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This process uses no organic solvents, and instead only water is used to decaffeinate beans. It is a technique first developed in Switzerland in 1933, and commercialized by Coffex S.A. in 1980. [6] The Swiss Water process was then introduced by The Swiss Water Decaffeinated Coffee Company of Burnaby, British Columbia, in 1988. [13]
Large quantities of water are present in the basement of Switzerland, and form a vast network linked to the geological structures. The underground lake of Saint-Léonard, located in Valais, with its 300 m long and 25 m wide is a notable example. Each year, one hectare of the Swiss plateau filter an average of four million liters of clean ...
In this process, solvent is added to moistened green coffee beans to extract most of the caffeine from the beans. After the beans are removed from the solvent, they are steam-stripped to remove any residual solvent. The caffeine is then recovered from the solvent, and the solvent is re-used. The Swiss Water Process is
Lake Cadagno in the Swiss Alps is a naturally meromictic alpine lake due to saline input from groundwater.. The annual cycle of stratification and mixing in lakes plays a significant role in determining vertical distribution of heat, dissolved chemicals, and biological communities. [12]
Occupying 25.5% of Swiss soil, these surfaces are in very slight decline (-0.1% over 10 years). They are predominant in the Central Alps (half of the soil), on the contrary they only cover 10% of the surface of the plateau and 1% of the Swiss Jura. The uncultivated mountain areas are exploited by the tourism and the production of hydroelectricity.
Satellite image of the Alps, March 2007 Folded rock layers exposed in the Swiss Alps. The Alps form part of a Cenozoic orogenic belt of mountain chains, called the Alpide belt, that stretches through southern Europe and Asia from the Atlantic all the way to the Himalayas. This belt of mountain chains was formed during the Alpine orogeny.
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