비톤토‬에서 가장 멋진 ‪3‬개의 협곡

Ruvo di Puglia 지역의 Il Canale del Pidocchio는 최종 구간에서 비포장도로가 되어 시골 풍경에 완벽하게 통합되는 'Ferrata' 시골길을 따라 도달할 수 있으며, 해발 500미터 이상의 고립되고 매혹적인 곳입니다. 경로를 둘러싼 석조 벽은 고대 농경지 구분을 증언하며, 종종 오늘날 부분적으로 폐허가 된 건초 더미나 석조 축사로 장식되어 있어 기존의 대토지 소유 시스템의 기억을 보여줍니다. 오늘날 일부 구간은 경작 작업으로 인해 끊어진 바위가 많거나 포장된 비포장 도로인 특징적인 'carrari'를 통과하면 완전히 석조로 지어진 매혹적인 석조 다리에 도달합니다. 부분적으로 폐허가 되었지만 역사적으로 중요한 작은 건축 보석으로, 이곳에서 경로는 Il Canale del Pidocchio의 넓은 전망을 제공하며 끝납니다.

Spectacular sinkhole of karst origin among the highest altitudes of this tour

The Pulo di Altamura is a sinkhole of karst origin of the bowl type, created by the channeling of rainwater right at this point. This created a more or less circular depression with a diameter of about 500 m. with a maximum depth of 75 meters. Along the walls, which are very steep in some points, caves and ravines have been created which indicate the different levels of excavation by the waters. These caves represent a real archaeological heritage because they were inhabited since the earliest ages of prehistory. The route includes an unpaved stretch of about 1 km that can also be easily covered by racing bike.

One of the most beautiful naturalistic places in Puglia. The view is breathtaking from every perspective; it can be easily reached by MTB. It is preferable to explore it on foot due to the cavities dug in the ground and the considerable presence of stones that make the MTB experience quite impervious.

karst dolina https://it.wikipedia.org/wiki/Pulicchio_di_Gravina

The Pulo di Molfetta is a characteristic karst collapse sinkhole located about 1.5 km from the center of the city of Molfetta, in a south-west direction, created by the collapse of the vault and dividing walls of one or more caves and tunnels formed starting from distant geological times and forming part of a complex karst system consisting of the confluence and intersection of several karst wells which originated precisely in that place from a series of geological coincidences.

Pleasant than 100 meters from the border that divides Palo del Colle from Toritto, after having traveled an ancient rural road that crosses the Mangiaquero district, in the rocky ridge that flanks the medium-low part of the blade that leads the torrential waters from the Murgia to the Adriatic Sea, find the door that leads to the large atrium of the Grotta di San Martino. Our ancestors used to call the cave, or rather the caves, with the name of the Grutt di Mangiaquair, but it is ascertained that the caves are located in the Torittese territory, even if the direction that the access passage to the caves and the subsequent path takes, is they move towards the territory of Palo. The cave of San Martino, of calcareous origin, opens on the low reliefs of the Murgia, at 287 meters above sea level and is a site linked to karst phenomena of considerable historical and archaeological importance.

Not far from Altamura, in the middle of the Alta Murgia Park, opens what looks like a deep chasm. This is the Pulo, a veritable sinkhole of karst origin created for convey rainwater, the largest in the entire park and one of the largest in Italy. Over the years, the waters have carved a shaped depression on the karst rock more or less circular. Along the walls, in some very steep points, the Pulo is characterized by the presence of caves and ravines, a real archaeological heritage as they have been inhabited since the most ancient ages of prehistory.