Kaiblinger Kogel
| Kaiblinger Kogel | ||
|---|---|---|
| height | 752 m above sea level A. | |
| location | Traunviertel , Upper Austria | |
| Mountains | Upper Austrian Pre-Alps / Enns and Steyrtal Flysch Mountains | |
| Coordinates | 47 ° 57 '24 " N , 14 ° 18' 21" E | |
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| rock | Flysch ( Altlengbach formation , cement marl series ) | |
| Age of the rock | 90–60 million years (Upper Cretaceous - Paleocene ) | |
The Kaiblinger Kogel is 752 m above sea level. A. high ridge in the south-eastern Traunviertel in Upper Austria .
Location and landscape
The Kaiblinger Kogel is located between the Lower Steyrtal near Steinbach an der Steyr , and the Ennstal near Ternberg , with the culmination on the municipal boundary .
Schweinsegg is on the west ridge , to the southwest the Bäckengraben goes by the houses Bäckengraben zur Enns, downstream from Ternberg , northwest a stream (led as a stream from the Kaiblinger Kogel) near Schattleiten to the Enns feeder Schädlbach . To the east is the basin of the Färberbach , which flows into the Steyr in Steinbach , with the Zehetner houses .
The mountain is at a 706 m above sea level. A. high saddle near Gasser upstream of the Herndleck massif ( 1026 m above sea level ), to the north it closes at 506 m above sea level. A. high saddle of Grünburgerstraße (Grünburg / Steinbach - Ternberg, L1328 ) the high-lift train ( 609 m above sea level ).
The mountain represents the southern end of the flysch zone of the eastern Upper Austrian pre-Alps ( flysch zone between Krems and Enns ) or the Enns and Steyrtal flysch mountains, the Herndleck south already belongs to the limestone pre-Alps ( Schoberstein group ). It forms a typical conical dome. The north slope of the mountain is forested, the south slope is open agricultural area.
geology
The Flysch is Altlengbach formation , with a series of cement marls on the ridge line (Wende Kreide – Tertiary, approx. 90–60 million years old).
Web links
- Kaiblinger Kogel. Tour description, nationalparkregion.com
Individual evidence
- ^ Rainer Braunstingl: The Flysch Zone southwest of Steyr (Upper Austria): Geological structure and considerations on the ultra-helvetic. In: Jahrbuch der Geologische Bundesanstalt , Volume 131 (1988), Issue 2, pp. 231–243 ( full article, pdf , geologie.ac.at).