Jump to content

Salzburg Slate Alps

From Wikipedia, the free encyclopedia

This is an old revision of this page, as edited by RRady (talk | contribs) at 04:12, 7 March 2016 (added infobox map & map caption). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.

Salzburg Slate Alps
Highest point
PeakHundstein
Elevation2,117 m (6,946 ft)
Geography
Lua error in Module:Location_map at line 526: Unable to find the specified location map definition: "Module:Location map/data/Alps location map (Salzburger Schieferalpen, AVE).png" does not exist.
CountryAustria
StateSalzburg
Parent rangeCentral Eastern Alps

The Salzburg Slate Alps (Template:Lang-de) are a group of mountains in the Central Eastern Alps in the Austrian state of Salzburg. Situated within the greywacke zone, they are also regarded as part of the Northern Limestone Alps.

The range is located between the Kitzbühel Alps, the continuation of the greywacke zone beyond Lake Zeller and Saalach river in the west, and the Dachstein massif in the east. In the north it is adjacent to the Berchtesgaden Alps, while in the south the Salzach valley separates it from the Hohe Tauern.

Subdivisions

This mountain group, designated by the Alpine Club Classification of the Eastern Alps (AVE) based on its underlying rock, cannot be assigned from a geological perspective either to the Northern or the Central Alps, so it does not fit into the general tripartite division of the Eastern Alps and, as a result, is variously treated in the literature. From a topographic perspective the group includes:

  • the Dienten Mountains (Dientener Berge), which are known in the region as slate mountains in the true sense, run from west of the Salzach to Zell am See, and include the Hundstein massif (2,117 m (AA)) and the Schneeberg-Hochglockner Group (Schneeberg-Hochglockner-Gruppe, (Schneebergkreuz 1,938 m above sea level (AA))
  • the Fritztal Mountains (Fritztaler Berge), running from east of the Salzach to the Styrian border and the Dachstein, including the:
    • Hochgründeck (1,821 m above sea level (AA)) in the triangle formed by Bischofshofen, St. Johann and Altenmarkt;
    • Rossbrand (1,770 m above sea level (AA)), which runs from Altenmarkt to the Mandling Pass near Radstadt;
    • Glutserberg, Halserberg and the Ramsauerleiten, three smaller regions that continue the Rossbrand to Schladming;
    • Gerzkopf (1,728 m above sea level (AA)), north of the Fritztal valley, which geologically belongs to the limestone region between the Tennen Mountains and the Dachstein, and are morphologically less related to the Dachstein massif and more to its southwestern outlier


See also