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카이스하임

카이스하임 주변 최고의 워킹 & 하이킹 경로

4.4

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정확한 경로를 찾는 것이 때로는 어렵지만 카이스하임에서 하이킹을 하면 다양한 경치를 마음껏 감상할 수 있답니다. 카이스하임에서 가장 멋진 하이킹과 워킹 중에서 마음에 드는 활동을 시작해보세요.

마지막 업데이트: 2월 18, 2026

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1. Leitheim에서 출발하는 Schloss Leitheim – 그라이스바흐 성 유적지 순환 코스

10.9km

03:01

200m

200m

보통 하이킹. 좋은 체력 필요. 실력과 관계없이 누구나 쉽게 갈 수 있는 길.

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초급용 하이킹. 모든 체력 수준에 적합. 실력과 관계없이 누구나 쉽게 갈 수 있는 길.

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초급용 하이킹. 모든 체력 수준에 적합. 실력과 관계없이 누구나 쉽게 갈 수 있는 길.

초급

초급용 하이킹. 모든 체력 수준에 적합. 실력과 관계없이 누구나 쉽게 갈 수 있는 길.

초급

초급용 하이킹. 모든 체력 수준에 적합. 실력과 관계없이 누구나 쉽게 갈 수 있는 길.

초급
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커뮤니티 팁

Emma ISt.

6월 7, 2025, Wooden Bridge in Naturpark Altmühltal

One of many on this section of the trail...

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It's one of the two huts located in the cross-country ski section. It offers a direct view of the pond (with a tree island), which you can walk around.

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It's one of two huts located in the cross-country ski section. The pond is somewhat hidden during the lush vegetation season. Signs with the relevant information can be found near the trees.

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Information board about hiking trails that start in Graisbach...

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Particularly colorful and beautiful in autumn

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Impressive castle with a beautiful view of the Danube.

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A Malm block measuring several thousand cubic meters within the colorful rubble masses in the area surrounding the Nördlinger Ries was used to extract raw materials and was partially mined. A small pond formed in the resulting hollow due to the low water permeability of the surrounding rubble rocks. The outcrop is located about 5.5 km southeast of the crater rim. The Gunzenheimer Gump is a small artificial pond (about 8 m deep), but it could only have been created due to the special geological conditions of its surroundings and human activities. The colorful rubble masses here consisted of large white Jurassic limestone blocks (Malm Delta) and clayey and sandy components from the Triassic and older Jurassic periods (Lias, Dogger). While the clayey-sandy deposits were removed, the more weather-resistant lime remained. The lime was used to build the Kaisheim monastery church. Due to the damming nature of the clays of the colorful rubble masses, water could rise under excess pressure (artesian rising spring) during lime mining and form a pond. The special geological significance of the Gunzenheimer Gump was taken into account in 2004. The Gunzenheimer Gump was included in the official geotope cadastre of the Bavarian State Office for the Environment and was thus awarded the "Geotop" seal of quality. [ Source: https://www.geopark-ries.de/geologische-besonderheit/gunzenheimer_gump-21524/ ]

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Edelweißweg

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Beautiful path through light mixed forest

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In the immediate vicinity of the Graisbach castle ruins there are several old linden trees (natural monuments).

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Beautiful wood carvings along the side of the Edelweiss Trail

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Beautiful wood carving on the side of the path - a bit "worn" but still clearly recognizable

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"Historic castle ruins on the "Schlossberg" on the northern edge of the village of Graisbach (municipality of Marxheim). The castle was presumably built by the "Edle von Graisbach" as a ministerial castle for the Counts of Lechsgmünd. After the counts' ancestral seat in "Lechsgmünd" was destroyed by Regensburg merchants in 1248, the counts resettled in Graisbach. From then on, they called themselves Counts of Lechsgmünd-Graisbach. The castle was further expanded over the centuries, partially destroyed and rebuilt in the 15th century. In the 18th century, the castle was abandoned and used as a quarry. Stones from the castle were used as building material in the region, for example, for the Danube bridge in Neuburg. Today, only remnants of the castle complex (Pallas, keep, curtain wall, northwest tower, fountain market) can be visited. Of particular note is the well-preserved Romanesque castle chapel of St. Pankratius with its reliefs on the north portal and remnants of the historic wall paintings." Source: https://www.ferienland-donauries.de/sehenswertes/burgruine_graisbach-1780/

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"It is probably rare to find a lake with deep, clear water on a slope surrounded by poor and dry grassland. There are many legends and legends surrounding the Gunzenheimer Gump. How does the water get to a high point within a very dry area? The Both opposites can only be explained with the events of the giant catastrophe. These are ejecta from the giant, where Jura rock had fallen onto a large clay block and sunk deeply. Because the dry heath in the area previously had no protection and little economic value, the Jura rock was quarried, just like in many other places on the edge of the Ries. Apparently soon after mining began, water began to collect in the surrounding clay layer, making further mining impossible. What remained was the mysterious Gunzenheimer Gump, a deep, clear lake. The water comes from groundwater sources and is always full to the brim, even in extremely dry times. Occasionally the excess water runs over the heaths to the west, which leads to a completely different spectrum of plants with lawns, gap sedges and blue rushes as key species. The underwater vegetation consists primarily of pondweed, while in the peripheral areas pond ledges, sedges and occasionally even flesh-colored orchid can be found." Source: Kaisheim - market and monastery (ed. Werner Schiedermair) https://www.kaisheim.de/de/marktgemeinde-kaisheim/ortsteile/gunzenheim/gunzenheimer-gump

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very nice little chapel, further down there is an open chapel and there are several benches with tables under the trees

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Beautiful wayside cross on the Edelweißweg

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Rarely have I sat better. Sun. Dry and the view of the small pond

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The way to and from there more than worth seeing

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Castle ruins in spring

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Here you come along the Donauwörther Edelweißweg

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