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Showing posts with label Mountains. Show all posts
Showing posts with label Mountains. Show all posts

Alpine System

Alps, great mountain system of south central Europe, forming an arc some 1200 km (750 mi) long from the Gulf of Genoa to the Danube River at Vienna. The Alps are the highest and most densely settled mountain belt of Europe, occupying an area of about 200,000 sq km (about 80,000 sq mi) and inhabited by some 20 million people. The valleys of the Alps are areas of year-round settlement; the flatter upland tracts comprise pastures and seasonally inhabited settlements, and the zone above the timberline serves as pasture and for recreation. Important economic activities include tourism, dairy farming, forestry, the production of hydroelectric power, and the extraction of salt and iron ore. With its important pass routes between central and southern Europe, the Alps have been an area of transit trade since ancient times.


Structurally, the Alpine mountain system is divided into the Western and Eastern Alps by a furrow that leads from the Rhine Valley in northern Switzerland, across Splügen Pass to Lake Como in northern Italy. The Western Alps average about 1000 m (about 3300 ft) higher and are narrower and more rugged than the Eastern Alps. The highest peak of the Alps, Mont Blanc (4807 m/15,771 ft), is on the Franco-Italian border. Among the principal ranges are the Maritime, Ligurian, Cottian, and Alpes Grées in France and Italy and the Bernese, Glarus, and Pennine (or Valais) Alps in Switzerland. The Jura Mountains are a northwestern outlier of the French Alps. From Lake Geneva the Alpine ranges curve northeast and become more widely separated, attaining a width of 250 km (155 mi) in the center of the arc. The ranges of the Eastern Alps diverge, finally to plunge to the Danubian Basin near Vienna. Well-known mountain chains of the Eastern Alps are the Bavarian Alps, Allgäu Alps, Hohe Tauern, and Niedere Tauern in the north and the Dolomite and Carnic Alps in the south.


Summit regions above 3000 m (about 9800 ft) are glaciated. Peaks and crests, however, rise above the ice, displaying jagged shapes (toothlike horns, needles, and knife-edged ridges). About 2% of the total area of the Alps is covered by ice. The longest valley glacier, the Aletsch Glacier in the Bernese Alps, is 18 km (11 mi) long.


Broad and deep longitudinal valleys, which hold the courses of the upper Rhône, upper Rhine, Inn, Salzach, Mur, and Drava (Drau) rivers, separate the structural units of the Alps, and contain the main settlements and the principal arteries for traffic. Deeply incised, transverse tributary valleys lead up to the pass regions. Passes at elevations above 2000 m (about 6600 ft) are blocked with snow during the winter months; these include the Mont Cenis, Great Saint Bernard, Simplon, and Saint Gotthard passes. Brenner Pass, at 1,371 m (4,497 ft), and Reschen Pass, at 1508 m (4948 ft), provide the easiest crossings. Engineering feats, such as tunneling of the higher passes for highways and railroads, have lessened the barrier effect of the Alps.

Source: Encarta

So Beautiful Cliffs






See my blog archives for more pictures.

Cliff






See my blog archives for more pictures....

Global Warming Causes Glacier to Grow

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The glaciers on Mount Shasta in California are growing because of global warming, experts say.

"When people look at glaciers around the world, the majority of them are shrinking," said Slawek Tulaczyk, a University of California, Santa Cruz, professor who studied the glaciers.

But the seven glaciers on Shasta, part of the Cascade mountains in northern California, "seem to be benefiting from the warming ocean," he said.

As the ocean warms, more moisture evaporates. As moisture moves inland, it falls as snow — enough on Shasta to more than offset a 1 C temperature rise in the past century.

The three smallest of the Shasta glaciers are more than twice the length they were in 1950.

Other glaciers in Norway, Sweden, New Zealand and Pakistan were in the same position as Shasta, but are now shrinking because rising temperatures have more than offset the increased snowfall.

As many as 90 per cent of Earth's mountain glaciers are getting smaller, said Lonnie Thompson from Ohio State University.

A U.S. government inventory found that, with one exception, Shasta's glaciers are the only ones growing on the U.S. mainland, said Andrew Fountain, a professor at Portland State University, who worked on the assessment.

The exception is a small glacier that is shaded in the crater of Mount St. Helens, Wash. It's unlikely to continue to grow once it leaves the shade, scientists said.

Four glaciers on the shady north and east sides of Mount Rainier, Wash., are stable.

 
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