4.6
(16344)
78,824
등산객
17
하이킹
Langenegg 주변의 하이킹은 700미터 고도에 위치하며, 완만한 언덕, 울창한 초원, 빽빽한 숲을 포함한 다양한 풍경을 제공합니다. 이 지역은 그림 같은 브레겐처아흐 계곡(Bregenzerache Valley)을 특징으로 하며, 강으로 이어지거나 강을 따라가는 많은 트레일이 있습니다. Langenegg는 또한 "Nord" 자연 보호 구역 내에 잘 보존된 습지대를 보유하고 있으며, 고산 초원과 독특한 지질학적 특징으로 유명한 나겔플루케테 자연 공원(Nagelfluhkette Nature Park)의 일부입니다.
마지막 업데이트: 4월 3, 2026
4.7
(19)
99
등산객
3.90km
01:07
90m
90m
초급용 하이킹. 모든 체력 수준에 적합. 실력과 관계없이 누구나 쉽게 갈 수 있는 길.
4.9
(8)
31
등산객
7.13km
01:59
140m
140m
초급용 하이킹. 모든 체력 수준에 적합. 실력과 관계없이 누구나 쉽게 갈 수 있는 길.
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4.7
(15)
61
등산객
17.1km
05:23
590m
590m
어려운 하이킹. 우수한 체력 필요. 대부분 갈 수 있는 길. 미끄러지지 않게 조심해야 함.
3.7
(6)
33
등산객
7.28km
02:12
230m
230m
보통 하이킹. 좋은 체력 필요. 실력과 관계없이 누구나 쉽게 갈 수 있는 길.
7
등산객
2.70km
00:44
40m
40m
초급용 하이킹. 모든 체력 수준에 적합. 실력과 관계없이 누구나 쉽게 갈 수 있는 길.
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The Baroque church, a listed historical monument, dates back to 1722 according to its keystone. The builder is believed to have been one of the masters of the Bregenzerwald school of architecture. Constructed from tufa stone, the chapel, with its Greek cross shape, is a unique structure in the entire region and has undergone several thorough renovations, most recently in 1968 and 1990. The ceiling frescoes, created in 1968 by the Schruns artist Konrad Honold, depict individuals who were either born in Vorarlberg or who worked there. Among them was Vorarlberg's first diocesan bishop, Bruno Wechner. The altarpiece portrays Saint Anne.
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A particularly beautiful natural monument is the tufa slope in Lingenau. It is one of the most magnificent travertine formations in Europe north of the Alps and thus one of the most outstanding geological features in Vorarlberg. Here, spring water plunges over a roughly 40-meter-high escarpment, approximately 30 meters wide, into the Subersach Gorge. The conglomerate rock outcrop, visible in some places, is partially covered by several meters of travertine and spring tufa. On the overhangs, mushroom-shaped layers of travertine have developed into stalactite-like canopies. At the base of the rock face, the water collects in several travertine pools. Beneath the waterfall, the calcareous water encrustes the slope down to the Subersach River. Plant and animal remains are covered and encrusted by the lime. After the organic matter dissolves, an exact imprint (fossils) remains. The resulting porous, sponge-like rock is called travertine, the denser form being travertine.
6
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A rather small statue of Mary, standing in a rock hollow in the tufa spring.
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A particularly beautiful natural monument is the tufa slope in Lingenau. It is one of the most magnificent travertine formations in Europe north of the Alps and thus one of the most outstanding geological features in Vorarlberg. Here, spring water plunges over a roughly 40-meter-high escarpment, approximately 30 meters wide, into the Subersach Gorge. The conglomerate outcrop, visible in some places, is partially covered by several meters of travertine and spring tufa. On the overhangs, mushroom-shaped layers of deposits have developed into stalactite-like canopies. At the base of the rock face, the water collects in several travertine pools. Beneath the waterfall, the calcareous water encrustes the slope down to the Subersach River. Plant and animal remains are covered and encrusted by the lime. After the organic matter dissolves, an exact imprint (fossils) remains. The resulting porous, sponge-like rock is called travertine, the denser form being travertine.
8
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Long wooden stairs provide access to the tufa spring. The steps can be a bit slippery after rainfall.
8
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A particularly beautiful natural monument is the tufa slope in Lingenau. It is one of the most magnificent travertine formations in Europe north of the Alps and thus one of the most outstanding geological features in Vorarlberg. Here, spring water plunges over a roughly 40-meter-high escarpment, approximately 30 meters wide, into the Subersach Gorge. The conglomerate outcrop, visible in some places, is partially covered by several meters of travertine and spring tufa. On the overhangs, mushroom-shaped layers of deposits have developed into stalactite-like canopies. At the base of the rock face, the water collects in several travertine pools. Beneath the waterfall, the calcareous water encrustes the slope down to the Subersach River. Plant and animal remains are covered and encrusted by the lime. After the organic matter dissolves, an exact imprint (fossils) remains. The resulting porous, sponge-like rock is called travertine, the denser form being travertine. Tufa is a light, porous rock that is easy to work. It has proven itself in the past as a building material – especially for stables and vaulted structures. Tufa was used in the construction of the nearby Baroque St. Anna Chapel, which dates from 1722.
6
0
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