Hahnenkamm (Spessart)
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Hahnenkamm (Spessart)
Hahnenkamm (Spessart) is a ridge of hills in the northwest of the Spessart range of Bavaria, Germany. It has an elevation of up to 435.5 m above NHN. Geography Location Hahnenkamm lies east of Alzenau in the district of Aschaffenburg in the far northwest of the state of Bavaria. It is part of the ''Mittelgebirge'' Spessart (more precisely the ''Vorspessart'') and is located between the ''Kahlgrund'', the valley of the river Kahl, and the ''Untermainsenke'', the valley of the river Main. To the north, the Hahnenkamm is delimited by the river Kahl, to the south by the . Schanzenkopf is part of the Hahnenkamm. Etymology ''Hahnenkamm'' means rooster's comb in German. The name likely derives from the ridge's quite small width (for a ''Mittelgebirge'') and the blocks of quartzite Quartzite is a hard, non- foliated metamorphic rock which was originally pure quartz sandstone.Essentials of Geology, 3rd Edition, Stephen Marshak, p 182 Sandstone is converted into quartzite throug ...
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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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Germany
Germany,, officially the Federal Republic of Germany, is a country in Central Europe. It is the second most populous country in Europe after Russia, and the most populous member state of the European Union. Germany is situated between the Baltic and North seas to the north, and the Alps to the south; it covers an area of , with a population of almost 84 million within its 16 constituent states. Germany borders Denmark to the north, Poland and the Czech Republic to the east, Austria and Switzerland to the south, and France, Luxembourg, Belgium, and the Netherlands to the west. The nation's capital and most populous city is Berlin and its financial centre is Frankfurt; the largest urban area is the Ruhr. Various Germanic tribes have inhabited the northern parts of modern Germany since classical antiquity. A region named Germania was documented before AD 100. In 962, the Kingdom of Germany formed the bulk of the Holy Roman Empire. During the 16th ce ...
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Spessart
Spessart is a ''Mittelgebirge'', a range of low wooded mountains, in the States of Bavaria and Hesse in Germany. It is bordered by the Vogelsberg, Rhön and Odenwald. The highest elevation is the Geiersberg at 586 metres above sea level. Etymology The name is derived from "Spechtshardt". ''Specht'' is the German word for woodpecker and ''Hardt'' is an outdated word meaning "hilly forest". Geography Location The Spessart is a ''Mittelgebirge'', part of the German Central Uplands, located in the Lower Franconia region of Bavaria and in Hesse, Germany. It is bordered by other ranges of hills: the Vogelsberg in the north, Rhön in the northeast and Odenwald in the southwest. Another way of describing the extent of the range is by naming the rivers that border it: the Main in the south and west, the Kinzig in the north and the Sinn in the northeast. The area of the Spessart totals around 2,440 square kilometres, of which 1,710 square kilometres are part of Bavaria. The high ...
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Normalhöhennull
' ("standard elevation zero") or NHN is a vertical datum used in Germany. In geographical terms, NHN is the reference plane for the normal height of a topographical eminence height above mean sea level used in the 1932 German Mean Height Reference System ('). The plane is in the shape of a quasi-geoid. The reference height is a geodetic, fixed point on the New Church of St. Alexander at Wallenhorst in the German state of Lower Saxony. The geopotential height of this point was calculated in 1986 as part of the United European Levelling Network (UELN), based on the Amsterdam Ordnance Datum. Definition The NHN plane is a theoretical reference plane. It is derived by deducting normal heights from the normal plumb line. The difference between the resulting quasi-geoid and the reference ellipsoid is called the height anomaly or quasi-geoid height. Change-over from NN to NHN Since 1 January 2000 the whole of Germany has changed its height system over to normal heights based on ...
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Hahnenkamm
Hahnenkamm (means "comb") may refer to *Hahnenkamm (Verwaltungsgemeinschaft), a federation of municipalities in Bavaria, Germany * Hahnenkamm, Greenland, a mountain in the Stauning Alps, Greenland *Hahnenkamm, Kitzbühel The Hahnenkamm is a mountain in Europe, directly southwest of Kitzbühel in the Kitzbühel Alps of Austria. The elevation of its summit is above sea level. The Hahnenkamm (''German'': rooster's comb) is part of the ski resort of Kitzbühel, a ..., a mountain in Tyrol, Austria * Hahnenkamm, Reutte, another mountain in Tyrol, Austria * Hahnenkamm, Spessart, a mountain in the Spessart, Germany {{disambig, geo ...
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Alzenau
Alzenau (; until 31 December 2006 officially ''Alzenau i.UFr.'') is a town in the north of the Aschaffenburg (district), Aschaffenburg district in the ''Regierungsbezirk'' of Lower Franconia (''Unterfranken'') in Bavaria, Germany. Until 1 July 1972, Alzenau was the district seat of the now abolished district of the same name and has a population of around 19,000. Geography Location Alzenau is one of the eastern outliers of the Frankfurt Rhine Main Region and is crossed by the river Kahl (river), Kahl. Most of its constituent communities nestle on or between the slopes of the western outliers of the Spessart with its Hahnenkamm (Spessart), Hahnenkamm (436 m above Normalhöhennull). The closest hills to the town are Heilberg and Schanzenkopf (Spessart), Schanzenkopf. With roughly 2,600 ha of woodland and 85 ha of vineyards, it has been referred to as ''Stadt im Grünen'' ("Town in the Green"). Alzenau is only a short drive on the Bundesautobahn 45, A 45 or tr ...
