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Türnachstock seen from the Hochschwab

Türnachstock seen from the Hochschwab

Highest peak Hochtürnach ( 1770  m above sea level )
location Styria , Austria
part of Ybbstal Alps ( AVE ), Lassingalpen / Lower Austrian Limestone Alps (Trimmel)
Classification according to Trimmel  1816
Türnach (Alps)
Door to
Coordinates 47 ° 39 '37 "  N , 15 ° 7' 21"  E Coordinates: 47 ° 39 '37 "  N , 15 ° 7' 21"  E
Type Limestone massif
rock Steinalm Formation ; Base throwing formation
Age of the rock 230–250 Ma ( Middle Triassic / Lower Triassic )
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The Türnach is a small mountain range in the southernmost Ybbstal Alps ( Lassingalpen ), on the middle reaches of the Salza in Styria not far from Mariazell . The massif culminates in Hochtürnach at 1770  m above sea level. A.

Boundary and Neighboring Groups

According to the mountain group classification for the Austrian cave directory of Trimmel , where it has the number 1811, the massif is as follows:

  • : in the northwest and north Bärenbach (Bärnbach) of the Salza (Bridge  632  m nbachsattels) to just south of the Bear [e] to about 1305  m  - down to the rear Rotmoos to Kräuterin (Trimmel No. 1812th)
  • in the east Radmerbach to the confluence (approx.  670  m ) in the Salza near Weichselboden to the Zellerhüten  (No. 1813)
  • in the south of Salza down to the Bärenbach to the Hochschwab (Trimmel No. 1744)

summit

On the elongated main ridge are from west to east:

  • Bärnstein  995  m
  • Guckkogel  1559  m
  • Hochtürnach  1770  m
  • Ameiskogel  1471  m
  • towards the north, towards the Rotmoos, the ridge ends in the Bockmauer

To the south, the Prescenyriegel branches off to the Prescenyklause der Salza power plant , to the north the Brunnriegel .

geology

The stick consists of the Steinalm-Wetterstein limestone from the anise of the Middle Triassic around 240 million years ago, which also continues over the Salza to the southwest into the Riegerin . The basis is formed by Werfen strata , slate and limestone from the Lower Triassic , these form the basement of the northern Limestone Alps, to the south adjoining the Grauwackenzone , which is known to the southwest in the Eisenerzer Erzberg .

Individual evidence

  1. Michael Moser, Wolfgang Pavlik, Olgo Piros: 1993 report on geological surveys in the Northern Limestone Alps in the Hochtürnach - Bärnbachgraben area . on sheet 102 Aflenz . In: Yearbook of the Federal Geological Institute . tape 137 issue 3, 1994, p. 481–483 ( pdf , geologie.ac.at).