Merkur (Baden-Baden)
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Merkur (Baden-Baden)
The Merkur or Großer Staufenberg is a mountain, , in the Northern Black Forest, Baden-Württemberg, Germany. It is the ''Hausberg'' of Baden-Baden and located between the spa town and the town of Gernsbach. Name The mountain is named after the Ancient Roman god of trade and commerce, Mercury, to whom a Roman votive stone on the summit is dedicated. The ''Merkurstein'' has been recorded since the 16th century. Today, there is a cast of the original votive stone on the summit plateau; its prototype is in the Baden-Baden Municipal Museum collection. The original name of the free-standing conical mountain was the ''Großer Staufenberg'', a reference to the shape of a turned drinking mug known as a '' Stauf''. Funicular The summit of the Merkur is only accessible on foot, by bicycle or on the Merkur Funicular Railway (the ''Merkurbergbahn'') from Baden-Baden. The funicular was built in , closed in for technical reasons, and re-opened in . It is long, one of the longest railw ...
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Fremersberg
The Fremersberg is a hill, , on the western edge of the northern Black Forest in south Germany on the territory of the town of Baden-Baden and the municipality of Sinzheim. On the summit plateau, which is made of bunter sandstone there is the residential area of ''Fremersberg Turm'' with rented inn, which was built by the town of Baden-Baden in 1884, and the 85-metre-high Fremersberg Tower, built in 1961, a transmission tower with an observation platform. Fremersberg Tower The construction of the first viewing tower on the Fremersberg was finished in 1883. It was raised in 1900 to a height of around , using rubble stone from a Sinzheim quarry. In 1954 it had to be demolished due to its instability and consequent danger of collapse. By July 1954 a new tower had been built from the old stone that was more stable. As the establishment of a TV studio for Südwestfunk in ''Hans-Bredow-Straße'' in Baden-Baden required a permanent microwave relay station, the tower was pulled down for ...
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European Mouflon
The European mouflon (''Ovis aries musimon'') is a feral subspecies of the primitive domestic sheep. It was originally found only on the Mediterranean islands of Corsica and Sardinia, but has since been introduced into many other regions of Europe. It is not to be confused with ''Ovis gmelini'', also called the mouflon, which is found in Western Asia and is also ancestral to modern domestic sheep. Description Male mouflon are known as rams and the females as ewes. The young animals are known as lambs. Appearance European mouflon have a body length of up to 120 cm, a shoulder height of 90 cm, a weight of 25 to 40 kg for ewes, 35 to 55 kg for the ram. The European mouflon has a smooth hairy coat, the rams are fox red-brown in the summer, usually with a whitish saddle patch, the ewes are brownish. Both sexes are darker in winter. The rams have helix-shaped horns up to 80 cm long; females have no horns on Sardinia, but on Corsica they have smaller ...
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Yburg Castle
The Yburg is a ruined hilltop castle atop the Yberg, on the western edge of the Black Forest near Baden-Baden, in southwestern Germany. History In 1190, Herman V, Margrave of Baden-Baden inherited the rights to the villages of Steinbach and Sinzheim. As the Yburg would have secured the Margraviate of Baden's new southwest border, it can be assumed that they built it at this time. The surrounding territory increasingly came under Baden's influence from mid-13th century on; Eberstein Castle was constructed nearby, Hohenbaden Castle was enlarged, and Steinbach was fortified and given the status of a township. Until 1369, the Yburg was administered by the Röder von Rodeck family, who served the House of Baden as civil servants. In the 15th century, under Margrave Bernhard I, a bailiff resided at Yburg, and it is likely the castle received its eastern annex for their residence. The Yburg was destroyed in 1525 during the German Peasants' War. In 1535, the Margraviate of Baden s ...
