Gutenstein Alps

Other important rivers are the Traisen in the west, the Gölsen and the Triesting in the north and the Schwarza south of the mountain range.

The gray to brown, usually layered sediment was formed in the lagoons of the Triassic and is related to Bunt dolomite.

With the exception of the Piesting valley (municipalities of Gutenstein, Pernitz, Markt Piesting) and the Puchberg Basin, only the valleys on the edge of the Gutenstein Alps and the plains on the eastern edge are densely populated.

Important places are Traisen, Hainfeld and Berndorf in the north, Wöllersdorf, Neunkirchen and Ternitz in the east, and St. Aegyd am Neuwalde and Lilienfeld in the west.

In particular, the Hohe Wand in the east is accessible by a variety of paths, scrambles and climbs, and has numerous mountain inns and huts.

The Kleinzell Hinteralm on the north side of the Reisalpe
Pine and spruce woods on the Almeskogel (1,061 m); in the background: the Unterberg