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水位が低いときは、小川を徒歩で渡ることができます。足を濡らしたくない場合は、すぐ隣にある歩行者用橋をご利用ください。また、渡渉点のすぐそばには、短時間で心地よく涼むためのクナイプ式腕浴槽があります。

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。

非常に印象的で、見事に改装されています。塔は開いており、素晴らしい景色が楽しめます。

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