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The Montenero di Bisaccia gullies, known locally as lame, are located behind the Sanctuary of the Madonna di Bisaccia. The area is characterized by erosive landforms that extend over approximately 120.8 hectares, creating a surreal landscape of deep valleys dominated by thin, jagged ridges.

Drinking water

Through the Calanchi of Montenero di Bisaccia

Morgia di Pietravalle or Morgia dei Briganti in Salcito Millions of years ago, while the most important mountain ranges in Europe were forming, the movements of the earth's crust brought to the surface large rocky spurs born in a marine environment: these are the famous Morge, monumental rocks rich in fossils.

Morgia di Pietravalle or Morgia dei Briganti in Salcito Millions of years ago, while the most important mountain ranges in Europe were forming, the movements of the earth's crust brought to the surface large rocky spurs born in a marine environment: these are the famous Morge, monumental rocks rich in fossils.

Designed in 1868 by Eng. D'Aloisio di Palmoli the Fontana Maggiore was completed in 1872 in the place where the urban expansion of Trivento had now begun. Initially surrounded by rammed earth, often described in nineteenth-century chronicles as a critical element for the inevitable creation of mud, the large public fountain served as a source of water supply for people and animals who, through the main road circuits, arrived or lived in the Trignino village.

From this stretch of the provincial road you can enjoy the view towards the village of Montenero di Bisaccia and the Calanchi di Montenero, an area of about 120 hectares, where there are erosive forms created by the action of rainwater on the clayey soil. The area is a site of community interest (SIC), identified by the Ministry of the Environment for its naturalistic and landscape importance.

From this stretch of the provincial road you can enjoy the view towards the village of Montenero di Bisaccia and the Calanchi di Montenero, an area of about 120 hectares, where there are erosive forms created by the action of rainwater on the clayey soil. The area is a site of community interest (SIC), identified by the Ministry of the Environment for its naturalistic and landscape importance.