The best family-friendly hikes and walks around Bingen

Pure relaxation while swinging. Afterwards, the well-deserved rest follows.

A great view into the Laucherttal valley.

Note: The jetty is relatively narrow (stroller might be a tight fit) and (being made of wood) a bit slippery when wet.

Witberghütte 655 m above sea level. - Hut - Donau-Zollernalb-Weg 🏞 - Hohenzollernweg 🏞 - Sigmaringen - LKR. Sigmaringen

AP Nägelesfelsen 670 m a.s.l. - Beautiful view into the Laucherttal - Donau Felsen Läufe Witbergrunde 🏞 - Sigmaringen

The Bittelschießer Täle is a canyon-like, densely wooded breakthrough valley in the lower reaches of the Lauchert, west of Bingen in the Sigmaringen district of Baden-Württemberg. The canyon is only about 400 meters long, 20–60 m wide and up to 30 m high (another 24 m of river sediments down to the rock floor). It is a scenically attractive part of the "Flächenalb" and also a geologically particularly significant Quaternary geotop. From the Middle Ages to the 19th century, the canyon and the Lauchert were also economically and as manorial property significant. The narrow valley is just as popular with hikers and cyclists from far and wide as it is for walks and local recreation for the residents of the surrounding villages. Until the Mindel glaciation (~1 Ma), the Lauchert used its current riverbed, but flowed into the then Upper Danube about five kilometers earlier at "Rückhau", between Hitzkofen and Heudorf, which at that time followed a more northerly route from Scheer to Riedlingen. At the end of the Mindel glaciation, about 900,000 years ago, an ancient Danube broke through the small pass near "Bahnhof Hanfertal" (today part of Sigmaringen-Nord). It shortened its route to Riedlingen by using the Lauchert bed to then continue its then more northerly route to Riedlingen. In the middle Riss glaciation, about 200,000 years ago, glacial masses from the Alpine Rhine Glacier advanced northwards in the area around Sigmaringen in two cold phases via the then Upper Danube. The glacier fan reached its maximum advance in its second cold phase ("Vilsingen-Stand II", location still south of the present-day Danube) near "Hertenstein, Lauchert", Billafingen, Langenenslingen and Riedlingen. The glacial sediments were so thick that the Upper Danube and the Lauchert were dammed. The backwater of the Upper Danube reached at least as far as Tuttlingen, that of the Lauchert probably as far as Hausen an der Lauchert. The Lauchert valley between "Hanfertal" station and Hitzkofen, used by the Upper Danube before the Riss glaciation and further deepened by it, and then completely blocked by moraine debris by the glacial advances, was again freed and used by the Lauchert from glacial debris – with one exception: a large mass limestone rock of the "Liegenden Bankkalk" formation standing in the direct path was not bypassed as before (as, incidentally, also previously by an ancient Danube), .... Source: https://de.wikipedia.org/wiki/Bittelschie%C3%9Fer_T%C3%A4le

Hornstein Castle is the ruin of a hilltop castle on a spur-like rocky ridge above the Lauchert river at around 630 m above sea level, near the Bingen district of Hornstein in the Sigmaringen district of Baden-Württemberg. It was first mentioned in 1244. The castle was the property of imperial knights, its first documentary mention dates back to 1244. Before that, the Lords of Hornstein, mentioned as early as the 11th century, probably resided in a castle in the Hornstein area. As the ancestral seat of the noble family of the same name, the von Hornstein family, the castle went through several phases of construction until it was converted into a stately Baroque palace around 1700. In 1787, the Hornsteins sold their property to the Princes of Hohenzollern-Sigmaringen. In 1818, the Prince of Hohenzollern-Sigmaringen decreed that a Hohenzollern "house of correction and reformatory" should be established in the castle. After the conversion was completed, the institution began operations on December 14, 1818. The institution's regulations also stipulated that the insane were to be admitted. In 1850, the Hohenzollern principalities were incorporated into Prussia. The Prussian state continued to operate the institution, and in 1859 it became a penal and correctional facility for men. The female inmates were transferred to Habsthal at the time. The institution was closed in 1869. In 1873, the complex was sold for demolition, the buildings were torn down, and the walls were left to decay. Only the castle chapel, a Baroque gem where the Christian liturgical year is celebrated, was preserved. From 1947 to 1962, the ruin was used as an open-air stage. Source: https://de.wikipedia.org/wiki/Ruine_Hornstein_(Bingen)

The beaver works here and dismantles the logs - Nature Park Obere Donau - Bingen - LKR. Sigmaringen