Alps: Difference between revisions

Browse history interactively ← Previous edit Next edit →Content deleted Content addedVisual WikitextInline

Revision as of 07:55, 15 December 2006 editSengkang (talk \| contribs)38,820 edits Revert to revision 94119781 dated 2006-12-13 19:59:03 by 141.156.160.168 using popups ← Previous edit		Revision as of 12:46, 15 December 2006 edit undo203.110.243.21 (talk)No edit summaryNext edit →
Line 154:		Line 154:
	]		]
	]		]
			]
	]		]
	]		]

Revision as of 12:46, 15 December 2006

For other uses, see the Alps in Europe.

File:Alps in the Chamonix Valley, near the Mer de Glace.jpg

The West face of the Petit Dru above the Chamonix valley near the Mer de Glace.

The Alps (Template:Lang-de; Template:Lang-fr; Template:Lang-it; Template:Lang-sl) is the name for one of the great mountain range systems of Europe, stretching from Austria and Slovenia in the east, through Italy, Switzerland, Liechtenstein and Germany to France in the west. The word "Alps" was taken via French from Latin Alpes (meaning "the Alps"), which may be influenced by the Latin words albus (white) or altus (high), or a Celtic word.

The highest mountain in the Alps is Mont Blanc at 4,808 metres (15,774 ft) on the French-Italian border. All the main peaks of the Alps can be found in the list of mountains of the Alps and list of Alpine peaks by prominence.

Geography

Main article: Geography of the Alps

Subdivision

The Alps are generally divided into the Western Alps and the Eastern Alps. The division is along the line between Lake Constance and Lake Como, following the Rhine. The Western Alps are higher, but their central chain is shorter and curved; they are located in Italy, France and Switzerland. The Eastern Alps (main ridge system elongated and broad) belong to Austria, Germany, Italy, Liechtenstein, Slovenia and Switzerland. The highest peak of the Western Alps is Mont Blanc, 4,808 metres (15,774 ft). The highest peak in the Eastern Alps is Piz Bernina, 4,052 meters (13,294 ft).

The Eastern Alps are commonly subdivided according to the different lithology (rock composition) of the more central parts of the Alps and the groups at its northern and southern fringes:

Flysch zone (from the Wienerwald to Bregenzerwald). Geographically, the Jura mountains do not belong to the Alps; geologically, however, they do.
Northern Limestone Alps, peaks up to 3,000 metres (9,850 ft)
Central Eastern Alps (Austria, Switzerland), peaks up to 4,050 metres (13,290 ft)
Southern Limestone Alps.

The border between the Central Alps and the Southern Limestone Alps is the Periadriatic Seam. The Northern Limestone Alps are separated from the Central Eastern Alps by the Grauwacken Zone.

File:Italian alps1.jpg

The Italian Alps as seen from the air

The Western Alps are commonly subdivided with respect to geography:

Series of lower mountain ranges run parallel to the main chain of the Alps, including the French Prealps. (See Alpine geography.)

The geologic subdivision is different and makes no difference between the Western and Eastern Alps: Helveticum in the north, Penninicum and Austroalpine system in the centre and south of the Periadriatic seam the Southern Alpine system and parts of the Dinarides (see Alpine Geology).

Main chain

Main article: Main chain of the Alps

The "main chain of the Alps" follows the watershed from the Mediterranean Sea to the Wienerwald, passing over many of the highest and most famous peaks in the Alps. From the Colle di Cadibona to Col de Tende it runs westwards, before turning to the north-west and then, near the Colle della Maddalena, to the north. Upon reaching the Swiss border, the line of the main chain heads approximately east-north-east, a heading it follows until its end near Vienna.

Principal passes

Main article: Principal passes of the Alps

The Alps do not form an impassable barrier; they have been traversed for war and commerce, and later by pilgrims, students and tourists. Crossing places by road, train or foot are called passes. These are depressions in the mountains to which a valley leads from the plains and hilly pre-mountainous zones.

