20의 가르가노 국립공원가지 명소 & 주요 장소

놀라운 관광지. 이탈리아에서 가장 아름답고 유명한 만 중 하나입니다. 비냐노티카에는 캠핑장(캠핑 비냐노티카)과 레지던스(비냐노티카 비치 아파트) www.vignanotica.it가 있습니다. 바로 근처에는 도보나 자전거로 갈 수 있는 3km의 자연 산책로 "사랑의 길"이 있습니다. 캠핑장이나 아파트에 머물 수 있습니다. 바로 근처에는 시장, 작은 식당, 해변에는 장비 갖춘 비치 클럽이 있습니다. 또한 가르가노의 가장 아름다운 동굴을 보기 위해 카약을 대여할 수도 있습니다!

On Monte Calvo, it's best to ascend from the east by mountain bike, despite the numerous unnecessary stone steps that clutter the initial section. The trail, which descends west from the summit to connect with the Sentiero delle Anguille, would be less rideable and much more difficult overall.

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.

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.