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Selz川の約1100mにわたる、自然に近い河川の流れを特徴づけるすべてを備えた、美しくデザインされた自然再生エリア。

Very impressive and beautifully renovated. The tower is open, and the view is fantastic.

View of the Nahe River from the direction of the bridge houses (landmark of KH). There are now restaurants and cafes on the bridge again, inviting visitors to linger and enjoy themselves (as of January 26th).

A relatively modern-looking large crucifix on the Nahe bridge.

The Selz River is the hydrographic axis of Rheinhessen. It flows for over 60 km in a large arc through Rheinhessen before emptying into the Rhine near Ingelheim. Hiking trails and a continuous cycle path (Selztal Cycle Path) run along the Selz. Anyone hiking in Rheinhessen should visit the source of the Selz. Cycling along the Selz also offers a beautiful cross-section of the Rheinhessen landscape.

The Aulheim Valley lies within the Flonheim district in Rheinhessen. Geologically, Rheinhessen largely corresponds to the Mainz Basin, the northeastern edge of the Upper Rhine Graben. When the Upper Rhine Graben collapsed millions of years ago during the folding of the Alps, a connection was created via the Rhone Valley to a subtropical sea in the south and via the Hessian Depression to what is now the North Sea. This led to two flooding phases in the Oligocene and Miocene. The Vorholz Peninsula was only briefly flooded. The floor of the Mainz Basin consists of rock formations from the Rotliegend or Permian periods (296–251 million years ago). There was volcanic activity here from fissure volcanoes that covered the surface with layers of lava. In the Aulheim Valley, the lava was fast-flowing, low-silica lava, which cooled quickly and solidified into porous sediment with numerous gas inclusions. This made andesite unsuitable as a building material. Water and minerals penetrated the inclusions, and after the water evaporated, agates and geodes slowly formed. On the path through the Aulheim Valley from the Geistermühle to the Aulheimer Mühle, you can still see the retaining walls of the slope on the side facing Flonheim. Boundary stones can still be found here, marking the old district boundary.

From here we go into the Rhine

The Seckerborn spring (also called "Brünnelschen") is located on the hilltop of Kahlenberg, northwest of Wendelsheim. Particularly beautiful agate almonds were discovered here during vineyard clearing. From here, you can enjoy a beautiful panoramic view of the trulli, Riedertal, and the Eckelsheim surf cliff. Source: Strampelmuse