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The Alps 2 Ocean Cycle Trail is a cycle trail in the South Island of New Zealand. This trail is one of the projects of the New Zealand Cycle Trail project. The trail extends more than 300 km (190 mi) from Aoraki / Mount Cook to Oamaru on the Pacific Ocean. From west to east, it descends from an altitude of 780 metres (2,560 ft) down to sea level.
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Alps_to_Ocean_Cycle_Trail,_Twizel.jpg (600 × 482 pixels, file size: 33 KB, MIME type: image/jpeg) This is a file from the Wikimedia Commons . Information from its description page there is shown below.
The Southern Alps are the first obstacle the winds encounter after South America, having moved east across the Southern Ocean. The height of Aoraki / Mount Cook was established in 1881 by G. J. Roberts (from the west side) and in 1889 by T. N. Brodrick (from the Canterbury side). Their measurements agreed closely at 12,349 feet (3,764 m).
The interim name of the new administrative region was a hyphenated placename, composed of the historic region of Auvergne, the river Rhône and the French Alps (Alpes). The same name has been chosen as the definitive name, which was officialized by the Conseil d'État on 28 September 2016.
In the early Jurassic period (180 Ma), a narrow ocean began to form between the northern (North America and Eurasia) and southern (Africa and South America) parts of Pangaea. The oceanic crust that was formed in the process is known as the Piemont-Liguria Ocean. This ocean is generally regarded as a western extension of the Tethys Ocean.
While some of the ranges of the French Alps are entirely in France, others, such as the Mont Blanc massif, are shared with Switzerland and Italy. At 4,808 metres (15,774 ft), Mont Blanc , on the France–Italy border , is the highest mountain in the Alps, and the highest Western European mountain .
In the western Alps the Penninic nappes are more obviously present than in the eastern Alps (in Austria), where they crop out as a narrow band. The name Penninic is derived from the Pennine Alps, an area in which rocks from the Penninic nappes are abundant. Of the three nappe stacks the Penninic nappes have the highest metamorphic grade.