周辺の天然記念物・トップ20
シエラスサブベティカスが誇る美しい風景を見てみたいなら、シエラスサブベティカスの素晴らしい天然記念物・トップ20
に行ってみましょう。あなたにぴったりの場所が見つかるよう、素晴らしい天然記念物を探索するために必要なすべての情報を集めました。次のアウトドアの冒険に出かける計画の参考にしましょう。
最終更新日: 2月 22, 2026
コウモリの洞窟
ハイライト • 洞窟
翻訳者 Google •
役立つ情報 は によるものです
チョレラス・デ・ラ・フエンセカ
ハイライト • 滝
翻訳者 Google •
役立つ情報 は によるものです
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バイヨン渓谷の石灰岩の地形と洞窟
ハイライト • 渓谷
翻訳者 Google •
役立つ情報 は によるものです
ナバ・デ・カブラのポルジェ
ハイライト (セグメント) • 自然記念物
翻訳者 Google •
役立つ情報 は によるものです
コミュニティからのヒント
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.
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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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