Jura Mountains

The Jura Mountains (/ˈ(d)ʒʊərə/ JOOR-ə, ZHOOR, French: [ʒyʁa] (listen), German: [ˈjuːra] (listen), locally [ˈjuːɾa];[needs Arpitan IPA] French: Massif du Jura; German: Juragebirge; Italian: Massiccio del Giura, Romansh: Montagnas da Jura) 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 as the Table Jura ("not folded Jura", Tafeljura) northeastwards through northern Switzerland and Germany.

Jura Mountains
Landscape of tree-clad valley stretching toward mountainous horizon
View towards Lélex from near the Crêt de la Neige
Highest point
PeakCrêt de la Neige
Elevation1,720 m (5,640 ft)
Coordinates46°16′15″N 5°56′22″E / 46.27083°N 5.93944°E / 46.27083; 5.93944
Geography
Satellite image of the Jura mountains and Western Alps, including Lake Geneva, with major cities labeled
Satellite image of the Jura Mountains (mostly dark green area in the upper left half of the image)
CountriesFrance and Switzerland
Regions/CantonsAuvergne-Rhône-Alpes, Bourgogne-Franche-Comté, Grand Est, Geneva, Vaud, Neuchâtel, Jura, Bern, Solothurn, Basel-Landschaft, Aargau and Zurich
Range coordinates46°40′N 6°15′E / 46.667°N 6.250°E / 46.667; 6.250Coordinates: 46°40′N 6°15′E / 46.667°N 6.250°E / 46.667; 6.250

NameEdit

The mountain range gives its name to the French department of Jura, the Swiss Canton of Jura, the Jurassic period of the geologic timescale, and the Montes Jura of the Moon.

It is first attested as mons Iura in book one of Julius Caesar's Commentarii de Bello Gallico. Strabo uses a Greek masculine form ὁ Ἰόρας ("through the Jura mountains", διὰ τοῦ Ἰόρα ὄρους) in his Geographica (4.6.11). Based on suggestions by Ferdinand de Saussure, early celticists such as Georges Dottin tried to establish an etymon "iura-, iuri" as a Celtic word for mountains,[1] with similar putative etymologies (e.g. *juris, "mountainous forest") still appearing in more recent non-academic publications.[2] However, since there are no clear cognates in the surviving corpus of the Celtic languages, modern studies of Proto-Celtic and Gaulish etymology tend not to list any lemmata connected to Jura, and the name must be considered fundamentally unclear.[3]

PhysiographyEdit

The Jura Mountains are a far province of the larger Central European uplands. The Jura range proper lies in France and Switzerland.[4]

In France, the Jura covers most of the Franche-Comté region, stretching south into the Rhône-Alpes region and north into the Grand Est region. The range reaches its highest point at the Crêt de la Neige (1,720 m (5,640 ft)), in department of Ain, 5km west from the Swiss border of the canton of Geneva, and finds its southern terminus in the northwestern part of the department of Savoie. The north end of the Jura extends into the southern tip of Alsace (Sundgau). Roughly 1,600 km2 (600 sq mi) of the mountain range in France is protected by the Jura Mountains Regional Natural Park.

 
Topographical map (relief map) of Switzerland showing the Jura range proper (Faltenjura) in the northwest and west, and the Alps in the south and east

The Swiss Jura is one of the three distinct geographical regions of Switzerland, the others being the Swiss plateau and the Swiss Alps. Most of the range covers the western border with France. In Switzerland, the Jura Mountains extend over an area covering (from northeast to southwest) the cantons of Zurich, Aargau, Basel-Landschaft, Solothurn, Jura, Bern (i.e., Bernese Jura), Neuchâtel, Vaud, and Geneva. The easternmost mountain of the Jura range proper is the Lägern, situated east of the Aare river. Much of the Swiss Jura region has no historical association with Early Modern Switzerland and was incorporated as part of the Swiss Confederacy only in the 19th century. In the 20th century, a movement for Jura separatism developed which resulted in the creation of the Canton of Jura in 1979.

