ゲーフィスでののおすすめウォーキング＆ハイキングルート

Nice place to grill and relax

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Unfortunately currently (May 2024) closed due to rockfall

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Wonderful single trail👍

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Not easy to find, but definitely worth a try.

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Always nice with the view of the Swiss mountains

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Niederes Kantenle 583 m / viewpoint Kanzelweg a scenic circular hike Short description: The Kanzele is a wonderful vantage point over the roofs of Feldkirch, which can be reached on a beautiful hiking trail that starts right near the town. Text / Source: Bergfex.at https://www.bergfex.at/sommer/vorarlberg/touren/wandel/54799,hohes-und-niederes-kaenzele-feldkirch--eine- outlooksreiche-rundwandel/

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Göfi's brother level 688 m

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Säntisblick 713 m, Göfis With fantastic views of the Alpstein Mountains with the Hoher Kasten, Saxer Lücke, Kreuzberge and also the Säntis as well as over the Rhine Valley to Lake Constance.

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Glacier pot, Göfis NATURAL MONUMENT GLACIER POT A special natural monument is the glacier pot discovered during construction work on the Amberg motorway tunnel. The mighty glacier pot with the 'glacial eggs' was professionally uncovered and made accessible to the public. It was created in the last ice age, when the surface of the Ill glacier was still 1,800 meters above sea level. The glacial meltwater rushed down the crevasses, reached the rocky subsoil and had an eroding and eroding effect. Text / Source: Göfis Municipal Office https://www.goefis.at/natur-kultur/naturdenkmal-gletschertopf/

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Nice place above Rankweil

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The high saddle is a mountain above Feldkirch and Göfis. According to the coordinates it must be this stone. With a little imagination it can look like a saddle.

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Cool itinerary. Drive carefully

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is a very nice yard

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A wonderful hike to the Säntisblick, also with children and dogs. The view over the Rhine Valley to Lake Constance is simply fantastic 😃

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(+_+)*\0/*(+_(+_+)=-O8-)8-)8-)8-):-|:-P+)

Nice viewpoint with a view of Feldkirch and the Rhine Valley

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The surface of the Illgletschers was in the last ice age up to 1800 meters over the sea level. Splinter movements created cracks, through which the meltwater plunged to the bottom, where it eroded and eroded the ground. The glacier pot was shaped for several centuries. Rock blocks transported by the glacier repeatedly reached the forming glacier pot, were set in motion by the meltwater and thus formed into so-called glacier eggs.

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