Main chain of the Alps

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Main chain of the Alps

The main chain of the Alps, also called the Alpine divide is the central line of mountains that forms the

Salzburg
.

Main features

The Alpine Divide is defined for much of its distance by the watershed between the drainage basin of the

Rhone, the Rhine and the Danube. Further east, the watershed is between the Adige and the Danube, before heading into Austria and draining on both sides into the Danube. For much of its distance the watershed lies on or close to the Italian border, although there are numerous deviations, notably, the Swiss canton of Ticino
which lies south of the range in the Po river basin.

For only a small portion of its total distance does the Alpine divide form a part of the main European watershed, in the central section where the watershed is between the Po and the Rhine.

The Alps are generally divided into Eastern Alps and Western Alps, cut along a line between Lake Como and Lake Constance, following the Rhine valley.[1]

  • The Western Alps are higher, but their central chain is shorter and much curved; they are located in France, Italy, and Switzerland.

Piz Bernina (4,049 metres) is the highest peak of the Eastern Alps while the highest peak of the Western Alps is Mont Blanc (4,810.45 metres).[2]

Eastern Alps

Main ridge (Fuscherkarkopf) in the Hohe Tauern range

From the

Ofen Pass (2,149 m), soon heads north and rises once more in Piz Sesvenna
(3,204 m).

The

Inn valley. Eastward of this pass, the main chain runs north-east to the Brenner Pass along the snowy crest of the Ötztal, the highest point being the Weißkugel (3,739 m), then crossing the Timmelsjoch (2,474 m) and rising again in Stubai Alps Both the highest summits of the Ötztal and the Stubai, the Wildspitze (3,774 m) and the Zuckerhütl
(3,505 m), stand a little to the north.

The Brenner (1,370 m) is the lowest of all the great road passes across the core part of the main chain and has always been the chief means of communication between Germany and Italy. For some way beyond it, the watershed runs eastwards over the highest crest of the Zillertal Alps, which attains 3,510 metres in the Hochfeiler. But, a little farther, at the Dreiherrnspitze (3,499 m), the chain splits: the main watershed between the Black Sea and the Mediterranean heads south, along the Rieserferner Group to the Dolomites, and Julian Alps.

The main alpine divide head east, traversing the

Grossvenediger (3,666 m), passing just north of Austria's highest peak (the Grossglockner), traversing Ankogel (3,252 m), before curving northern across the Lower Tauern, traversing its highest peak, Hochgolling (2,863 m) in the Schladming Tauern and then continuing on the same eastward path up to the Schober Pass in Styria. The drainage divide further runs eastwards through the Northern Limestone Alps, ending at "Vienna Gate", the steep slopes of the Leopoldsberg (425 m) high above the Danube water gap and the Vienna Basin
.

Western Alps

Starting from the

Val Pellice the main chain runs north-west and diminishes much in average height until it reaches the Mont Thabor (3,178 m), which forms the apex of a salient angle which the main chain here presents towards the west. From here the divide extends eastwards, culminating in the Aiguille de Scolette (3,505 m), but makes a great curve to the north-west and back to the south-east before rising in the Rocciamelone (3,509 m). From there the direction taken is north as far as the eastern summit (3,619 m) of the Levanna, the divide rising in a series of snowy peaks, though the loftiest point of the region, the Pointe de Charbonnel (3,760 m), stands a little to the west. Once more the chain bends to the north-west, rising in several lofty peaks (the highest is the Aiguille de la Grande Sassière, 3,751 m), before attaining the considerable depression of the Little St Bernard Pass
.

View of the Witenwasserenstock with the tripoint between the Rhone, Rhine, and Po basins (center left)

The divide then briefly turns north to the

Great St. Bernard Pass, a generally eastern direction that it maintains until it reaches Monte Rosa, where it bends northwards, making one small dip to the east to the Simplon Pass. It is in the portion of the watershed between the Grande St Bernard Pass and the Simplon that the main chain maintains a greater average height than in any other part. But, though it rises in a number of lofty peaks, such as the Mont Vélan (3,727 m), the Matterhorn (4,478 m), the Lyskamm (4,533 m), the Nord End of Monte Rosa (4,575 m), and the Weissmies (4,023 m), many of the highest points of the region, such as the Grand Combin (4,314 m), the Dent Blanche (4,357 m), the Weisshorn (4,505 m), the true summit or Dufourspitze (4,634 m) of Monte Rosa itself, and the Dom
(4,545 m), all rise on its northern slope and not on the main chain. On the other hand, the chain between the Grande St Bernard and the Simplon sinks at barely half a dozen points below a level of 3,000 metres.

The

Lunghin pass, it reaches the main triple divide of the Alps: where water can flow to the Atlantic, the Mediterranean or the Black Sea. The main European watershed leaves the Alpine divide here, heading north, while the divide continues east to the Maloja Pass
(1,815 m).

Glaciers

The main chain has more glaciers and eternal snow than the independent or external ranges. The longest of these were both 14.9 kilometres (9+14 miles) a century ago, the Mer de Glace at Chamonix (now 7.6 km or 4+34 mi) and the Gorner Glacier at Zermatt (now 12.5 km or 7+34 mi). In the Eastern Alps the longest glacier was the Pasterze Glacier (8.4 km or 5+14 mi in 1911), which is not near the true main watershed, though it clings to the slope of the Grossglockner (3,798 m) in the Hohe Tauern range east of the Dreiherrenspitze. But two other long glaciers in the Eastern Alps (the Hintereis, and the Gepatsch) are both in the Ötztal Alps, and so are close to the true main watershed.

See also

References

 This article incorporates text from a publication now in the public domainLake, Philip; Knox, Howard; Coolidge, W. A. B. (1911). "Alps". In Chisholm, Hugh (ed.). Encyclopædia Britannica. Vol. 1 (11th ed.). Cambridge University Press. pp. 737–754.

External links