Bernese Alps

GeographyEdit

One of the most considerable Alpine ranges, the Bernese Alps extend from the gorge of Saint-Maurice, through which the Rhone finds its way to Lake Geneva, to the Grimsel Pass or, depending on the definition, to the river Reuss (thus including the Uri Alps). The principal ridge, a chain that runs 100 kilometres (62 mi) from west (Dent de Morcles) to east (Sidelhorn), whose highest peak is the Finsteraarhorn, forms the watershed between the cantons of Bern and Valais. Except for the westernmost part, it is also the watershed between the Rhine (North Sea) and the Rhone (Mediterranean Sea). This chain is not centered inside the range but lies close (10 to 15 km) to the Rhone on the south. This makes a large difference between the south, where the lateral short valleys descend abruptly into the deep trench forming the valley of the Rhone and the north, where the Bernese Alps extends through a great part of the canton of Bern (Bernese Oberland), throwing out branches to the west into the adjoining cantons of Vaud and Fribourg. There the mountains progressively become lower and disappear into the hilly Swiss Plateau.

The main chain west of Gemmi Pass consists mainly of a few large prominent summits (as the Wildhorn) slightly above 3,000 metres (9,800 ft), generally covered by glaciers. On the eastern part, the main chain became suddenly wider and the peaks reach over 4,000 metres (13,000 ft), in the most glaciated part of the Alps.

A characteristic in the orography of the Bernese Alps is, that whereas the western of that chain consists of a single series of summits with comparatively short projecting buttresses, the higher group presents a series of longitudinal ridges parallel to the axis of the main chain, and separated from each other by deep valleys that form the channels of great glaciers. Thus the Tschingel Glacier and the Kander Glacier, separate the portion of the main range lying between the Gemmi Pass and the Mittaghorn from the equally high parallel range of the Doldenhorn and Blümlisalp on its northern side. To the south the same portion of the main range is divided from the still higher parallel range whose summits are the Aletschhorn and the Bietschhorn by the Lötschental and the Lötschenlücke. To this again succeeds the deep trench through which the lower part of the Aletsch Glacier flows down to the Rhone, enclosed by the minor ridge that culminates at the Eggishorn.

It is in the central and eastern portions of the range only that crystalline rocks make their appearance; the western part is composed almost exclusively of sedimentary deposits, and the secondary ridges extending through Bern and the adjoining cantons are formed of jurassic, cretaceous, or eocene strata.

ExplorationEdit

The beauty of the scenery and the facilities offered to travellers by the general extension of mountain railways make the northern side of the range, the Bernese Oberland, one of the portions of the Alps most visited by tourists. Since strangers first began to visit the Alps, the names of Grindelwald, Lauterbrunnen, and Interlaken have become famous. But unlike many other Alpine regions, which have been left to be explored by strangers, this region has been long visited by Swiss travellers and men of science. Among them were the brother Meyer of Aarau and Franz Joseph Hugi. They have explored most of the mountain ranges not very difficult of access, and, further than this, have attained most of the higher summits. In 1841, Louis Agassiz, with several scientific friends, established a temporary station on the Unteraar Glacier, and, along with scientific observations on the glaciers, started a series of expeditions. The works of Desor and Gottlieb Studer have been followed by several other publications that bear testimony to Swiss mountaineering activity. Notwithstanding the activity of their predecessors, the members of the English Alpine Club have found scope for further exploits, amongst which may be reckoned the first ascents of the Aletschhorn and the Schreckhorn, and the still more arduous enterprise of crossing the range by passes, such as the Jungfraujoch and Eigerjoch, which are considered amongst the most difficult in the Alps.

Jungfrau-Aletsch areaEdit

The Jungfrau-Aletsch area is located in the eastern Bernese Alps in the most glaciated region of the Alps. It was inscribed as a UNESCO World Heritage Site (Swiss Alps Jungfrau-Aletsch) in 2001 and further expanded in 2007. Its name comes from the Aletsch Glacier and the two summits of the Jungfrau and Bietschhorn, which constitute some of the most impressive features of the site. The actual site (after the extension) includes other large glacier valleys such as the Fiescher Glacier and the Aar Glaciers.

List of peaksEdit

The chief peaks of the Bernese Alps are:

GlaciersEdit

Main glaciers:

List of passesEdit

The chief passes of the Bernese Alps are: