Salzburg Slate Alps

Coordinates: 47°23′N 13°13′E / 47.39°N 13.21°E / 47.39; 13.21
Source: Wikipedia, the free encyclopedia.
Salzburg Slate Alps
Burg Hohenwerfen
Highest point
PeakHundstein
Elevation2,117 m (6,946 ft)
Coordinates47°20′17″N 12°54′40″E / 47.33806°N 12.91111°E / 47.33806; 12.91111
Dimensions
Length60 km (37 mi)
Width10 km (6.2 mi)
Geography
Salzburg Slate Alps (in red) within the Alps.
Borders of the range according to the
Alpine Club classification of the Eastern Alps
Country
Salzburg
Range coordinates47°23′N 13°13′E / 47.39°N 13.21°E / 47.39; 13.21
Parent rangeNorthern Limestone Alps
Geology
Age of rockPaleozoic-Early Triassic
Type of rockGreywacke zone/Werfen Formation

The Salzburg Slate Alps (

Salzburg. Situated within the greywacke zone, they could be regarded either as part of the Northern Limestone Alps or of the Central Eastern Alps
.

Geography

The range is located between the

Low Tauern ranges of the Alpine crest. The Salzburg Slate Alps stretch about 60 kilometres (37 mi) in west–east direction, from the Salzburg Pinzgau region, north of the Salzach, into the Pongau region and along the Enns river up to the border with Styria
.

This inner-Alpine

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.

Subdivisions

From a topographic perspective there are two subgroups, separated by the Salzach river where it bends northwards near St Johann im Pongau:

  • the Dienten Mountains (Dientener Berge), which are known in the region as slate mountains in the true sense, running from west of the Salzach to Lake Zell and including 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 massif, 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;
    • Dachstein
      , and are morphologically less related to the Dachstein massif and more to its southwestern outlier

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