The Ernstberg (also Erresberg) southeast of Hinterweiler is, at 698.8 m, the highest of the west Eifel volcanoes and, after the Hohe Acht, the second highest mountain in the Eifel overall. Its summit consists of pyroclastic rocks (Schweißschlacken) that form a volcanic crater that is open towards the east. This is where the basalt masses flowed out, forming a semicircle on the eastern slope of the mountain. It lies within the Waldeifel region.
The Ernstberg (also Erresberg) southeast of Hinterweiler is, at 698.8 m, the highest of the west Eifel volcanoes and, after the Hohe Acht, the second highest mountain in the Eifel overall. Its summit consists of pyroclastic rocks (Schweißschlacken) that form a volcanic crater that is open towards the east. This is where the basalt masses flowed out, forming a semicircle on the eastern slope of the mountain. It lies within the Waldeifel region.
In winter there are excellent winter sports conditions on the Ernstberg due to its height. Cut langlauf tracks, a toboggan slope and ski hire hut are available.
Discovered by embedding cosine similarity (sentence-transformers MiniLM, 384-dim).