Canal Cuna, the valley where time stands still, is crossed by the path 810 which connects Cai Tramonti di Mezzo and St. Francis de Vito d'Asio. The valley stretches from west to east for more than 4 km, in the upper basin of the river Comugna, flanked by mountains to a large, but rough, with a valley that slopes down from 750 to about 450msulmare. It has a typical profile "V" of clear river.
His performance was strongly influenced by the presence of important geological structures. The rocks outcropping in the channel of Cuna all belong to the formations of dolomite-Major, composed mainly of limestone and dolomitic limestone-white or gray, arranged in regular layered bedrock, bowed to the north with angles ranging between 30 and 60 °. Thanks to the discovery of some fossils could be
determine the age of the rocks related to the geological period called "late Triassic, between 220 and 210 million years ago.
The main peaks emerging from the mountain ridges that mark the limit of the river channel, are Mount Sciarra Grande (1686m.), the Spoleit This (1687 m.), the mountains Drea (1278 m.), Agarial (1189 m .) Giaf (1085 m.), Vence (1045 m.), Givoli (1029 m.), the tip Boscher 1110 m.), and the Zuc of Santins (1309 m). An internal short dorsal branches off southward from Cuesta Spolei Osel and culminates in the mountains (1338 m) and Rovoleit (1061 m). The valley is crossed
by steep watercourses, very striking for their clear waters. In addition to Comugna, the most significant are the culprits of CuAl boat, by Sachs, the Frari, and What to Giaveada of Stra. The Cuna
Canal is part of the municipality of Tramonti di Sotto and the first news of the valley date from the latter half of 1500, was used first as a seasonal dwelling shepherds of Tramonti di Mezzo, and later became a installation disk, divided into the nuclei villages of Mosareit, What diMasut, Pascalon, Morasit, Frari, Val Parmiedia, Deer, Piedigiaf, Chiaschiermes, and in the pasture for stavoli animals Sauvieit, Gardelin, and Giaveada Siriviella.
In 1870 it reached the valley the highest population growth, there were counted 170 people and 18 homes, but in 1944 the inhabitants were reduced to 61 and 14 fireplaces.
Due to the isolation (the valley is not reached by any driveway), in 1954 the last Cjianaglin left the valley, but the emotional bond with the descendants of the Canal Cuna remains very much alive.
Brief History In 1745
Pascalon town, was built a church dedicated to St. Vincent Ferrer.
1794 An earthquake of strong intensity destroying villages and causing four deaths. In the early years of the 800 locations in Tomb is built a water mill. The altar
1855 wood is replaced with a beautiful stone altar.
1880 A Nannini Morasit master teaches children in the valley. The church is loaded with a shovel by the painter Luigi Schiasutti Belluno.
1904 is founded "case workers" for savings.
1916 The school is regularly attended by 23 children. After the 1928 earthquake
Pascalon is built to the school.
1944 during a raid in Pidigiaf Cossack, were killed and Mrs Mary and Leonardo Lorenzini.
1954 Last Cjianaglin (inhabitant of the channel) leaves the valley.
1963 The bells are removed from the tower and take in Tramonti di Mezzo.
1975 May 1: Pro on site and the people of San Francisco initiates the tradition of the festival in the valley.
1 May 1993, a young local woman launched the idea of \u200b\u200bputting his hand to repair the church. Thanks to the contribution of the Mountain Community Meduna /
What / Arzino, municipalities and Vito D'Asio Tramonti di Sotto, with their respective Pro Loco Pro Associations Pordenone Pordenone and natural society "Silvia
Zennari, helicopters Casarsa , to 'Provincial ANA and a very active group of volunteers are natives of the surrounding valleys ended his recovery
of the church.
1995 May 1: Goatskin 700 people went into the valley to celebrate the completion of restoration work of the church.
1 May 2006: Pastoral Visit of His Excellency Bishop Ovidio Poletto.
1 May 2008: Presentation of the book in Menegon Canal Cuna.
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