마지막 업데이트: 2월 22, 2026
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하이라이트 • 자연 기념물
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하이라이트 • 자연 기념물
번역자 Google •
팁에 의해
하이라이트 • 자연 기념물
번역자 Google •
팁에 의해
Google 검색 결과에서 komoot을 선호하는 출처로 추가하세요.
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One of the most suggestive points of the slope. The boulder on the edge of the path (called split stone) is really impressive.
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The melilitolite of Prete della Scimmia (1km north of Lago Piccolo of Monticchio) is characterized by phenocrysts of melilite (rich in Åkermanite) and titaniferous clinopyroxene immersed in a holocrystalline groundmass composed of melilite, clinopyroxene, magnetite, leucite, nepheline, apatite and garnet
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Its woods, consisting mainly of beech, chestnut and Turkey oak, represented the hunting reserve of Frederick II of Swabia. Later, the same woods were a shelter for brigands led by the famous Carmine Crocco.
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Lago Grande and Lago Piccolo lie, at about 650 meters above sea level, on the crater of Monte Vulture, an extinct volcano. Their greenish waters, separated by a thin line of land, are surrounded by lush forests of beech and oak.
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These beautiful lakes are located at the foot of the now extinct Vulture volcano. The beauty of this place has earned it the nickname of "Switzerland of Basilicata". The lakes are located within the Vulture Regional Nature Reserve.
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Artificial basin set in the Campania Apennines at 460 m above sea level. It receives its water from the Osento stream that originates in the Lacedonia area and has a fair flow of water, especially in winter. In the sixties, the Capitanata di Foggia decided to build this reservoir to allow the collection of the torrent waters, and then put them in the riverbed during drought periods, to be used for irrigation purposes in the lands of the nearby Puglia. The artificial reservoir has a maximum full capacity of 17,100,000 cubic meters and is delimited by the municipal boundaries of Monteverde, Aquilonia and Lacedonia, all common members of the Alta Irpinia Mountain Community. Lake San Pietro or Aquilaverde (i.e. Aquilonia - Monteverde) today is a place of peace and rare beauty due to the very green crown of the surrounding pine forests and is a wetland affected by the passage of migratory fauna. Only the large dam makes us remember that we are on the banks of an artificial basin. In the part closest to the access road, the bank is low and slopes gently into the water; the other bank is characterized by large rocky walls, dominated by abundant vegetation. A large picnic area develops along the north-east side of the lake
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