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THE TERRITORY
"VALLE CAMONICA"

Valle Camonica takes its name from the Camuni, the ethnic group
populating it since remote times. It is located in the north-eastern
part of Lombardy, oriented to north-east/south-west, occupies an area
of 1347 square km and extends for 80 km in the typical elongated shape
of alpine valleys. It includes 46 municipalities, with a population of
114,000 inhabitants. Of these municipalities, four (Lovere,
Costavolpino,
Rogno and Castro) belong to
the province of Bergamo, while
the others are part of the province of
Brescia. Valle Camonica is practically
surrounded by mountains: to the north the
Rhaetian Alps with the
Ortles-Cevedale chain and the
Corno dei Tre Signori (3360 m); to
the south the Pre-Alps of the
Brescia area; to the east the
Adamello Brenta chain; to the west the
Alps of the Bergamo area
with the Pizzo della Presolana.
From a geological viewpoint
its history began in a period between 570 million and 1 billion years
ago: the most ancient rocks in fact date back to that era. These are
metamorphic rocks with a crystalline base. There are also sedimentary
rocks formed in a marine and continental environment and more recent
igneous intrusive rocks of the
largest batholith in Italy: the Adamello.
The lithologic heterogeneity that characterise
Valle Camonica makes it unique in
its kind and for this reason it is a study site for Italian and
foreign geologists.
The
quaternary glaciations succeeding each other until 11,000 years ago
were fundamental in defining the morphological aspect of the camunian
territory. The glacier, upon retreating, conferred on the valley its
typical “U” shape, its super-excavating activity brought about
morphological leaps, great steps that created the so called “hanging
or suspended valleys” with their spectacular high-altitude glacial
lakes, such as, for instance, the lake of
Aviolo (1930 m), the lake of
the Vacca (2357 m), the Baitone
lake (2249 m), the Salarno lake
(2070 m), but also, at more accessible heights, the
lake of Lova (1299 m) and the
Moro lake (600 m). Erosion on the
mountain and deposit in the valley by the glacier formed the morenic
amphitheatres, remains of which can today be observed at
Cislano (the pyramids of
Zone) and
Lozio.
Valcamonica is also extremely varied in terms of
climactic and vegetation strata,
ranging from the lower valley up to a maximum altitude of 3539 m of
the peak of the Adamello. The
vegetation, both floral and arboreal, is surprisingly varied
throughout the valley, with endemisms of beautiful plants rare to be
found in other places, monumental or multi-centenary trees and
peat-land vegetation linked to particular microclimates.
Valle Camonica
is especially rich in water: the river
Oglio that is born of the union of the water from the
Frigidolfo and
Narcanello streams, at
Pontedilegno, flows in its entirety through the valley into the
lake of Iseo. This is the fifth
Italian river in terms of length; it has many affluent rivers, fed by
springs and high-altitude lakes. Since 1900 the water has been
exploited for production of electric energy, and before then to move
the malls used for iron-works.
Agriculture
is not practised on a vast scale: in the wider areas there are
orchards of apple-trees, while wine growing is practised only
privately. Animal breeding too
is aimed at family needs. As a real economic activity we can only
mention cattle, goats and sheep, horses and pigs, used to make local
cheese and salt-meats. We also mention
typical products such as honey, grappa and liqueurs made with local
herbs.
Valle Camonica,
moreover, is valued for its natural
vocation to tourism.

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