The area lies entirely in the Municipality of Perrero, between 1,796
and 2,856 meters above sea level; you can reach it by taking a military
carriage road leaving from SP road Val Germanasca and heading to Lago
Lauson and then to Conca Cialancia: given the roadbed conditions, it is
recommended to use an all-terrain vehicle.
The name of the Park
comes from the local dialect "cialancio", meaning landslide. If you
visit the place, you will understand the reason for this name: the
whole valley is furrowed by several gullies leaving material in any
season, continuously changing the shape of the territory. The area
houses some summer grazing lands which are still used in the summer as
pastures. The typically alpine vegetation includes green alders,
mountain ashes, and several herbaceous species like the Twoflower
Violet, the White Hellebore, the Common Wood Sorrel, and the Common
Lady's-mantle. At higher altitudes there is the acidophilus sub-alpine
willow grove together with wonderful pioneer species like saxifrages,
the Bavarian Gentian, the Alpine Rock-Jasmine, and the Glacier
Crowfoot. As far as fauna is concerned, the area is populated by the
typical ungulates of the Alps (chamois, wild goat, deer, and roe deer),
the mountain hare, the fox, the ermine, the partridge, the black grouse
the rock partridge, the snowfinch and many others. Among the
amphibians, there is the large alpine salamander, an endemic species of
Alpi Cozie, which adapted to the high-mountain environment delivering,
unlike the other amphibians, entirely developed babies.
Conca Cialancia, like the whole Val Germanasca, is situated in a central position in the western alpine chain and is part of Dominio Pennidico, which is divided in the following units:
Val
Germanasca includes sections of the Dora-Maira Massif and the
Piemontese Area (or Calcareous Schist Complex with green stones).
The
massif Dora-Maira extends from Val Susa in the north to Val Maira in
the south, has an elliptic shape bordered in the east by the Quaternary
deposits of pinerolese and cuneese plain and in the west and in the
north by the Calcareous Schist Complex with green stones. It is divided
into two structural units: the lower one is formed by metasediments of
permo-carboniferous origin which probably covered an ancient rise,
whose evidences can be found in the rests of the upper unit, formed by
polymetamorphic schists with marbles and metabasites. Moreover, in both
units there are gneiss rocks and metagranitoid rocks with chemism
varying from granitic to tonalitic and dioritic. There are also
discontinuous and reduced stretches of a Mesozoic covering.
Piemontese
Area is a very complex geological unit involving the whole western
alpine chain. Also called Calcareous Schist Complex with green stones,
it is formed by metasediments deriving from impure carbonate rocks,
arenites, pelites, and radiolarites of Mesozoic age with metabasite and
metaultrabasites associations of oceanic crust or under oceanic mantle.
As far as superficial (quaternary) formations are concerned, they are
dominated by pluvial-colluvial deposits; however, they are also
characterized by interesting examples of glacial deposits which have
sometimes preserved associated morphologies, like morainic cords or
snow moraines in the high-mountain deposits.
The fauna we can sight in Conca Cialancia protected area is typical of the alpine environment. Among the most significant animals, we can observe:
As far as vegetation is concerned, the area of Conca Cialancia is characterized by features which are typical of the alpine environment situated above the limit of the arboreal populations and belongs to the climax of the prostrate shrubs and mountain steppes. It has various kinds of vegetal covering: shrubby, herbaceous, and more rarely arboreal covering.
Sub-level ares with a high humidity degree are characterized by shrubby populations dominated by green alder (Alnus viridis); they are thick coenoses linked to the soil humidity and the long permanence of snow, as well as to the mechanical effects of snowslides. In the areas where the alder has recolonized ancient pasturelands, it is associated to other pioneer broadleaf trees like the European mountain ash (Sorbus aucuparia), preparing the soil to the future entrance of the conifers. In general, we can state that pure alder populations defend the highest slopes from erosion and play an important role in the protection of wildlife (black grouse, ungulates) where they alternate with meadow-pasture areas dominated by herbaceous species like the Twoflower Violet, the White Hellebore, and the Common Lady's-mantle.
The highest areas of the Park, characterized by rocky features and humidity, as well as abundant and prolonged snowfall, are covered with acidophilous sub-alpine willow groves dominated by Salix elvetica and Salix glaucoserica, growing together with pioneer species like saxifrages, the Bavarian Gentian, the Alpine Rock-Jasmine, and the Glacier Crowfoot.
The lower altitudes are characterized by ilex tree woods (Larix decidua) on rhododendrons-bilberries and pastures near Alpe Lauson and Alpe Cialancia. Where the rhododendron covering under the ilex tree is reduced, the conditions of the turf are good: in particular, around the summer grazing lands, the flora is dominated by precious graminaceous and leguminous plants of great value. The ilex tree woods are also characterized by areas with outcropping rocks along the ridge or on high slopes, giving them a characteristic natural and aesthetic-landscape mark. Large areas, in particular those above Alpe Lauson and those situated in the basin crossed by rio Cialancia, are covered by rhododendron, sometimes associated with bilberry, bog blueberry, and alpine azalea with in late summer-autumn give these areas a characteristic purple red color.