Schoibernberg
| Schoibernberg | ||
|---|---|---|
| height | 883 m above sea level A. | |
| location | near Oberhofen am Irrsee , Upper Austria | |
| Mountains | Mondsee Flysch Mountains , Salzkammergut Mountains | |
| Dominance | 4.86 km → Saurüssel | |
| Notch height | 215 m ↓ south of Schweibern | |
| Coordinates | 47 ° 56 '17 " N , 13 ° 20' 21" E | |
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| rock | Flysch ( cement marl series and Altlengbach formation ) | |
| Age of the rock | 90–50 million years ( Coniacium - Thanetium ) | |
| Development | Forest road around the summit | |
The Schoibernberg is 883 m above sea level. A. high mountain on the northern edge of the Alps near Oberhofen am Irrsee in Upper Austria .
Location and landscape
The mountain is a gentle knoll that rises northeast over the Irrsee . It belongs to the Mondsee Flysch Mountains of the Salzkammergut Mountains and forms the north-western subgroup of the mountains between Irrsee / Mondsee and Attersee , from which they are separated by the uppermost Vöckla in the east. There on the other side are the Rehberg (Die Röten 819 m above sea level ) and the northwestern foothills of the Glashüttenwald .
At the northern neighboring summit of the Kogler Berg ( 819 m above sea level ) the Alps end orographically, and the Hausruck and Kobernaußerwald train follows as part of the Alpine foothills . The Gommersberg secondary peak ( 806 m above sea level ) stretches to the south-west to the Irrsee.
The western flank of the mountain drains to the Oberhofner Bach (Mühlbach) , which already flows into the Mattig and thus the Inn, while the Vöckla and Nössenbach on the north slope flow as a tributary to the Traun . To the Irrsee itself - and thus to the Attersee – Mondsee catchment area - the Banngraben at Laiter goes on the southwest slope .
The larger towns around the mountain are Oberhofen to the northwest, Laiter am Irrsee to the west and Zell am Moos to the southwest, and Haslau to the southeast . The Salzburg state border, which bulges eastwards around Straßwalchen, passes north at Oberholz ( Hüttenedt / Jagdhub an der Vöckla area). 7 kilometers to the north-west is Straßwalchen , just as far to the north-east of Frankenmarkt .
Surname
At GM Vischer 1667 , the Pergerhuet can be found here , probably after the location Berg am Fuß above Oberhofen, which itself takes its name from the mountain.
The name-giving place Schoibern is located on the back of the Gommersberg. This name appears as early as 1787.
geology
The mountain belongs to the cement marl series ( Coniacium - Campanium , middle Upper Cretaceous, approx. 90–70 million years old) of the Flysch Zone , south of the Gommersberg and north of the Koglerberg lies the Altlengbach Formation ( Maastrichtian - Thanetian , Wende Kreide / Paleocene, 70–50 Million years). This tectonic discordance leads in a straight line to Straß im Attergau and is one of several on the northern edge of the Mondsee – Attersee-Flysch Mountains. You can also find it at Irrsberg on the other side of the Irrsee.
The Mondseeland was furrowed by a tongue of the Dachstein glacier, whose terminal moraines lie on the Krenwald and Kobernaußerwald. In the Mindel (around 450,000 years ago) and Riss ice ages (around 200,000 years ago), Koglerberg – Schoibernberg and Irrsberg were typical nunataks , rock islands protruding from the ice mass. Throughout the western foot along at about 500- 650 m above sea level. A. run the younger Riss edge moraines of the Irrseegletscher, also in the Haslau and further to the south lying Lackenberg . In Schoibern to about 700 m higher Mindel moraine located.
Development
The mountain is easy to climb from all sides: marked routes over forest roads lead from Gommersberg to the southwest, which can be reached from the lake and the Haslau, via Obernberg near Oberhofen and from Angern an der Vöckla via Jagdhub . The three paths lead to a forest road that leads to the summit at around 800 m above sea level. A. runs around. Various small forest paths and trails lead to the wooded summit itself.
Individual evidence
- ↑ Georg Matthäus Vischer : Archiducatus Austriae Superioris Descriptio facta Anno 1667 (layer online at DORIS , topic first regional recordings ) - Pergerhuet and Rabenshwenthner Huet are shown , the second probably the Schoibernberg; the upper Vöckla is called Sprentzl River there ; because of the projection distortion online at the position of Irrsberg or Oberhofen (as of 10/2014).
- ^ Carl Schütz , Franz Müller: Mappa of the land above the Enns. In the year 1781 reduced and engraved by CS Schütz and written by F. Müller 1787 (layer online at DORIS, subject of the first regional recordings ); because of the projection distortion online at Postition von Gollau in der Haslau (status 10/2014).
- ^ Rainer Braunstingl: Report 1984 on geological recordings in the flysch on sheet 65 Mondsee. In: Jahrbuch der Geologische Bundesanstalt 128 / Heft 2, p. 259 ( pdf , geologie.ac.at).
- ^ Eduard Stummer: The interglacial lakes of Salzburg. In: Negotiations of the Federal Geological Institute. 1936, p. 105 (full article p. 101–107, PDF on ZOBODAT , p. 5 there).
- ^ Walter del Negro : Geology of the State of Salzburg. Publication series of the state press office, special publications 45, Salzburg 1983, p. 26.
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↑ Julius Fink: Contributions to Plaistocene Research in Austria: Excursions between Salzach and March. Federal Geological Institute, 1955, p. 20;
Erich Seefeldner: Salzburg and its landscapes. A geographic study of the country. Verlag Das Bergland-Buch, 1961, p. 490;
(Unknown article) In: Mitteilungen der Geographische Gesellschaft in München , Vol. 48–50, Geographische Gesellschaft in München, 1963, p. 490 (on the reconstruction of the summit corridor ).