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最終更新日: 2月 26, 2026
ハイライト • 山小屋
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ハイライト • 湖
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ハイライト • 展望台
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ハイライト • 山小屋
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ハイライト • 山小屋
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Martinsmadhütte is an Alpine hut located at 2,002 metres above sea level in the Glarus Alps, above Elm in the canton of Glarus, Switzerland. Built in 1907 and expanded in 1938, the hut is operated by the Randen section of the Swiss Alpine Club (SAC) and offers 48 beds during the summer season. It is an ideal starting point for hikes in the UNESCO World Heritage Site of the Tektonikarena Sardona. Access to the hut can be facilitated by using a small cable car up to the Nideren Alp, followed by a hiking trail. Facilities include a breakfast buffet, but there are no showers; a stream behind the hut offers an option for cooling off.
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A beautiful hike through the Flims forest to Il Spir at any time of year
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A lovely, authentic hut with a dormitory and very friendly hosts. The daughter played the accordion and yodeled in front of the hut after dinner. It was a special treat for the guests. There's a barefoot path behind the hut where you can refresh your tired feet. Chamois and ibex can also be seen on the mountain in the mornings and evenings.
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From the small viewing platform at the "mountain station" you have the most beautiful view of the lake.
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This is actually the best place to see the lake from above. Since it is in the middle of the forest, there are too many trees on most hiking trails that prevent a broad view of the lake. On the shore of the lake, the colors often look different again, depending on the time of day and the lighting conditions.
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Lake Cauma, the Pearl of Flims Called "Lag la Cauma" in Romansh, which means "Lake of Midday Rest," Lake Cauma is the pearl of Flims. Origin This mountain lake was formed as a result of the largest landslide in the Alps, which occurred almost 10,000 years ago. The formation of the lakes is attributed to prehistoric landslides. The water seeped through the porous rockslide masses. However, it can also dissolve the limestone with the help of its carbonic acid. Over time, it created an underground passage. A deeper, impermeable clay layer ensures that the water does not completely seep into the ground. Text / Source: Flims Laax Falera https://www.caumasee.ch/geschichte/
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