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마지막 업데이트: 4월 11, 2026
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하이라이트 • 자연 기념물
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헤칭겐 주변 인기 장소
On the track of the knights – 7 stages on the Hohenzollernweg
독일의 Hohenzollern 자전거 길 - 7개의 구간을 통해 Swabian Alb를 가로지르다
스바이비시 순례 - 호헨좀슬랭 야고보의 길
베우론 성 야고보의 길에서 천국같은 하이킹
독일의 Hohenzollern 자전거 길 - 슈바벤 알프를 가로지르는 6개의 구간
Ride in Germany’s Zollernalb – Albtrauf and Hohenzollern mountains
Weekend excursion to the Swabian Alb
스바비아 알프스 - 성채, 동굴 및 트레일
헤칭겐 하이킹
헤칭겐 사이클링
A geological peculiarity is included in the tour.
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The Hohenzollern Graben is a geological fault line that stretches from southwest Germany to Austria. It was created by tensions in the Earth's crust that led to shifts millions of years ago. The rift is particularly striking along the Swabian Alb, where it clearly shapes the landscape. Rock layers are exposed here that would otherwise remain hidden. The area is of great interest to geologists because it provides deeper insights into the development of Central Europe.
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There are always impressive cracks on the edge of the cliff, but these have nothing to do with the Zollerngraben. The fault zone even runs across the Albtrauf and is actually higher than the surrounding area.
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The power plant in Starzeltal supplies environmentally friendly electricity, around 140,000 kWh per year. This is enough to supply 40 households.
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The Hohenzollern Graben was formed 15 million years ago as a result of the tectonic tensions caused by the folding of the Alps under the pressure of the African plate and the associated uplift of the Swabian Alb. The enormous forces created cracks, crevices and trenches. Although it is a collapse area, the terrain inside the graben towers above its surroundings. This so-called relief reversal is particularly evident in the example of the Hohenzollern, where a height difference of up to 350 meters is reached. As a witness mountain, it owes its position and formation to the harder, more erosion-resistant types of rock inside the graben. On the Alb plateau, too, the hilly, wooded terrain along the graben stands out from the flatter, unforested surroundings outside the graben. Source: https://de.wikipedia.org/wiki/Hohenzollerngraben#Entstehung If the above is correct, this is nothing more than a crack/cleft but not the Zollerngraben.
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In the upper part of the valley you are almost always alone
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The Hohenzollerngraben or Zollerngraben is the name given to the geological rift in the southwestern Swabian Alb in Baden-Württemberg, which is over 30 kilometers long and on average 1.5 kilometers wide. https://www.zollernalb.com/attraktionen/hohenzollerngraben-7eefd052cc
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