Juniper
Junipers are coniferous trees and shrubs in the genus ''Juniperus'' () of the cypress family Cupressaceae. Depending on the taxonomy, between 50 and 67 species of junipers are widely distributed throughout the Northern Hemisphere, from the Arctic, south to tropical Africa, throughout parts of West Asia, western, Central Asia, central and South Asia, southern Asia, east to eastern Tibet in the Old World, and in the mountains of Central America. The highest-known juniper forest occurs at an altitude of in southeastern Tibet and the northern Himalayas, creating one of the highest tree lines on earth. Description Junipers vary in size and shape from tall trees, tall, to columnar or low-spreading shrubs with long, trailing branches. They are evergreen with needle-like and/or scale-like leaves. They can be either monoecious or dioecious. The female Conifer cone, seed cones are very distinctive, with fleshy, fruit-like coalescing scales which fuse together to form Juniper berry, a&n ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Calcareous Grassland
Calcareous grassland (or alkaline grassland) is an ecosystem associated with thin basic soil, such as that on chalk and limestone downland. Plants on calcareous grassland are typically short and hardy, and include grasses and herbs such as clover. Calcareous grassland is an important habitat for insects, particularly butterflies and ants, and is kept at a plagioclimax by grazing animals, usually sheep and sometimes cattle. Rabbits used to play a part but due to the onset of myxomatosis their numbers decreased so dramatically that they no longer have much of a grazing effect. There are large areas of calcareous grassland in northwestern Europe, particularly areas of southern England, such as Salisbury Plain and the North and South Downs. The machair forms a different kind of calcareous grassland, where fertile low-lying plains are formed on ground that is calcium-rich due to shell sand (pulverised sea shells). See also * Alvar * Chalk heath * Edaphic * Gypcrust * Gypsum flora ... [...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] |
Crucifixion Of Christ
The crucifixion and death of Jesus occurred in 1st-century Judea, most likely in AD 30 or AD 33. It is described in the four canonical gospels, referred to in the New Testament epistles, attested to by other ancient sources, and considered an established historical event. There is no consensus among historians on the details. Christopher M. Tuckett in ''The Cambridge companion to Jesus'' edited by Markus N. A. Bockmuehl 2001 Cambridge Univ Press pp. 123–124 In the canonical gospels, Jesus is arrested and tried by the Sanhedrin, and then by Pontius Pilate, who sentences him to flagellation and finally crucifixion by the Roman Empire.''The Cradle, the Cross, and the Crown: An Introduction to the New Testament'' by Andreas J. Köstenberger, L. Scott Kellum 2009 pp. 104–108Evans, Craig A. (2001). ''Jesus and His Contemporaries: Comparative Studies'' p. 316 Jesus was stripped of his clothing and offered vinegar mixed with myrrh or gall (likely posca), to dri ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jesus Christ
Jesus, likely from he, יֵשׁוּעַ, translit=Yēšūaʿ, label=Hebrew/Aramaic ( AD 30 or 33), also referred to as Jesus Christ or Jesus of Nazareth (among other names and titles), was a first-century Jewish preacher and religious leader; he is the central figure of Christianity, the world's largest religion. Most Christians believe he is the incarnation of God the Son and the awaited Messiah (the Christ) prophesied in the Hebrew Bible. Virtually all modern scholars of antiquity agree that Jesus existed historically. Research into the historical Jesus has yielded some uncertainty on the historical reliability of the Gospels and on how closely the Jesus portrayed in the New Testament reflects the historical Jesus, as the only detailed records of Jesus' life are contained in the Gospels. Jesus was a Galilean Jew who was circumcised, was baptized by John the Baptist, began his own ministry and was often referred to as "rabbi". Jesus debated with fellow Jews on ho ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Easter Week
The Octave of Easter is the eight-day period, or octave, that begins on Easter Sunday and ends with the following Sunday. In Christian churches that celebrate it, it marks the beginning of Eastertide. The first seven of these eight days are also collectively known as Easter Week. Days in the octave # Easter Sunday # # # # # # # Second Sunday of Easter (also Divine Mercy Sunday in the Roman Catholic Church) Liturgical celebration Roman Rite Catholicism In the Ordinary Form of the Roman Rite of the Catholic Church, Easter is one of two solemnities with an octave, the other being Christmas. The days of the octave are given the second-highest rank in the calendar (second only to the Paschal Triduum and Easter itself), ranking even above normal solemnities. The paschal sequence '' Victimae paschali laudes'' may be sung before the Gospel reading on each of these days. The Gospel readings for each of middle days within the octave are taken from the various Scriptural acc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fritz Von Wille
Friedrich Gustav August Julius Philipp Rudolf von Wille, known as Fritz (21 April 1860, Weimar - 16 February 1941, Düsseldorf), was a German landscape painter and art professor; associated with the Düsseldorf School. Biography He was born into a Hessian family that had been raised to the nobility in 1780. His father, August von Wille, and his mother Clara, were both painters. From 1879 to 1882, he attended the Kunstakademie Düsseldorf, where he initially studied with Andreas Müller and Heinrich Lauenstein, then took specialized courses from Peter Janssen. At first, he was heavily influenced by his father's works, and was concerned that the two would become confused; signing his paintings with "Jr.". In the late 1880s, he made numerous trips throughout Germany. In 1885 and 1886, he visited the Italian Riviera. His experiences there led to a change in his approach to color, and he came under the influence of Eugen Dücker. In 1886, he also became a member of "Malkasten" ( ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eifelsteig
The Eifelsteig is a long-distance hiking trail in the Eifel, Germany. It leads in 15 stages of from the Aachen district Kornelimünster to Trier and is maintained by the Eifel Club. File:Eifelsteig Kornelimünster.JPG, Kornelimünster monastery, Northern start point of the Eifelsteig File:Nationalpark Eifel.jpg, On the hill "Modenhübel" near Gemünd Gemünd is a municipality in the district of Bitburg-Prüm, in Rhineland-Palatinate, western Germany Germany,, officially the Federal Republic of Germany, is a country in Central Europe. It is the second most populous country in Eu ... File:Lieserpfad_6.JPG, The Lieserpfad is part of the Eifelsteig References ;Citations ;Bibliography * * * * * * * * External links {{Authority control Hiking trails in Rhineland-Palatinate Hiking trails in North Rhine-Westphalia Eifel ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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