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
Main features
The Alpine Divide is defined for much of its distance by the watershed between the drainage basin of the
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 Eastern Alps (main ridge elongated and broad) belong to Austria, Germany, Italy, Slovenia, and Switzerland.
- 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
From the
The
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
Western Alps
Starting from the
The divide then briefly turns north to the
The
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+1⁄4 miles) a century ago, the Mer de Glace at Chamonix (now 7.6 km or 4+3⁄4 mi) and the Gorner Glacier at Zermatt (now 12.5 km or 7+3⁄4 mi). In the Eastern Alps the longest glacier was the Pasterze Glacier (8.4 km or 5+1⁄4 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
public domain: Lake, 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.
This article incorporates text from a publication now in the- ISBN 9789264031692.
They are generally divided into the Western Alps and the Eastern Alps, separated by Rhine and the Splügen pass in eastern Switzerland.
- ^ a b "Mont Blanc shrinks by 45cm in two years". The Sydney Morning Herald. 2009-11-05. Archived from the original on 2023-02-14.
- Federal Office of Topography. Retrieved 4 April 2022.
External links
- Simplified depiction of the Alpine divide on GeoFinder.ch