우세다에 있는 멋진 협곡 4
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마지막 업데이트: 2월 25, 2026
하이라이트 (구간) • 트레일
번역자 Google •
팁에 의해
하이라이트 • 트레일
번역자 Google •
팁에 의해
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하이라이트 • 강
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하이라이트 • 협곡
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하이라이트 • 협곡
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When you walk along the Patones stream, it is impressive to see how a small channel, which dries up in summer, has been able to excavate such a deep and important ravine.
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This road, which connects the towns of Patones de Arriba and Patones de Abajo, was one of the only accesses to the slate town until the 1930s, with the construction of the narrow road. Through a limestone and slate ravine pierced by the Patones stream, the geological and landscape value of this path is indisputable. Being today one of the best ways to access Patones de Arriba due to restrictions on the use of private vehicles in the town, it is worth walking through this place and being enchanted by its colors and views.
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The Cañada de la Caleriza is a winding path that runs along the banks of the Lozoya River. This section coincides with the beginning of the GR 88, which runs through the provinces of Madrid, Segovia and Guadalajara. The Lozoya is a tributary of the Jarama along whose 91-kilometer route six reservoirs have been built.
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This Martian landscape has been caused by strong water erosion on the clayey slope, forming these ditches that make up a science fiction landscape. It is also beautiful because of the surrounding environment, be careful and respect the signs, there are paths where it is forbidden to ride a bike so you will have to get off it.
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The climb is not easy but it is well worth it to admire these incredible natural formations. Next to which there is a small pine forest perfect for camping. There is no water or sources nearby, but before starting the climb next to the dam there is a beach bar where you can take supplies if you need them.
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The gullies are the sinkholes produced in rocks and soils of places with slopes due to the avenues of rainwater. These produce the so-called remounting erosion. They occur only in the clay-type substrate, if there are two or more gullies that advance parallel in a straight line, it is called rills.
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