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마지막 업데이트: 3월 2, 2026
추레라스 데 라 푸엔세카
하이라이트 • 폭포
번역자 Google •
팁에 의해
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바일론 협곡의 석회암 지형과 동굴
하이라이트 • 협곡
번역자 Google •
팁에 의해
나바 데 카브라 폴예
하이라이트 (구간) • 자연 기념물
번역자 Google •
팁에 의해
라스 초레라스 폭포
하이라이트 • 폭포
번역자 Google •
팁에 의해
무료로 가입하여 시에라스 수베티카스의 더 많은 자연 기념물을 발견하세요.
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커뮤니티 팁
It is a prehistoric cave, the largest in the province of Córdoba, declared a Natural Monument in 2001. Its name comes from the bats, of different species, that inhabit this cave. In his tourist visit, a descent of up to 65 m deep is made.
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It is a prehistoric cave, the largest in the province of Córdoba, declared a Natural Monument in 2001. Its name comes from the bats, of different species, that inhabit this cave. In his tourist visit, a descent of up to 65 m deep is made.
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Seasonal waterfalls that appear after copious rains. Due to the porosity of the terrain, only when the amount of water is greater than what the terrain is capable of absorbing, do waterfalls form, sometimes even making it difficult to pass and not being able to make the route in a circular way. It is convenient to inquire at the Santa Rita Visitor Center about their status and check if an authorization is required to visit them, which is sometimes established to control the influx of people to this Zone A Reserve of the Protected Natural Area.
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A poljé is a large, elongated, flat valley-shaped depression in an area of karst rock. It is formed after a subsidence of the land in which water often stagnates seasonally. In this case, the Bailón river has produced a drainage of it, and in 2012 a pónor also arose through which the poljé drainage also occurs.
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This trail is full of impressive limestone rock walls, with a multitude of vegetation sprouting between its numerous pores. They have been formed over time by the force of the Bailón River. From some angles you can see Zuheros and its castle peeking out between the walls.
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This cave is a system of galleries typical of limestone formations, very porous. Its name is due to the fact that various species of bats inhabit it.
•2
0
A poljé is a large, elongated, flat valley-shaped depression in an area of karst rock. It is formed after a subsidence of the land in which water often stagnates seasonally. In this case, the Bailón river has produced a drainage of it, and in 2012 a pónor also arose through which the poljé drainage also occurs.
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