Garggler

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Garggler
Gargglerin from the south-southeast

Gargglerin from the south-southeast

height 2470  m above sea level A.
location Tyrol , Austria
Mountains Stubai Alps , Eastern Alps
Dominance 1 km →  Pflerscher Pinggl
Notch height 154 m ↓  Badlerscharte
Coordinates 47 ° 0 '32 "  N , 11 ° 19' 43"  E Coordinates: 47 ° 0 '32 "  N , 11 ° 19' 43"  E
Gargglerin (Tyrol)
Garggler
Type Rock peaks
rock dolomite
Age of the rock Triad
First ascent A. Kerner v. Marilaun, F. Sauter, “Beginning of the 1870s” or H. Waitzenbauer and G. Pittracher, July 1874
Normal way marked trail from the south
Gargglerin from the north-northwest (hawk)

Gargglerin from the north-northwest ( hawk )

Template: Infobox Berg / Maintenance / BILD1

The Gargglerin , also Garklerin , is 2470  m above sea level. A. high mountain in the Stubai Alps in the Austrian state of Tyrol . The easily climbed summit is popular because of its view of the rear Gschnitztal , the Tribulaune and the Habicht .

Location and surroundings

The Gargglerin forms the highest point of a mountain ridge, which extends from the main Alpine ridge about 2 kilometers south to the north. In the northwest and north lies the Gschnitztal, in the east the Sandestal , a side valley of the Gschnitztal. The Tribulaunhütte ( 2064  m ) is the most important base for climbing the mountain there. To the northeast, the ridge continues to the upstream Eningkopf , also Nenningkopf ( 2183  m ). In the west is the Badlalm .

Geology and structure

The Gargglerin rises as a distinctive, jagged rock summit made of dolomite rocks from the Brennermesozoic , which, similar to the nearby Weißwandspitze , lie directly on a base made of crystalline rock , especially gneiss and mica schist . The main dolomite from the Triassic , which forms the summit structure, is light gray to white in color and has sericite inclusions . Due to the exposed location of the steep and narrow summit rock, mountain tears occur here , so that the summit structure is divided into numerous individual rock towers.

Bases and paths

The normal route to the Gargglerin leads from the south of the Badlerscharte , one on 2350  m located notch between Gschnitz- and Sandestal, on a marked path to the top. The Badlerscharte can be reached on a marked path from the Gschnitzer district Obertal over the Sandestal, whereby the Tribulaunhütte is often used as a base. Another ascent from Obertal, which leads over the northwest flank to Badlerscharte, was not accessible for a long time due to a rock fall , but has enabled a transition again since it was relocated in 2010. Alpine climbing routes lead through the south and east walls in the II. And III. Degree .

Literature and map

Individual evidence

  1. a b Garklerin. Stein & Kraut, accessed August 29, 2009 .
  2. Horst Kübler, Wolf-Eberhard Müller: The geology of the Brenner Mesozoic between the Stubai and Pflersch valley (Tyrol) . In: Yearbook of the Federal Geological Institute . tape 105 . Vienna December 1962, p. 173–242 ( geologie.ac.at [PDF; accessed on August 29, 2009]).