The Alps

The English name Alps was taken via French from Latin Alpes, which formerly was believed to be ultimately cognate with Latin albus (white). Few... more

by Odon Czintos

Title

The Alps

Artist

Odon Czintos

Medium

Painting

Description

The English name Alps was taken via French from Latin Alpes, which formerly was believed to be ultimately cognate with Latin albus ("white"). Few scholars share this opinion today. The German Albe, Alpe or Alp (f., Old High German alpâ, plural alpûn), the Occitan Alp/Aup[2] and the French Alpage or Alpe in the singular mean "alpine pasture", and only in the plural may also refer to the mountain range as a whole.[3]
Another theory says that Lat. Alpes is a name of non-Indo-European origin (which is common for prominent mountains and mountain ranges in the Mediterranean region). According to the OED, Lat. Alpes might possibly derive from a pre-Indo-European word *alb "hill", with Albania being a related derivation. Interestingly, Albania (which is a foreign name for modern Albanians) has been used as a name for a number of mountainous areas across Europe. In Roman times, Albania was a name for the eastern Caucasus, while in the English language Albania (or Albany) was occasionally used as a name for Scotland.The Alps is split into five climate zones, each with a different kind of environment. The climate, plant life and animal life vary on different sections or zones of the mountain.
Pine trees above the Aletsch Glacier, Valais

The section of the Alps that is above 3,000 metres is called the névé zone. This area, which has the coldest climate, is permanently coated with compressed snow. Plants are therefore scarce in the névé zone.
The alpine zone lies between the height of 2,000 and 3,000 metres. This zone is less cold than in the névé zone. Wildflowers and grasses grow here.
Just below the alpine zone is the subalpine zone, 1,500 to 2,000 metres high. Forests of fir trees and spruce trees grow in the subalpine zone as the temperature slowly goes up.
At about 1,000 to 1,500 metres high is the arable zone. Millions of oak trees sprout in this area. This is also where farming takes place.
Below 1,000 metres are the lowlands. Here, a larger variety of plants are produced. Aside from plants, villages are also in the lowlands because the temperature is more bearable for both humans and animals.

The Alps is a classic example of what happens when a temperate area at lower altitude gives way to higher-elevation terrain. Elevations around the world which have cold climates similar to those found in polar areas have been called Alpine. A rise from sea level into the upper regions of the atmosphere causes the temperature to decrease (see adiabatic lapse rate). 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 in the form of snow or rain.

Uploaded

February 26th, 2012