ヴィーコデルガルガノ周辺のアトラクション＆必見スポット - トップ20

To see one of the most beautiful beech forests in the world.

Itineraries accessible to all...well signposted...relaxing landscapes

The Laghetto d'Umbra is a rainwater-fed lake. The turtles living here were released, but they seem to thrive here.

Don't miss, if you're in the Bosco Quarto, with its hornbeams and beech trees, the Ragusa Valley, formed by one of the numerous east-west oriented tectonic fissures that mark the Gargano promontory between the Umbra Forest and the area of San Marco in Lamis. It's very easy to cycle through and can be reached by anyone with a basic understanding of cartography and navigation, yet the impression is of being immersed in an environment profoundly removed from any human presence. On the southern slope, near Coppa del Giglio and Casa Natura, runs what was the line of a Decauville a century ago.

Fantastic view of Vieste and the rock. The beach is not really for me. More information about the rock: https://it.wikipedia.org/wiki/Pizzomunno?wprov=sfla1

A beautiful walk in the Umbra forest in the Gargano region that starts from Laghetto d'Umbra near Caserma dei Carabienieri Forestali and follows the path to Caserma Murgia. From here you can deviate a bit to visit the ruins and then return along the path to Lago d'Otri, a small lake in the Gargano forest.

auto_awesome Source language: Italian 887 / 5,000 The Pizzomunno rocky outcrop, which rises about 25 meters above the Castello beach, has the shape of an ellipse (20 x 12 meters) and is located at a distance of at least about 25 meters from the rocky wall of the San Francesco promontory, from which it cannot be overcome due to erosion phenomena. Marina, with the procedure of applying the original Tettonia fracture. Subsequently, the lighthouse is raised and proceeds with the lowering of a further modeling according to the chemical measures of the sea spray. The Pizzomunno and the lower part of the rocky wall are made up of white limestone of the “scaglia” type, dating to the Late Cretaceous period (145.5 years and 0.3 million years ago). It is a soil formation with slightly diametrically opposed white limestones, gradually stratified with a selection of red spots. The layers of the stone slab, with a thickness of 5 to 10 cm, have a northeast-southeast direction and an inclination of 13° to the northeast.

The famous and evocative white monolith that rises 25 meters from the sea, very close to the beach of Vieste.