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마지막 업데이트: 4월 8, 2026
하이라이트 • 산장
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랍비 하이킹
랍비 로드 사이클링 경로
Quite a difficult route but beautiful views of the Cevedale group
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Monte Cevedale is a symbolic mountain of the Ortles-Cevedale group, 3,769 meters high. It establishes the border between Lombardy and Trentino-Alto Adige. To reach its summit you need good preparation and the ability to move in alpine environments.
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The approach to the summit cross is somewhat exposed in winter past a wire entanglement. It may be necessary to unbuckle.
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The descent from Cevedale is the only part you need to pay attention to, you need to get off early to avoid risks
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In my collection of the highest "hiking peaks" of every Alpine country, Monte Vioz has replaced Rocchiamelone (and Punta Rossa del Grivola) for Italy. A higher peak that can be reached "hiking" [for me that means without glacier equipment and with a maximum of short, not too exposed climbing sections in the 1st degree] should not be found anywhere in Italy [if you know one, please message me! 🙂]. For my criterion, the only option was to leave the valley without a cable car, since it's almost 2,000 meters of ascent and descent. In addition, I wanted to take the Punta Linke with me as the 19th peak over 3500 m [in the meantime there are 21 😉]. At the end of September, the cable car and hut were already closed, but in good weather the summit could still be (almost) snow-free. Although you always have to be aware that there can be a lot of snow at this height, even in midsummer - the much-cited "alpine experience" is always recommended, despite the comparatively easy path (T3+) for the height.
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The summit is only about 100 m above the hut. The summit cross is a little further ahead of the highest point. While the view to the south was already comparable from the hut, it now opens up over wide glacier areas to the north and to the Palon de la Mare.
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Easy summit reachable via an easy path and ropes in the most exposed points. Important difference in height. Panorama on the Forni valley and its glaciers.
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When the snow melted in spring, the residents of the Martell Valley had to expect that the meltwater would suddenly pour out beneath the glacier (today it is only a shadow of its former self) and cause the Plimabach to swell to such an extent that severe flooding would occur further down in the valley . It was then decided to build a simple dam that would allow the residents to drain the meltwater in a controlled manner. This meant that the risk of flooding in the lower Martell Valley was largely averted.
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