폭포에서 숨 막히는 절경을 감상하고 싶나요? 그렇다면 라 가리가에 있는 아름다운 폭포 12
개를 살펴보세요. 아래에서 여러 폭포 사진과 팁을 살펴본 후에 마음에 드는 폭포를 다음 모험 계획에 간편하게 추가해보세요!
마지막 업데이트: 3월 5, 2026
하이라이트 • 역사적 장소
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하이라이트 • 강
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하이라이트 • 강
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하이라이트 • 폭포
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이미 komoot 계정이 있나요?
The Centelles streams are short, but with a considerable gradient, which gives rise to these beautiful waterfalls and pools. In 2008, work began to restore the Centelles area and its tributaries of the Congost River. The area includes restoring paths, replanting native trees, and cleaning up illegal dumps. Thus, restoring all of Centelles' natural beauty.
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Beautiful path that follows the course of the stream, it even has a small waterfall.
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This is a relatively large waterfall that is beautiful when water is flowing. Even when it's dry, it's worth visiting.
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Located in the Montsenyen half of the municipality, included in the Montseny Natural Park, it covers a large part of the Vallcàrquera valley, drained by the stream that bears the same name, at the foot of the Tagamanent hill. It runs along the southernmost slope of the Vall de Vallcàrquera to cross the tramuntana side at the Pont de la Font del Molí, and descend more or less steeply to Can Bosc to end up flowing into the Gorge in the section known as the creek The Vallcàrquera valley is a territory with a humid Mediterranean character where the vegetation is basically coastal and mountain oak. Despite this, the accentuated relief and the geological diversity of the municipality, together with the several permanent watercourses, have made Figaró one of the municipalities with a diversity of the most remarkable plant communities in the Vallès.
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The Bosc Negre torrent is the most important of the water courses that lead to Sot del Bac, where the Salt del Prat stands out, where a magnificent horse's tail manifests itself in the most generous periods of water of about 30 meters height, and goes to deposit the water in the gorge of the Bac, the surplus continues its course until the confluence with the river Congost, next to the Figaró. You can see how Travertine has been formed by the action of water on the rock.
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