누스플링겐‬에서 가장 멋진 ‪5‬개의 폭포

A bit hidden but a nice place

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

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

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

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

Beautiful water stairs here in the valley.

A small great tufa that flows in dur Bära.