The Gailtal Alps ( or Drauzug), is a mountain range of the Southern Limestone Alps in Austria. It rises between the River Drava ( Drau) and the Gail valley (in southwestern Carinthia) and through the southern part of East Tyrol. Its western group called "Lienz Dolomites" ( Lienzer Dolomiten), is sometimes counted as part of this range and sometimes seen as separate.
Name
The mountain range was described as the Gailthal Alps (
Gailthaler Alpen) with its present-day extent as early as 1845 by Adolf Schaubach in his standard work,
Die Deutschen Alpen.
[Adolf Schaubach: Die Deutschen Alpen, Vol. I, Jena 1845, pp. 174–176] The name Lienz Dolomites (
Lienzer Dolomiten) for the part west of the
Gailberg Saddle is more recent and was introduced in 1885 by the Lienz branch of the German and Austrian Alpine Club but quickly caught on.
[ Zeitschrift des Deutschen und Oesterreichischen Alpenvereins, 1899, p. 279.]
Classification
According to the Alpine Club classification of the Eastern Alps (AVE) the Gailtal Alps (No. 56) are subdivided into the
Drauzug proper and Lienz Dolomites subgroups, while in common parlance the umbrella term
Drauzug conversely applies to the whole
Limestone Alps range between the Drava and Gail rivers, including the Gailtal Alps and the Lienz Dolomites. In traditional geography according to
Eduard Suess and
Leopold Kober,
Drauzug or
Drau-Sava-Zug denoted all Southern Limestone Alps ranges stretching along the Drava River, from the Lienz Dolomites in the west to the
Karawanks in the east.
Located south of the broad Drava Valley, the Gailtal Alps orography count as part of the Southern Limestone Alps. However, they rise north of the Periadriatic Seam an therefore geologically do not rank among the Southern Alps ranges. In regard to their orogeny, they represent the remnants of the limestone which had been moved northwards across the Central Eastern Alps to form the Northern Limestone Alps.
Despite their name, the Lienz Dolomites are not made up of dolomite, though the steep rugged karst topography resembles the South Alpine Dolomite rock formations. The northern Latschur group with Mt. Goldeck near Spittal an der Drau does not consist of limestone rocks, but is a crystalline basement massif.
Geography
The 100 km long range, which narrows in the west, stretches between the Gail in the south and the
Drava in the north. In a trough between the Gailtal Alps and the Goldeck lies the Weißensee at , the highest lake for bathing in Austria. The Drava range is divided in a west-east direction into five ridges separated by transverse valleys and a longitudinal valley.
Neighbouring ranges
Based on the AVE classification, the adjacent ranges are:
Subdivisions
The Gailtal Alps can be divided into five massifs in east–west direction, separated by draws and the Weissensee longitudinal valley:
-
Lienz Dolomites, stretching about from the Kartitsch Saddle mountain pass (east of Sillian) to Gailberg Saddle near Oberdrauburg (highest summits: Große Sandspitze, , Spitzkofel, , both south of Lienz, Gamswiesenspitze, , and Lumkofel, )
-
Drauzug or Gailtal Alps proper, stretching about from the Gailberg Saddle to the confluence of Drava and Gail near Villach:
-
Reißkofel Group, between Gailberg and the Kreuzberg Saddle south of Greifenburg (Reißkofel, , The Jauken massif, with the highest peak Torkofel, the Spitzkofel, , and Sattelnock, )
-
Latschur Group, between Weissensee and the Drava bend near Sachsenburg (Latschur, )
-
The Spitzegel Group, southeast of the Weißensee between Kreuzberg Saddle and the Bad Bleiberg Graben (Spitzegel, )
-
Dobratsch or Villach Alp, , the easternmost foothills of the Gailtal Alps with the Schütt nature reserve.
Literature
-
Hubert Peterka, Willi End: Alpenvereinsführer Lienzer Dolomiten, Bergverlag Rother. Munich, 1984,
External links
