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Cinque Vette Park

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Through Italy, World War I and World War II

Location

The Cinque Vette Park is situated within the domain of the Varese Prealps, the western section of the Lugano Prealps. It covers an area of 14 kilometers squared and it comprises the councils (comuni) of Cuasso al Monte, Marzio, and Valganna, all located within the Province of Varese. Approximately 85% of the park territory belongs to the council of Cuasso al Monte, 15% to the council of Valganna and 5% to the council of Marzio. The park features a variety of panoramic views and natural landscapes. The park is sponsored by Lega Italiana Protezione Uccelli. The surrounding area hosts important habitats and ecosystems, and for that reason it has become part of the Life TIB project, which includes the natural corridor that links the Alps and the Po Valley.

The park includes Lake Ghirla, Lake Ganna, and the Laghetto di Cavagnano. The last is a protected site (as Lake Ganna) due to the rare and endangered autochthonous fauna that inhabits the water. Adjacent to the park are Lake Maggiore and Lake Lugano.

Geological aspects

The territory of the park is classified as part of the Varesine Prealps, which are geologically significant and linked to the evolution of the Alpine Chain, which today appears as one complex structure with recognizable framed polyphasic tectonics deformations in the Plate tectonics model. The area of Mount Piambello is characterized by the presence of silicate rocks that originated about 290 million years ago from the multiple volcanic eruptions that took place in this area. In Valganna there are also deposits of travertine rock, locally called "Travertino della Valganna".

Climatic aspects

The park is located in an area characterized by high rainfall values, with strong variability in rainfall from one year to the next. From an analysis of the "isoiete" trend (closed curves that indicate areas affected by the same amount of precipitation), carried out between the years 1921 and 1972, a regular increase of the tendency of regional rainfall starting from the southernmost to the northernmost areas has been observed.
This is determined by the influence caused by the mountain ranges belonging to the Alpine arc, and by the influence brought by the Lake Maggiore, located a few kilometers West.

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