サンタマリアデルヴァルには 8
の息を呑むほど美しい峡谷があります。以下に紹介する必見の峡谷一覧に掲載されている写真、おすすめ情報、その他のデータを参考にして、次の冒険でサンタマリアデルヴァルの美しい峡谷を訪れる際に役立てましょう。
最終更新日: 4月 20, 2026
ハイライト • 構造物
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ハイライト • 自然記念物
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ハイライト • 峡谷
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役立つ情報 は によるものです
ハイライト (セグメント) • トレイル
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In the Cliffs of this Barranco del Hocino, in addition to its impressive appearance, there is a Via Ferrata where climbers secrete all their adrenaline.
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On the right bank of the Escabas River, it is a narrow pass between rocks. To make the road they had to drill a large mouth in these rocks.
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The Gate of Hell is one of the tunnels excavated in the rock of the Escabas River. One of the many obligatory stops available in the upper Serranía de Cuenca. Be very careful when taking photos, the road is very narrow.
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Steep and technical climb to exit the Cuervo River canyon towards the town of Carrascosa while avoiding following the course of the river. The bike may have to be pushed. With spectacular scenery, it is worth not being discouraged by the route and enjoying the surroundings.
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The Gate of Hell is one of the tunnels excavated in the rock of the Escabas River. One of the many obligatory stops available in the high mountains of Cuenca. Be very careful when taking photos, the road is very narrow.
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In order not to backtrack from the beautiful Embalse del Molino de Chincha to Puente de Vadillos, on the route to Beteta, you have to cross the nature reserve above the Chincha dam. The steep climb along the Barranco del Hoyo follows a faint single track path, barely visible due to a small landslide at the beginning of the climb. This is a tough hike-a-bike where you have to carry your bike over some steep rocky sections. Only try this at day time in good weather. At night or in wet weather this can be quite dangerous.
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A spectacular river canyon, a beautiful and unique place. They are approx. 6 kilometers of cliffs over 80 meters high, created by the waters of the Guadiela River.
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Considered a Natural Monument, the Torcal de Lagunaseca is made up of several torcas, gigantic depressions in the ground that can measure between 30 and 500 m in diameter. At first glance they give the impression of having been formed after the impact of a meteorite, but the truth is that they are formed naturally by wind and water erosion given the particular conditions of the terrain.
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