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The Limmat is a river in Switzerland. The river commences at the outfall of Lake Zurich, in the southern part of the city of Zurich. From Zurich it flows in a northwesterly direction, continuing a further 35 km until it reaches the river Aare. The confluence is located north of the small town of Brugg and shortly after the mouth of the Reuss.
Map of the Aar basin. High Rhine. Aare. Limmat. Linth () . Lake Walen. Seeztal; Klöntal; Sernftal; Reuss. Lake Lucerne. Sarner Aa (Brünig Pass connects to the Aare ...
The Alps continue fairly smoothly into the following related Alpine mountain ranges: the Apennines to the southwest, the Dinarides to the southeast and the Carpathians to the northeast. In the east the Alps are bounded by the Viennese Basin and the Pannonian Basin, where east–west stretching of the crust takes place.
Natural-colour satellite image of north-eastern Italy showing parts of the Cellina, Meduna, and Tagliamento rivers. The Tagliamento (Italian: [taʎʎaˈmento]; Friulian: Tiliment; Venetian: Tajamento) is a braided river in north-east Italy, flowing from the Alps to the Adriatic Sea at a point between Trieste and Venice.
At places throughout the Alps the European basement was, after being detached of its cover rocks, tectonically uplifted in a late stage of the orogeny. Thus the "external massives" were formed, places where the Hercynian basement rock crops out in large anticlinoria at the southern (or in France eastern) side of the Helvetic zone.
Danube or Donau is a timespan in the glacial history of the Alps. Danube is currently regarded to have started approximately 1.8 million years ago, at the start of the Calabrian age of the international geochronology. It ended approximately one million years ago. Deep sea core samples have identified approximately 20 glacial cycles during ...
The Massa (German pronunciation:) is a seven kilometre long river in the eastern Bernese Alps in the Swiss canton of Valais. It is mainly fed by the melt-water from the Aletsch Glacier. [1] It passes through the Massa Gorge and flows into the Stausee Gibidum reservoir and onwards to its confluence with the Rhône.