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Alt Eberstein
The ruins of Alt-Eberstein are the remains of the former Schloss Eberstein (Eberstein Castle), located on a hill near the town of Ebersteinburg and directly upstream of the modern city of Baden-Baden, in the state of Baden-Württemberg, Germany. The original structure was built in 1100 as the primary residence of the Counts of Eberstein The County of Eberstein was a territory within the Holy Roman Empire, situated in the southwest of modern Germany. From 1085 up into the 13th century, the Counts of Eberstein lived in the castle known today as Alt Eberstein which lies on a moun ..., but by the end of the 16th century had been abandoned and much of the castle was torn down to provide materials for other structures. Presently it is a German national monument and a State Palace of Baden-Wuerttemberg. History A spur castle situated on a once-strategic mountain peak, the fortress was constructed as the seat of the Counts of Eberstein perhaps as early as 1100. The oldest part of ...
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Battert
The Battert is a hill, , on the western edge of the Northern Black Forest north of Baden-Baden in Germany. On its western slopes are the ruins of Hohenbaden Castle (the ''Altes Schloss'' or "Old Castle"), on the southern side is the climbing area and nature reserve called the Battert Rocks (''Battertfelsen''). On the hill ridge are the remains of a circular rampart, probably built by Celtic settlers. On the eastern side lies the village of Ebersteinburg. The Battert is a destination for ramblers and climbers all year round, heading for the 15–60-metre-high ''Battertfelsen''. Above and below the rock face is a footpath around the rocks. The red rock face is visible from far off and may be easily reached on the road to the ruins of Hohenbaden or from a car park near Ebersteinburg. Geology Consisting of sediments of Rotliegend, the Battertfelsen were formed about 251-299 million years ago. By contrast with their immediate environment, the rocks of the Battertfelsen silicified ...
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Hohenbaden Castle
Hohenbaden Castle (at the time of its establishment ''Schloss Hohenbaden'', now ''Old castle'' or ''Altes Schloss'') in German Baden-Baden was the residence of the margraves of Baden for almost 400 years. The castle was built around 1100 by Herman II, Margrave of Baden (1074–1130) on the west flank of the Battert rock. Under Margrave Bernard I (1372–1431) the Gothic lower castle was built. This was expanded again by Jacob, Margrave from 1431 to 1453. At its peak, the castle had a hundred rooms. Christopher I built the ''New castle'' in the town of Baden Baden (; ) is a historical territory in South Germany, in earlier times on both sides of the Upper Rhine but since the Napoleonic Wars only East of the Rhine. History The margraves of Baden originated from the House of Zähringen. Baden i ... itself and moved there in 1479. The ''Old castle'' then served as a widow's residence until it was destroyed by fire in 1599. Baden-Baden-Altes Schloss Hohenbaden-01a-Ritte ...
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Odenwald
The Odenwald () is a low mountain range in the German states of Hesse, Bavaria and Baden-Württemberg. Location The Odenwald is located between the Upper Rhine Plain with the Bergstraße and the ''Hessisches Ried'' (the northeastern section of the Rhine rift) to the west, the Main and the Bauland (a mostly unwooded area with good soils) to the east, the Hanau-Seligenstadt Basin – a subbasin of the Upper Rhine Rift Valley in the Rhine-Main Lowlands – to the north and the Kraichgau to the south. The part south of the Neckar valley is sometimes called the ''Kleiner Odenwald'' ("Little Odenwald"). The northern and western Odenwald belong to southern Hesse, with the south stretching into Baden. In the northeast, a small part lies in Lower Franconia in Bavaria. Geology The Odenwald, along with other parts of the Central German Uplands, belongs to the Variscan, which more than 300 million years ago in the Carboniferous period ran through great parts of Europe. The cause ...
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Haardt (Pfalz)
The Haardt () is a range of wooded, sandstone hills in the state of Rhineland Palatinate in southwestern 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 betwe .... The range is some long and lies within the Palatinate Forest (''Pfälzerwald''). Its highest point is the Kalmit, near Maikammer, which stands above sea level. References Hill ranges of Germany Geography of the Palatinate (region) Natural regions of the Palatinate Forest Landscapes of Rhineland-Palatinate Landforms of Rhineland-Palatinate {{RhinelandPalatinate-geo-stub ...
