Handlesberg – Haberkogel

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Handlesberg – Haberkogel
Highest peak Handlesberg ( 1370  m above sea level )
location Industrial district , Lower Austria
part of Gutenstein Alps , Lower Austrian Limestone Alps
Classification according to Trimmel  1865
Handlesberg – Haberkogel (Lower Austria)
Handlesberg – Haberkogel
Coordinates 47 ° 50 ′  N , 15 ° 44 ′  E Coordinates: 47 ° 50 ′  N , 15 ° 44 ′  E
rock Dolomite ( Wetterstein and main dolomite ), u. a.
Age of the rock around 240–220 million years ( Ladinium - Norium )
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The Handlesberg – Haberkogel train is a mountain group of the Gutenstein Alps , a group of foothills in Lower Austria .

geography

Southwest roofing of the group: Handlesberg with Atzberg ( 1093  m above sea level ) left and Lange Wand (approx. 1115  m above sea level ) right (from Hirschbach )

Location and landscape

The Handlesberg – Haberkogel group is located around 35 kilometers west of Wiener Neustadt and 25 kilometers northwest of Neunkirchen , between Gutensteiner Klostertal and Schwarzau in the mountains in the upper Schwarzatal . It extends in a south-west-north-east direction about 15 km, with a width of a good 10 km.

It forms the south-western subgroup of the Gutenstein Alps. Its main mountains are the Handlesberg  ( 1370  m above sea level ) near Schwarzau, the Edlaberg ( 1096  m above sea level ) near Rohr im Gebirge and the Haberkogel  ( 1041  m above sea level ) between Rohrer Sattel and Unterberg .

Boundary and neighboring mountain groups

According to the Austrian mountain group structure according to Trimmel , the group has the number 1867, and belongs as a subgroup to the Gutenstein Alps  (1860, AVE  23), a subgroup of the Lower Austrian Limestone Alps  (1800).

It is bounded by Trimmel (clockwise from the northwest, border lines in italics, high and low points with kote):

Outline and summit

  • The main ridge of the group runs in an S-shape from Gutenstein over the Kleiner and Großer Geiskopf  ( 1006  m above sea level ) to the Haberkogel  ( 1041  m above sea level ), then south over Haselrast - Winsakogel  ( 948  m above sea level ) - Rohrer Berg  ( 980  m above sea level ) - Rohrersattel - Streimling  ( 980  m above sea level ) - Winsaberg  ( 1008  m above sea level ) - Hahnstab / Wildföhrenstein ( 948  m above sea level ) - Handlesberg  ( 1370  m above sea level) A. ) - Baumeckkogel ( 972  m above sea level ) to Voitsmaut
  • A side ridge runs from Hahnstab between the upper cell stream and Paxbach over the Kienstein  ( 976  m above sea level ) to Edlaberg  ( 1096  m above sea level ) towards Rohr

Hydrography and geology

The west side of the group is the catchment area of ​​the Schwarza of the Leitha , the east side of the Piesting area of the Fischa . The small brooks in the group go largely star-shaped from the Handelsberg-Hahnstab area.

The group belongs entirely to the Northern Limestone Alps of the Northern Alps (Eastern Alpine Permomesozoic , Triassic - Lower Cretaceous ). The northern part of the group is bankiger Hauptdolomit (here Oberkarn - Obernor , 230-210 mya), the central part of older Wettersteinplatz dolomite ( Laden - Cordevolian to 240 mya), southern follows again the handle Berg Hauptdolomit, the transition of the sub-mount blanket for about donating Göller- Ceiling as two of the partial ceiling of the Ötscher ceiling . The southwest flanks around Schwarzau are younger, small clods of Dachstein limestone (Anninger limestone ), Plassenkalk , Ramsaudolomit and Flachwassergosau , which are documented in the Falkenstein Nature Park .

Especially the Südschrofen of the Handlesberg and the valley near Schwarzau show some caves.

Individual evidence

  1. Lukas Plan: Verbal description of the delimitation of the subgroups of the Austrian cave directory . Status: Jan 08 2008. Ed .: Association of Austrian Speleologists. ( hoehle.org [PDF; 321 kB ; accessed on May 15, 2018]).
  2. FK Bauer, R. Oberhauser: The geological structure of Austria. Springer-Verlag, 2013, ISBN 978-3-7091-3745-1 , p. 258, column 1 f and Tectonic map sketch of the eastern section of the Kalkalpen , p. 252 f.