가장 멋진 폭포 4곳

A bit hidden but a nice place

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The Kohlstattbrunnenbach stream runs beautifully along the hiking trail. Water cascades can be seen again and again. You also pass the spring.

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Kohlstattbrunnenbach 🌊 - HochAlbPfad Felsquellweg 🏞🌊 - Meßstetten-Oberdigisheim - Zollernalbkreis

The Bärenthaler Kalktuff is a freshwater limestone from the Swabian Alb, which is still mined today in the municipality of Bärenthal in the Tuttlingen district. These limestone tuffs are widespread in Germany in the Jura (especially the Swabian Alb) and in the Muschelkalk of northern Württemberg and have been mined in many places. Most of the limestone tuff deposits there are exhausted today (2020). In the 1890s and 1930s, the limestone tuff from the Bäratal was a frequently used building stone in southwest Germany. In the Bära Valley, only part-time mining of this natural stone is carried out. On the western side of the valley of Bärenthal there is still a 700 meter long lens-shaped limestone tuff blanket of the Bära Valley. A further six limestone tuff sedimentations have been identified on the slopes of the Bära Valley (Upper and Lower Bära, Ensisheim). At the southern end of the limestone tuff cover, a waterfall is registered as a natural monument “Bierenthaler Tuffsteinkaskaden”. Fresh limestone tuff still forms here today. Part of the large limestone tuff ceiling is still a quarry that is still run as a part-time business today. The deposited layer, which is suitable for stone extraction and is well consolidated, is around 4 to 5 meters. There used to be several quarries in the Bära Valley. The thickness in Bärenthal can be up to 9 meters and in Ensisheim even more. In the hamlet of Ensisheim, 2.1 km north, but still part of the municipality of Bärenthal, there are large parts of a limestone tuff bar that are still freely accessible and worth seeing. You can see two well-preserved mining remains with vertical walls, on which the structure and structures of the limestone tuff are clearly visible and the process of their mining is understandable. Caves, niches and typical karstification phenomena (e.g. remains of leaves, tree branches, hollow spaces) are still preserved. Source: https://de.wikipedia.org/wiki/B%C3%A4renthaler_Kalktuff

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A small waterfall on the hiking trail around the Schömberg reservoir.

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Beautiful waterfall 🌊 on the Schlichem 🌊 Schlichemwanderweg 🏞🌊 - Hausen am Tann - Zollernalbkreis

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Beautiful water stairs here in the valley.

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A small great tufa that flows in dur Bära.

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Idyllic course of the Schlichem and great dog bathing place

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April 2022: It is currently forbidden to enter the upper part of the cascades. The entire structure is very sensitive and can easily break, and the mosses necessary for the formation of tufa are very sensitive to foot traffic. But you can also admire and enjoy the beauty of this spot very well if you stay behind the barrier. Once a video, above the water up to the barrier, filmed with a 3-meter selfie stick: https://www.youtube.com/watch?v=UlZmN4p_wvw And again, with immersion in the water: https://www.youtube.com/watch?v=eW2DREag9A0

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Apparently peat is grown here. In any case, you don't see something like that every day.

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The tuff cascades look beautiful. From above, the water splashes in several steps down to the Bära...

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Small but fine 🌊 and still beautiful 👍🏻

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On the way up through the dark valley to Geyersbad, the lively stream flowing alongside is a delight. As peaceful as it cascades down, the slope beside it appears daring – a wild ravine of rock and fallen tree trunks. It has a wonderful charm that pictures can hardly capture.

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which of the two inlets is the source?

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mini waterfall but with water

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You don't expect a great hidden little waterfall.

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Beautiful little waterfall, the water splashes down the limestone cascades before it reaches the barracks.

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Idyllic stream, part of the Felsquellweg Oberdigisheim / HochAlbPfad

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The Bärenthaler Kalktuff is a freshwater limestone, which is mined at the small community Bärenthal in the district Tuttlingen in Baden-Württemberg. Tufts are widespread in Baden-Württemberg and have been mined in many places. Most of the local lime deposits are exhausted today (2014). In the 1890s and 1930s, the tufa from the Bäratal was a commonly used building block in Baden-Württemberg. In Bäratal only a sideline mining of this natural stone is operated. The result is the Bärenthaler Kalktuff in the Holocene. During the Holocene, calcareous calcareous spring waters formed this lime deposit when the calcium carbonate contained in it was precipitated and deposited. Even today, lime deposits on a slope, over which a waterfall flows. The tufa formed a more than 700 meter long lenticular rock body. This tuff is in solid, loosened and in only partially solidified form. The thickness is 8 to 9 meters. The deposited layer, which is well-consolidated, is about 4 to 5 meters. In the Bäratal formerly there were several quarries. Source Wikipedia https://de.wikipedia.org/wiki/Bärenthaler_Kalktuff

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