The east of the Jura range proper separates the Rhine and Rhône basins. The northern and eastern part of the range drains towards the Rhine river and its tributaries Aare and Ill, whereas the western and southern parts drain towards the Rhône river and its (sub)tributaries Doubs, Saône, and Ain. Initially the river Doubs (a subtributary of the Rhône) flows about 100 km (62 mi) northeast, briefly venturing into Switzerland, then changing direction and flowing about 170 km (110 mi) southwest before joining the Saône ca. 140 km (87 mi) north of the French city of Lyon. In Lyon, the Saône joins the Rhône. While the Rhine flows into the North Sea, the Rhône flows into the Mediterranean Sea.

The highest peaks of the Jura Mountains are:

Northeast, the Jura range proper (known as "folded Jura", Faltenjura) is continued as the Table Jura (Tafeljura). The Table Jura ranges (from southwest to northeast) across the Swiss cantons of Basel-Landschaft, Aargau, and Schaffhausen (Randen), and the southern German states of Baden-Württemberg and Bavaria (as Klettgau Jura, Baar Jura, and the Swabian and Franconian plateaus).

GeologyEdit

The range is built up vertically while decreasing in size laterally (along a rough northwest–southeast line). This deformation accommodates the compression from alpine folding as the main Alpine orogenic front moves roughly northwards. The deformation becomes less pervasive away from the younger, more active Alpine mountain building.

The geologic folds comprise three major bands (lithological units) of building that date from three epochs: the Lias (Early Jurassic), the Dogger (Middle Jurassic) and the Malm (Late Jurassic) geologic periods. Each era of folding reveals effects of previously shallow marine environments as evidenced by beds with carbonate sequences, containing abundant bioclasts and oolitic divisions between layers (called horizons).

Structurally, the Jura consists of a sequence of geologic folds, the formation of which is facilitated by an evaporitic decollement layer. The box folds are still relatively young, which is evident by the general shape of the landscape showing that they have not existed long enough to experience erosion, thus revealing recent mountain building.

TourismEdit

The Jura range offer a variety of tourist activities including hiking, cycling, downhill skiing and cross-country skiing. There are many signposted trails including the Jura ridgeway, a 310 km (190 mi) hiking route.

Tourist attractions in the Swiss Jura include natural features such as the Creux du Van, lookout peaks such as the Chasseral, caves such as the Grottes de l'Orbe, as well as gorges such as Taubenloch. The Swiss Jura has been industrialized since the 18th century and became a major centre of the watchmaking industry. The area has several cities at very high altitudes, such as La Chaux-de-Fonds, Le Locle and Sainte-Croix (renowned for its musical boxes); however, it generally has had a marked decline in population since 1960. Both Le Locle and its geographical twin town La Chaux-de-Fonds are recognised as an UNESCO World Heritage Site for their horological and related cultural past.

In the French Jura, the 11th-century Fort de Joux, famously remodeled and strengthened by Vauban in 1690 and subsequently by other military engineers, is situated on a natural rock outcropping in the middle of the range not far from Pontarlier. Part of the A40 autoroute crosses through a portion of the southern Jura between Bourg-en-Bresse and Bellegarde-sur-Valserine, which is known as the "Highway of the Titans".

See alsoEdit

ReferencesEdit

  1. ^ Dottin, Georges (1918). La Langue gauloise : grammaire, textes et glossaire. Paris: Klincksieck. p. 263.
  2. ^ Bossard, Maurice; Chavan, Jean-Pierre (1990). Nos lieux-dits : toponymie romande. Nouv. éd. revue et augmentée. Yens sur Morges: Cabédita. p. 161. ISBN 9782882954640.
  3. ^ Matasović, Ranko (2009). Etymological Dictionary of Proto-Celtic. Leiden: Brill. ISBN 978-90-04-17336-1.
  4. ^ Becker, Arnfried (June 2000). "The Jura Mountains — an active foreland fold-and-thrust belt?". Tectonophysics. 321 (4): 381–406. doi:10.1016/S0040-1951(00)00089-5.

External linksEdit