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The Haller Mauern are a mountain range of the Northern Limestone Alps in northern Styria and southern Upper Austria. They reach their highest point at the Großen Pyhrgas with 2244 meters above sea level. The Haller Mauern are a subgroup of the Ennstal Alps and form their northwestern terminus. The landscape-defining main ridge is predominantly composed of Dachstein limestone and is heavily karstified. The high altitudes are largely natural, providing habitats for many animal and plant species, and are largely under nature protection. A multitude of mountain pastures serve alpine farming, which declined significantly at the beginning of the 20th century. Through protective huts and a large network of trails, the Haller Mauern are open to tourism. The mountain range is named after the town of Hall near Admont, where salt was extracted until the 16th century.
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The northern boundary begins at Windischgarsten and follows the Dambach eastwards over the Hengstpass along the Laussabach to Altenmarkt bei Sankt Gallen. In the east, the Enns at Weißenbach, the Buchauer Bach, and the line Buchauer Sattel to Admont form the boundary. The Enns is also the southern boundary from Admont upstream to Liezen. From there, the boundary follows the Pyhrnbach northwards over the Pyhrnpass along the Teichl to Windischgarsten.[1]
The Haller Mauern have a maximum extent between the Pyhrnpass in the west and Altenmarkt in the east of 28 kilometers and from north to south of 18 kilometers. The mountain range covers a total area of approximately 288 km².