周辺の天然記念物・トップ20

A very special alleyway on the way to or from the Tell Chapel. It's paved with large stones that require sure footing. Large stones along the sides are covered in moss, offering hikers a unique experience.

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If you're already in the area, you should definitely come here. An idyllic spot not far from civilization. Wagenmoosweiher is an artificially created lake in the Meggerwald forest, within the municipality of Udligenswil in the canton of Lucerne. It's located in a forest clearing at an altitude of 597 meters above sea level. The lake is surrounded by reeds. On the western shore of Wagenmoosweiher, you'll find a lovely picnic area with a barbecue and a water fountain.

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If you haven't had enough of hiking, you can do some exercise in between.

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The pond lies in the heart of the Lower Forest nature reserve, surrounded by various fens. A fen in a nature reserve is a damp, often boggy area, usually found in river valleys, near lakes, or in depressions. It is a special habitat characterized by high biodiversity and sensitive ecological conditions. The vegetation often consists of reeds, sedges, rushes, rushes, and other wet meadow plants. It provides a habitat for many endangered animal and plant species.

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Idyll in the middle of the forest

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https://erlebnis-geologie.ch/geoweg/gletscherspur-seebodenalp/ Route The starting point for the gently undulating panoramic trail is the granite boulder on Chrüzegg, also known as the "Albert Heimstein." On the hiking trail to Ruodisegg, simply follow the information boards on various topics or walk along the tree-lined avenue to the Hinterboden junction. At Färbersegg, leave the path to Ruodisegg, cross the field path, and then hike through the fascinating nature reserve. Now follow the signs until just before the Hinterboden mountain inn and begin the short climb through the forest forest toward Holderen. At Alp Holderen, the descent across the alpine meadows begins, or you can take the field road back to Seebodenalp.

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https://seebodenalp.ch/gletscherspur/ The last great ice age reached its peak around 1,321,000 years ago. Mount Rigi was surrounded by the Reuss Glacier, which extended far into the Swiss Plateau and left clear traces. At that time, a thick layer of ice lay in the valleys surrounding Mount Rigi. Large quantities of debris and boulders (erratics from the Gotthard Massif) were carried from the upper Uri Reuss Valley into our region. Information panels are located at various locations. They provide information about the history of the Seebodenalp glacial landscape and about changes that have occurred over the centuries due to human or climatic influences. Other topics include current forms of management on Seebodenalp, nature conservation and biodiversity, and landscape design.

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Our beautiful city of Zug and Lake Zug😁

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