Bordano 주변의 최고의 자연 기념물은 산, 큰 자연 호수, 중요한 강으로 특징지어지는 이탈리아 프리울리 베네치아 줄리아 지역에서 발견됩니다. 이 지역은 다양한 나비 종으로 유명합니다. 방문객들은 빙하 호수부터 야생 강바닥, 산악 트레일까지 다양한 자연 환경을 탐험할 수 있습니다.
마지막 업데이트: 5월 16, 2026
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하이라이트 • 자연 기념물
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Great view of the river and the mountains, bridge without a bike path and with traffic.
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Cuc de Cros, panoramic point on the way down towards Montenars.
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To visit the nearby early Christian basilica.
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This stretch of the Tagliamento is very panoramic.
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The Tagliamento is 170 kilometres long, rises at the Mauria Pass in the province of Belluno, flows through Carnia, takes in the Fella from the Val Canale, enters the northern Italian plain at Gemona del Friuli and flows into the Adriatic Sea between Bibione and Lignano Sabbiadoro.
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Small lake with wonderful colours, at the foot of rocky cliffs which are home to colonies of griffon vultures which can easily be seen circling in the sky above us.
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Very beautiful panoramic point, with the clear air you can glimpse the glow of the sea!
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Lake Cornino is a small body of water that originated during the retreat of the ice, which occurred around 10,000 years ago. In this period numerous and impressive landslides occurred along the sides of the valleys, which were suddenly deprived of the support represented by the mass of ice itself. The current morphology is the result of one of these landslides. These waters are easily distinguishable from those coming from the Prealps by a chemical "trace" that distinguishes them: coming from the Tagliamento basin they are loaded with calcium sulphate obtained from the dissolution of the chalks that abound in its basin. Waters of different origins also reach the lake, coming from the Monte Prat plateau. The lake is just over 140 meters long and 8 m deep. It has neither tributaries nor emissaries, but the underground water circulation is such that it still allows rapid water exchange. Hence its particular transparency and the very low temperature variations (which generally fluctuate between 9-11 °C) over the course of the year. These characteristics allow it to be classified as an oligotrophic lake as it is poor in nutrients. The bottom is populated by green algae that form dense underwater meadows, while the rocks are colonized by blue algae. The scarcity of nutrients present and the low temperature of its waters significantly reduce the possibility of life within it. The fish fauna present is scarce and linked to the introduction of Cyprinids and Salmonids but the presence of the Crayfish is certainly interesting.
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