オーバータウフキルヒェンの天然記念物・トップ11

A dead-ice basin is a dry, swampy, or water-filled depression formed by the melting of dead ice. Blocks of ice that break away from the glacier tongue during melting and remain there are called dead ice. Dead-ice basins in which a water-retaining layer has developed, or whose steep slopes sometimes extend below the groundwater level, are water-filled, swampy, or boggy. Their funnel shape allowed rain and meltwater to collect. These small bodies of water have experienced varying degrees of siltation and moor development, even within the same basin. The range of vegetation formations is very broad. It ranges from small reed beds to large sedge marshes, small sedge marshes, quaking grasslands, floating leaf and aquatic vegetation, transitional bogs, and even black alder swamps. Source: https://www.toteiskessel.de/uber-toteiskessel/was-ist-ein-toteiskessel/

Col de Landshut!

From here it's downhill no matter which direction you go.

From here you have a great view towards the Alps (when the weather is nice ;))

Highest point of the Vilstalweg between Dorfen and Velden (498m) with far-reaching views over the hilly countryside, along with rest areas "Auf der Hauser Höhe" and "Am Weinberg". The watershed between Isen and Vils also means the separation of the Inn and Danube (although both of them later come together again). On the skates you have to master a noticeable incline from both directions, while it is easy to go down on the other side.

Perfect for the break in between! There are enough seats and there is free shade when you are out and about on hot summer days ;-)

A special kind of watershed - the Inn later also flows into the Danube!

Highlights are always beautiful - the view extends as far as the Alps