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Vosges
The Vosges ( , ; german: Vogesen ; Franconian and gsw, Vogese) are a range of low mountains in Eastern France, near its border with Germany. Together with the Palatine Forest to the north on the German side of the border, they form a single geomorphological unit and low mountain range of around in area. It runs in a north-northeast direction from the Burgundian Gate (the Belfort–Ronchamp– Lure line) to the Börrstadt Basin (the Winnweiler– Börrstadt–Göllheim line), and forms the western boundary of the Upper Rhine Plain. The Grand Ballon is the highest peak at , followed by the Storkenkopf (), and the Hohneck ().IGN maps available oGéoportail/ref> Geography Geographically, the Vosges Mountains are wholly in France, far above the Col de Saverne separating them from the Palatinate Forest in Germany. The latter area logically continues the same Vosges geologic structure but traditionally receives this different name for historical and political reasons. From ...
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Upper Rhine Plain
The Upper Rhine Plain, Rhine Rift Valley or Upper Rhine Graben (German: ''Oberrheinische Tiefebene'', ''Oberrheinisches Tiefland'' or ''Oberrheingraben'', French: ''Vallée du Rhin'') is a major rift, about and on average , between Basel in the south and the cities of Frankfurt/Wiesbaden in the north. Its southern section straddles the France–Germany border. It forms part of the European Cenozoic Rift System, which extends across Central Europe. The Upper Rhine Graben formed during the Oligocene, as a response to the evolution of the Alps to the south. It remains active to the present day. Today, the Rhine Rift Valley forms a downfaulted trough through which the river Rhine flows. Formation The Upper Rhine Plain was formed during the Early Cenozoic era, during the Late Eocene epoch. At this time, the Alpine Orogeny, the major mountain building event that was to produce the Alps, was in its early stages. The Alps were formed because the continents of Europe and Africa colli ...
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Gaggenau
Gaggenau is a town in the district of Rastatt, in Baden-Württemberg, Germany. It is located some 8 km northeast of Baden-Baden. History Gaggenau was first mentioned in local records in 1243 under the name "Gaggenaw". The present district of Bad Rotenfels is even older, having been mentioned in a royal donation letter in 1041. Gaggenau remained a small village until the 19th century: Originally part of the Ufgau, it came under the jurisdiction of the marquisate of Baden in the 13th century, and was included in the territory claimed by the Margrave of Baden-Baden in 1535, which held it until 1689. At that time, it was placed under the jurisdiction of the Kuppenheim district of the Bishopric of Speyer. It was eventually assigned to the jurisdiction of the Rastatt Office of the State of Baden, which later became the District of Rastatt. In 1691, the area was at the heart of the Palatinate War of Succession and was almost completely destroyed by the French forces. In 1772, A ...
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Murg (Northern Black Forest)
The Murg is an 80.2-kilometre-long river (including its headstream, the ''Rechtmurg'') and a right tributary of the Rhine in Baden-Württemberg, Germany. It flows through the Northern Black Forest into the Upper Rhine Plain, crossing the counties of Landkreis Freudenstadt, Freudenstadt and Landkreis Rastatt, Rastatt. Geography Course The Murg valley is one of the largest and deepest valleys in the Black Forest (up to over 700 metres deep) and generally runs in a northerly direction. It separates the precipitation-rich main crest of the Northern Black Forest, including the Hornisgrinde (1,164 m), to the west, from the densely forested bunter sandstone plateaux in the east. The Murg originates from 2 large headstreams in the western part of the municipality of Baiersbronn. Below the Schliffkopf at about , the main headstream of the Right Murg (''Rechtmurg'') is formed by the Schurbach stream and Tränkenteich pond, a little above the ''Murgursprung'' ("Murg Source"). The o ...
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