Swiss Geography
Excerpts from "Switzerland",
© 1993 Kümmerly & Frey, Geographical
Publishers, Berne, Switzerland
Fascinating natural history
Close study of the origins
of Switzerland's landscape reveals a complex
development reaching far back and far down.
The 'superficial' impression is one of mainly
recent shaping be post Ice-Age streams and
rivers, landslides of earth and rock, Ice-Age
glaciers and rivers formed by their melting
ice. In addition to, and beneath, these
features with ages ranging from just a few
thousand to one hundred thousand years, the
basic foundation, which is some 500'000'000
years old in all, consists of mighty layers
dating from the Tertiary Period (e.g. molasse
in the Central Plain) and from the Mesozoic
Sea (e.g. limestone alps, Jura) as well as
even older mountain cores.
A landlocked, mountainous country on the
north-south axis
If one were to try to
capture in one word the essence of Switzerland
as a whole, it would surely be the word
'diversity' that would be the most
appropriate. More essentially, one could say
that overall it is this diversity which gives
Switzerland its unique identity. It is rare to
find so small a country encompassing such
scope, variety and individuality in its
national life and above all in its natural
features. 7Situated in southern central
Europe, Switzerland is first and foremost a
land of hills and mountains.
There is no direct access to the sea: the
nearest port to the south of the country being
Genoa, in Italy, 250 kilometres away.
Switzerland embraces the central part of the
Alps, with its four main passes - Grimsel,
Furka, St.Gotthard and Oberalp; here also
spring the sources of the Rhone and the Rhine.
The Swiss rivers, Ticino and Inn, also feed
the Po and the Danube, giving rise to its
popular description as the 'Fountain of
Europe'. Due to its central position,
Switzerland has been, throughout its history,
an important link in communications and
transport between northern and southern
Europe.
Some geographical data
Area:
|
41'293.2
km2 |
Maximum
North-South extent: |
220.1
km |
Maximums
West-East extent: |
384.4
km |
Highest
point: |
Dufour
Peak 4'634 m |
Lowest
point: Lago Maggiore (water level): |
193
m |
Highest
village: |
Juf/GR
2'126 m |
Lowest
Village: |
Ascona/TI
196 m |
Total
frontiers: |
1'881.5
km |
hereof
with Italy: |
741.3
km |
with
France: |
571.8
km |
with
Germany: |
362.5
km |
with
Austria: |
164.8
km |
with
Liechtenstein: |
41.1
km |
Geology
The geological structure of
Switzerland is complex. It forms part of the
Alpine arc which stretches almost 1'000
kilometers from Nice (Frenche Maritime Alps)
to Vienna (Austrian Alps). The Jurea and the
Central Plateau do not form part of the Alps
but their development and variety of shapes
have been very much affected by the Alpine
chain. Although the country boundaries stretch
as far as the upper Italian plateau in the
south and to the Black Forest byond the Rhine
in the north, the major regions of Switzerland
are, however, geologically speaking, the Alps
and Pres-Alps (60%), the Central Plateau (30%)
and the Jura (10%).
Plenty of rivers and lakes, thanks to
abundant rainfall as a general rule
Because of its central
position, Switzerland's weather is influenced
by the four main European air currents - from
the Atlantic, the eastern continent, the
northern sub-polar region and the
Mediterranean south. These external factors
and the varied relief of the country itself,
with its sudden changes from mountain to
plateau, give rise to many local and regional
microclimates which can be both unexpected and
quite remarkable.
In general, Switzerland has more rainfall than
most other regions in Europe, but the amount
of rain varies greatly from region to region.
The Glaciers
The Swiss Alps have more
glaciers than the rest of the range - some
3'000 km2 in all. The glaciers we see today
represent only a small part of the total area
covered by ice during the various glacial
periods, when almost the whole country was
glaciated. Although some glaciers are still
advancing the majority have been retreating
for the last hundred years or so.
Rivers
Switzerland forms part of
the three main continental river basins: 67.6%
of the country is drained by the Rhine into
the North Sea; the Rhone (18%), the Swiss
tributaries of the Po (9.6%) and the Adige
(0.3%) drain 27.9% of the waters into the
Meriterreanean. 4.4% flows via the river Inn
into the Danube and eventually into the Black
Sea.
The Lakes
The lakes are a very
striking feature of the Swiss scenery, indeed
it is possible to cross the whole country and
never be further than 15 kilometers from a
lake. There a quite a few main lakes like Lake
Geneva (582.4 km2), Bodensee (539 km2), Lago
Maggiore (212,3 km2).
But Switzerland also boasts
hundreds of smaller natural and man-made lakes
and reservoirs, mainly in the Alps.
More extensive nature and environmental
protection
The increase in population
in a relatively small country has created
tensions and conflicts between economic
necessity and efforts to protect natural
resources and cultural heritage. New
legislation concerning forests, which cam into
effect beginning of 1993, qualifies forests as
natural habitats. The total area of forest and
its distribution remains protected. If
permission is given for felling, an equal area
must be replanted with trees of equal
ecological value.
Fortunately, Switzerland has
so far been spared large-scale environmental
disasters, but steadily increasing pressure on
the Swiss environment has prompted the
preparation of more extensive environmental
protection measures. Further efforts are
indispensable, particularly in connection with
preventing air pollution.
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