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Aschaffenburg (district)
Aschaffenburg (Low Franconian: ''Ascheberg'') is a ''Landkreis'' (district) in Bavaria, Germany. It is bounded by (from the west and clockwise) the districts of Darmstadt-Dieburg, Offenbach, Main-Kinzig (all in the state of Hesse), the districts Main-Spessart and Miltenberg, and the town of Aschaffenburg. History The Aschaffenburg history goes back to as far as the year 957. Initially, being a Roman settlement, it came under the authority of the electors of Mainz in 982 and was chartered in 1173. Remains of Roman settlements were found on the river Main. There was a Roman military camp in what is today the municipality of Stockstadt am Main. After the Roman retreat the region became subject to Alemanni and Franks before eventually being a part of the Electorate of Mainz. While the banks of the Main were populated all these centuries, the hills of the Spessart were virtually unsettled until the 13th century. The districts of Aschaffenburg and Alzenau were established in 186 ...
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Mittelgebirge
A ''Mittelgebirge'' (German: ''Mittel'', "middle/medium"; ''Gebirge'', "mountain range") is a type of relatively low mountain range or highland area typical of the geography of central Europe, especially central and southern Germany; it refers to something between rolling low hill country or ''Hügelland'' and a proper mountain range (german: link=no, Gebirge or ''Hochgebirge'') like the High Alps. Characteristics The term is not precise, but typically refers to topography where the peaks rise at least to ''above the surrounding terrain'' (as opposed to above sea level). The summits usually do not reach the tree line and were not glaciated after the last glacial period. In contrast, ''Hochgebirge'' is used to refer to mountain ranges rising above approximately to . The delineation corresponds with the differentation between Montane and Alpine level according to altitudinal zonation. ''Mittelgebirge'' ranges In the plural, ''die Mittelgebirge'' (as opposed to the singular, ''d ...
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Kahl (river)
The Kahl is a river in the northern Spessart in Bavaria and Hesse, Germany. It is a right tributary of the Main (river), Main and is long. The name Kahl comes from the Old High German word ''kaldaha'', which means cool and clear. The Kahl rises from two sources left and right of the road at the foot of the Spessart hills, near Kleinkahl. These springs produce 50–60 litres per second. The Kahl flows into the river Main in Kahl am Main. The mouth is near the old Kahl Nuclear Power Plant. The largest tributaries are Westerbach (Kahl), Westerbach, Sommerkahl (Kahl), Sommerkahl, Reichenbach (Kahl), Reichenbach and Geiselbach (river), Geiselbach. Tributaries Tributary, Tributaries from source to mouth: Left * Büchelbach * Edelbach (Kahl), Edelbach * Kleine Kahl * Kleinlaudenbach (Kahl), Kleinlaudenbach * Höllenbach (Kahl), Höllenbach * Sommerkahl (Kahl), Sommerkahl * Blankenbach (Kahl), Blankenbach * Erlenbach (Kahl), Erlenbach * Feldkahl * Weibersbach (Kahl, Schimborn), Weibersb ...
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Main (river)
The Main () is the longest tributary of the Rhine. It rises as the White Main in the Fichtel Mountains of northeastern Bavaria and flows west through central Germany for to meet the Rhine below Rüsselsheim, Hesse. The cities of Mainz and Wiesbaden are close to the confluence. The largest cities on the Main are Frankfurt am Main, Offenbach am Main and Würzburg. It is the longest river lying entirely in Germany (if the Weser-Werra are considered separate). Geography The Main flows through the north and north-west of the state of Bavaria then across southern Hesse; against the latter it demarcates a third state, Baden-Württemberg, east and west of Wertheim am Main, the northernmost town of that state. The upper end of its basin opposes that of the Danube where the watershed is recognised by natural biologists, sea salinity studies (and hydrology science more broadly) as the European Watershed. The Main begins near Kulmbach in Franconia at the joining of its two headst ...
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Schanzenkopf (Spessart)
Schanzenkopf (Spessart) is a wooded hill of Bavaria, Germany. It lies in the ''Mittelgebirge'' Spessart in the district of Aschaffenburg. Schanzenkopf has a maximum elevation of 343 metres. It is located in the municipal territory of Alzenau and is part of the ridge Hahnenkamm, the highest elevation of which lies just to the northeast of Schanzenkopf. There is another hill named Schanzenkopf (also known as Schwedenschanze) not far to the northeast, on the other side of the Kahl. The remains of a hill fort A hillfort is a type of earthwork used as a fortified refuge or defended settlement, located to exploit a rise in elevation for defensive advantage. They are typically European and of the Bronze Age or Iron Age. Some were used in the post-Roma ... have been discovered on Schanzenkopf (''Schanze'' is German for fieldwork or rampart). However, it is unclear whether this dates from prehistoric or medieval times. References External links Mountains of Bavaria H ...
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Quartzite
Quartzite is a hard, non- foliated metamorphic rock which was originally pure quartz sandstone.Essentials of Geology, 3rd Edition, Stephen Marshak, p 182 Sandstone is converted into quartzite through heating and pressure usually related to tectonic compression within orogenic belts. Pure quartzite is usually white to grey, though quartzites often occur in various shades of pink and red due to varying amounts of hematite. Other colors, such as yellow, green, blue and orange, are due to other minerals. The term ''quartzite'' is also sometimes used for very hard but unmetamorphosed sandstones that are composed of quartz grains thoroughly cemented with additional quartz. Such sedimentary rock has come to be described as orthoquartzite to distinguish it from metamorphic quartzite, which is sometimes called metaquartzite to emphasize its metamorphic origins. Quartzite is very resistant to chemical weathering and often forms ridges and resistant hilltops. The nearly pure silica conte ...
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