Hadriwa (Bavarian Forest, Zell)
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Hadriwa (Bavarian Forest, Zell)
The Hadriwa is a mountain, 677 m above sea level, in the municipality of Zell in the county of Cham in the German state of Bavaria, and the highest point in the region south of Zell between the Perlenbach and Göppenbach streams. There is another mountain called the Hadriwa in the Bavarian Forest in the county of Straubing-Bogen which is 922 m high. References {{DEFAULTSORT:Hadriwa Zell Mountains under 1000 metres Mountains of Bavaria Mountains of the Bavarian Forest Cham (district) ...
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Bavarian Forest
The village of Zell in the Bavarian Forest The Bavarian Forest (German: ' or ''Bayerwald''; bar, Boarischa Woid) is a wooded, low-mountain region in Bavaria, Germany that is about 100 kilometres long. It runs along the Czech border and is continued on the Czech side by the Bohemian Forest (Czech: ''Šumava''). Most of the Bavarian Forest lies within the province of Lower Bavaria, but the northern part lies within Upper Palatinate. In the south it reaches the border with Upper Austria. Geologically and geomorphologically, the Bavarian Forest is part of the Bohemian Forest - the highest of the truncated highlands of the Bohemian Massif. The area along the Czech border has been designated as the Bavarian Forest National Park (240 km2), established in 1970 as the first national park in Germany. Another 3,008 km2 has been designated as the Bavarian Forest Nature Park, established 1967, and another 1,738 km2 as the Upper Bavarian Forest Nature Park, established in 1 ...
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Cham (district)
Cham () is a Districts of Germany, ''Landkreis'' (district) in Bavaria, Germany. It is bounded by (from the south and clockwise) the districts of Regen (district), Regen, Straubing-Bogen, Regensburg (district), Regensburg and Schwandorf (district), Schwandorf and by the Czech Republic, Czech Plzeň Region. History The first historical date in the regional history is the year 748, when the bishop of Regensburg ordered the foundation of a monastery in the sparsely populated region. About 100 years later, the royal castle of Cham was built and became a summer residence for the Holy Roman Emperors. The region was called ''Campriche'' or ''Mark Cham''. In 1204, the Mark Cham became subject to Bavaria, in 1352 to the Electorate of the Palatinate and in the 17th century back to Bavaria. Nowadays, Cham still enjoys the laid-back lifestyle from the days of yore. Many projects have been initiated to give this area an impetus to grow, yet in spite of this, it is still one of the least-popul ...
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Bavaria
Bavaria ( ; ), officially the Free State of Bavaria (german: Freistaat Bayern, link=no ), is a state in the south-east of Germany. With an area of , Bavaria is the largest German state by land area, comprising roughly a fifth of the total land area of Germany. With over 13 million inhabitants, it is second in population only to North Rhine-Westphalia, but due to its large size its population density is below the German average. Bavaria's main cities are Munich (its capital and largest city and also the third largest city in Germany), Nuremberg, and Augsburg. The history of Bavaria includes its earliest settlement by Iron Age Celtic tribes, followed by the conquests of the Roman Empire in the 1st century BC, when the territory was incorporated into the provinces of Raetia and Noricum. It became the Duchy of Bavaria (a stem duchy) in the 6th century AD following the collapse of the Western Roman Empire. It was later incorporated into the Holy Roman Empire, became an ind ...
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Hadriwa (Bavarian Forest, Haibach)
The Hadriwa ádriwɐis a completely forested mountain, 922 m, near Elisabethszell in the municipality of Haibach in the Bavarian Forest in Germany. It is the highest point on the ridge between the Klinglbach and Grüner Bach in the east and the Elisabethszeller Bach and the Menach and its side streams in the west. According to a survey, the Hadriwa is one of 16 possible top sites for pumped-storage hydroelectric stations in Bavaria. In Straubing-Bogen county, the Pfarrerberg to the south and the Kobelberg near Wiesenfelden are also among the sites deemed suitable for such installations. Until the early 20th century, there was a farmstead near the summit, also called the Hadriwa. Today its traces are still visible in the form of the remains of a building and well-preserved rubble stone walls. The origin of the name is unclear. One possible meaning is based on the Czech word, ''Hadr'', for disagreement, quarrel, strife and the fact that the boundary between the ab ...
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Straubing-Bogen
Straubing-Bogen is a ''Landkreis'' (district) in the eastern part of Bavaria, Germany. Neighboring districts are (from the north clockwise) Cham, Regen, Deggendorf, Dingolfing-Landau, Landshut and Regensburg. The independent town of Straubing is surrounded by the district. The seat of the government of the district ( Landratsamt) is located in Straubing. The only towns within the district itself are Bogen and Geiselhöring. Geography The main river is the Danube, which crosses the district from the west to the east. There are two major geographical regions in the district. One is the Gäuboden with the Danube region and lowlands, the other are the mountains of the Bavarian Forest (''Bayerische Wald''). History The district was created in 1972 by merging the previous districts Straubing and Bogen and parts of the district Mallersdorf. Coat of arms The coat of arms is based on the coat of arms of the former district Straubing. In the bottom are the white-and-blue diamonds as t ...
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Mountains Under 1000 Metres
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 ...
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Mountains Of Bavaria
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 ...
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Mountains Of The Bavarian Forest
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 (topography), 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 Monadnock, isolated summits, but most occur in mountain ranges. Mountain formation, Mountains are formed through Tectonic plate, 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 Slump (geology), slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce Alpine climate, colder climates than at sea level at similar latitude. These colder climates strongly affect the Montane ecosystems, ecosys ...
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