Table Jura in the context of "Jura Mountains"

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⭐ Core Definition: Table Jura

The so-called Table Jura or Plateau Jura (German: Tafeljura; French: le Jura tabulaire) is the northeastern extension of the Jura Mountains. It stands in opposition to the folded Jura (Faltenjura) of the Jura range proper.

The Table Jura stretches across the Swiss cantons of Basel-Landschaft, Aargau and Schaffhausen into southern Germany (Baden-Württemberg, Bavaria). It includes the Randen, Baar, the Swabian Jura and the Franconian Jura. The Table Jura thus ranges from near the Swiss city of Basel to the German city of Coburg.

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Table Jura in the context of Jura mountains

The Jura Mountains (/ˈʊərə, ˈʒʊərə/ JOOR-ə, ZHOOR) are a sub-alpine mountain range, a short distance north of the Western Alps, and mainly demarcate a long part of the French–Swiss border. While the Jura range proper ("folded Jura", Faltenjura) is located in France and Switzerland, the range continues northeastwards through northern Switzerland and Germany as the Table Jura ("not folded Jura", Tafeljura), which is crossed by the High Rhine.

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Table Jura in the context of Swabian Jura

The Swabian Jura (German: Schwäbische Alb [ˈʃvɛːbɪʃə ˈʔalp] , more rarely Schwäbischer Jura [ˈʃvɛːbɪʃɐ ˈjuːʁa] ), sometimes also named Swabian Alps in English, is a mountain range in Baden-Württemberg, Germany, extending 220 km (140 mi) from southwest to northeast and 40 to 70 km (25 to 43 mi) in width. It is named after the region of Swabia. It is part of the Table Jura (Tafeljura).

The Swabian Jura occupies the region bounded by the Danube in the southeast and the upper Neckar in the northwest. In the southwest it rises to the higher mountains of the Black Forest. The highest mountain in the region is the Lemberg (1,015 m (3,330 ft)). The area's profile resembles a high plateau, which slowly falls away to the southeast. The northwestern edge is a steep escarpment (called the Albtrauf or Albanstieg, rising up 400 m (1,300 ft), covered with forests), while the top is flat or gently rolling.

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Table Jura in the context of Franconian Jura

The Franconian Jura (German: Fränkische Alb [ˈfʁɛŋkɪʃə ˈʔalp] , Fränkischer Jura, Frankenalb or Frankenjura) is an upland in Franconia, Bavaria, Germany. Located between two rivers, the Danube in the south and the Main in the north, its peaks reach elevations of up to 600 metres (2,000 ft) and it has an area of some 7053.8 km. It is part of the Table Jura (Tafeljura).

Large portions of the Franconian Jura are part of the Altmühl Valley Nature Park. The scenic meanders and gorges formed by the river Altmühl draw tourists to visit the region.

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Table Jura in the context of Randen (mountain range)

The Randen is a small mountain range located between the Jura and the Swabian Jura, north of the Rhine. Predominantly located in the Swiss canton of Schaffhausen, they culminate in the German state of Baden-Württemberg. The Randen, which belong to the Table Jura (Tafeljura), are situated north of Schaffhausen and south of Blumberg.

The highest peak is the Schlattersteig (930 m (3,051 ft)), which is part of the more prominent Hoher Randen (909 m (2,982 ft)) in Germany. Other important summits are the Hage (912 m (2,992 ft)), the Lange Rande (900 m (2,953 ft)), and the Schlossranden (890 m (2,920 ft)) with the Schleitheimer Randenturm (896 m (2,940 ft)) in Switzerland.

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Table Jura in the context of Baar (region)

The Baar (German pronunciation: [baːɐ̯] ) is a plateau that lies 600 to 900 metres above sea level in southwest Germany. It is part of the Table Jura (Tafeljura). It is bordered by the southeastern edge of the Black Forest to the west, the southwestern part of the Swabian Alb known as the Heuberg to the east, and the Randen mountain to the south.

The Baar contains the source of the Neckar (a bog in Villingen-Schwenningen) and the Danube. The sources of the Danube, the Brigach and Breg, originate in Furtwangen im Schwarzwald and Sankt Georgen im Schwarzwald and join the smaller Donaubach in Donaueschingen.

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Table Jura in the context of Albtrauf

The term Albtrauf (Alp escarpment) refers to the northwest facing escarpment of the Swabian Alps, situated in Baden-Württemberg and Bavaria. It is the most distinctive stepped slope within the alpine region of the South German Scarplands, leading roughly from the southwest to the northeast.

The Albtrauf has its geological extension in the northeast, in the stepped slopes of the Franconian Jura and in the southwest and west among the Jurassic period stepped slopes of the Baaralb, Hegaualb, Randen, Klettgau, Aargau as well as the Table Jura stretches from the city of Basel to the Ajoie and the French Scarplands.

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