Pizzo Camino
Pizzo Camino is a mountain in the Bergamo Prealps, with a height of 2492 metres (8,176 ft).

It belongs to the massif dividing the upper Val di Scleve from the upper Val Camonica
Val Camonica
Val Camonica is one of the largest valleys of the central Alps, in eastern Lombardy, about 90 km long. It starts from the Tonale Pass, at 1883 metres above sea level and ends at Corna Trentapassi, in the comune of Pisogne, near Lake Iseo...

, together with the Concarena
The Concarena is a massif in the Bergamo Prealps; its highest peak is the Cima Bacchetta, with a height of 2,549 m.The Concarena is the highest part of the range dividing the mid Val Camonica and the Valle di Scalve, lying at its north-eastern tip...

 and the Cimone della Bagozza
Cimone della Bagozza
Cimone della Bagozza is a mountain of Lombardy, Italy. It is located within the Bergamo Alps....

. It is on the boundaries between the provinces of Brescia
Province of Brescia
The Province of Brescia is a Province in Lombardy, Italy. It borders with the province of Sondrio in the N and NW, the province of Bergamo in the W, province of Cremona in the SW and S, the province of Mantova to the S, and to the east, the province of Verona and Trentino .Source for statistical...

 and Bergamo
Province of Bergamo
The Province of Bergamo is a province in the Lombardy region of Italy. It has a population of 1,098,740 , an area of 2,722.86 square km, and contains 244 comuni...


The summit is composed from limestone
Limestone is a sedimentary rock composed largely of the minerals calcite and aragonite, which are different crystal forms of calcium carbonate . Many limestones are composed from skeletal fragments of marine organisms such as coral or foraminifera....

 rocks, formed in the middle Triassic
The Triassic is a geologic period and system that extends from about 250 to 200 Mya . As the first period of the Mesozoic Era, the Triassic follows the Permian and is followed by the Jurassic. Both the start and end of the Triassic are marked by major extinction events...

 period from the former Tethys Ocean
Tethys Ocean
The Tethys Ocean was an ocean that existed between the continents of Gondwana and Laurasia during the Mesozoic era before the opening of the Indian Ocean.-Modern theory:...

. The lower sides have instead a more sandstone
Sandstone is a sedimentary rock composed mainly of sand-sized minerals or rock grains.Most sandstone is composed of quartz and/or feldspar because these are the most common minerals in the Earth's crust. Like sand, sandstone may be any colour, but the most common colours are tan, brown, yellow,...

Marl or marlstone is a calcium carbonate or lime-rich mud or mudstone which contains variable amounts of clays and aragonite. Marl was originally an old term loosely applied to a variety of materials, most of which occur as loose, earthy deposits consisting chiefly of an intimate mixture of clay...

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