Climate

Main article: Climate of the Alps

The Alps are a classic example of what happens when a temperate area at lower altitude gives way to higher elevation terrain. As a matter of fact, elevations around the world which have cold climates similiar to those found in polar areas has been called alpine. As we rise from sea level into the upper regions of the atmosphere, the temperature decreases. The effect of mountain chains on prevailing winds is to carry warm air belonging to the lower region into an upper zone, where it expands in volume at the cost of a proportionate loss of heat, often accompanied by the precipitation of moisture in the form of snow or rain.

Geology

Main article: Geology of the Alps

The Alps arose as a result of the pressure exerted on sediments of the Tethys Ocean basin as its Mesozoic and early Cenozoic strata were pushed against the stable Eurasian landmass by the northward-moving African landmass. Most of this occurred during the Oligocene and Miocene epochs. The pressure formed great recumbent folds, or nappes, that rose out of what had become the Tethys Sea and pushed northward, often breaking and sliding one over the other to form gigantic thrust faults. Crystalline rocks, which are exposed in the higher central regions, are the rocks forming Mont Blanc, the Matterhorn, and high peaks in the Pennine Alps and Hohe Tauern.

The landscape seen today is mostly formed by glaciation during the past two million years. At least five ice ages have done much to change the region, scooping out the lakes and rounding off the limestone hills along the northern border. Glaciers have been retreating during the past 10,000 years, leaving large granite erratics scattered in the forests in the region. As the last ice age ended, it is believed that the climate changed so rapidly that the glaciers retreated back into the mountains in a span of about 200 to 300 years.

Political history

Main article: History of the Alps

Little is known of the early dwellers in the Alps, save from the scanty accounts preserved by Roman and Greek historians and geographers. A few details have come down to us of the conquest of many of the Alpine tribes by Augustus.

The successive emigration and occupation of the Alpine region by various Teutonic tribes from the 5th to the 6th centuries are known only in outline, because to them, as to the Frankish kings and emperors, the Alps offered a route to other places rather than a permanent residence.

It is not until the final breakup of the Carolingian Empire in the 10th and 11th centuries that it becomes possible to trace out the local history of the Alps.

Exploration

Main article: Exploration of the High Alps

The higher regions of the Alps were long left to the exclusive attention of the people of the adjoining valleys, even when Alpine travellers (as distinguished from Alpine climbers) began to visit these valleys. The two men who first explored the regions of ice and snow were H.B. de Saussure (1740-1799) in the Pennine Alps, and the Benedictine monk of Disentis, Placidus a Spescha (1752-1833), most of whose ascents were made before 1806, in the valleys at the sources of the Rhine.

Flora

A natural vegetation limit with altitude is given by the presence of the chief deciduous trees — oak, beech, ash and sycamore maple. These do not reach exactly to the same elevation, nor are they often found growing together; but their upper limit corresponds accurately enough to the change from a temperate to a colder climate that is further proved by a change in the wild herbaceous vegetation. This limit usually lies about 1,200 metres (3,940 ft) above the sea on the north side of the Alps, but on the southern slopes it often rises to 1,500 metres (4,920 ft), sometimes even to 1,700 metres (5,580 ft).

This region is not always marked by the presence of the characteristic trees. The interference of man has in many districts almost removed them, and, excepting the beech forests of the Austrian Alps, a considerable wood of deciduous trees is rare. In many districts where such woods once existed, their place has been occupied by the Scots pine and Norway spruce, which suffer less from the ravages of goats, the worst enemies of tree vegetation. The mean annual temperature of this region differs little from that of the British Islands; but the climate conditions are widely different. Here snow usually lies for several months, till it gives place to a spring and summer considerably warmer than the average of British seasons.

Above the forestry, there is often a band of short pine trees (Pinus mugo), which is in turn superseded by dwarf shrubs, typically Rhododendron ferrugineum (on acid soils) or Rhododendron hirsutum (on basic soils). Above this is the alpine meadow, and even higher, the vegetation becomes more and more sparse. At these higher altitudes, the plants tend to form isolated cushions. In the Alps, several species of flowering plants have been recorded above 4,000 metres (13,125 ft), including Ranunculus glacialis, Androsace alpina and Saxifraga biflora.