Zinken

Zinken stands on the Hochschwab plateau in the Northern Limestone Alps of Styria. The summit rises to 1,926 metres above sea level, forming a sharp ridge that breaks away in steep walls toward the Ilgen valley to the south. Below the top lies the deep Dipperkar cirque, while to the east the Schönbergkar and a hollow called Hirschgrube separate it from the higher Great Beilstein. A lower outlier named Türndl, just under 1,700 metres high, juts up between these two cirques on the western flank.

The mountain’s rocks tell a story of shifting seas and ice. Wettersteinkalk, a soluble limestone, dominates the plateau and has carved the karst landscape. On the Zinken’s south-western side younger limestones of the Sonnschien and Steinalm formations lie above it, while beneath them Werfener schist appears near the Sackwiesensee. During the last ice age a plateau glacier covered the area, but its movement was so slow that the high surfaces show little glacial scouring. Only at the edges, where the rock drops away in cliffs and scree slopes, do the classic glacial cirques give the terrain its high-alpine character.

The main local route starts at Bodenbauer inn and climbs through Häuslalm to join an unmarked path that leads to the summit. The long-distance trails E6 and E4 pass just north of the peak, offering another approach for those who prefer marked routes. From the east, experienced hikers can ascend through Schönbergkar, where the walls of the cirque and the narrow ridges between them frame views of the surrounding plateau. The contrast between the gentle high-level surfaces and the dramatic drops at the edges makes the Zinken a rewarding destination for walkers who want to feel the scale of the Hochschwab.