Serdiški breg
| Serdiški breg | ||
|---|---|---|
 Serdiški breg from the southeast |
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| height | 416 m. i. J. | |
| location | Prekmurje , Slovenia | |
| Mountains | Goričko ( Southeastern Alpine Foreland ) | |
| Dominance | 1.5 km → Sotinski breg | |
| Notch height | 80 m ↓ tri-border area | |
| Coordinates | 46 ° 49 ′ 50 " N , 16 ° 0 ′ 47" E | |
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| rock | Phyllite schist | |
| Age of the rock | Paleozoic | |
Serdiški breg or Rdeči breg is a 416 m. i. J. high hill in Goričko in the Slovenian region of Prekmurje . After the neighboring Sotinski breg (Stadelberg) it forms the second highest elevation in the Prekmurje and Pomurska regions .
Location and surroundings
Serdiški breg is located about 1300 m southeast of the triangle of Styria / Burgenland / Slovenia near the Austrian border. It is located in the districts of Ocinje and Serdica in the Rogašovci municipality . In the east, the Ledava cut separates the elevation from Sotinski breg ( 418 m ). While the south and south-east slopes are largely populated and used for agriculture , for example for viticulture , the north side near Kalch ( Neuhaus am Klausenbach municipality ) is completely forest-covered. The Rotterberg ( Slovene Kefašev breg ) on the Austrian side reaches a height of 408 m above sea level. A. The hill is part of the Raab-Őrség-Goričko trilateral nature park .
Geology and geomorphology
Geologically, the Serdiški breg lies on the eastern edge of the Graz Bay , which is determined by tertiary sediments. Like the neighboring Stadelberg, Serdiški breg is also part of a geological window described in Austrian literature as the “Neuhauser Schieferinsel” . It consists mainly of Paleozoic slates , which, according to Helmut Flügel, belong to the Sausal group. The rock, which is not very susceptible to weathering, retained its plateau character. The name "Rdeči breg" (literally Red Hill ) is derived from the reddish soil, which is caused by the appearance of clay slate on the so-called Stadelberg level . The hill Črešnjevec ( 311 m ) to the southeast is separated from the Serdiški breg by a stream, which, like the Ledava Gorge, may have resulted from a disturbance .
tourism
Before the first geodetic surveys, Serdiški breg was believed to be the highest point of Goričko. A chalet built by the Rogašovci Tourist Board on the plateau is open on weekends and can be reached both on an asphalt road and via hiking trails. Like Sotinski breg , the hill is located on Via Pomurje (Pomurska Planinska Pot) , a 300 km long long- distance hiking trail through the Pomurska region. There is a control stamp on the outside of the chalet. In the immediate vicinity at the highest point of the mountain there is a wooden obelisk erected in 1995 .
photos
View from the east
View from the Ledava valley
Holiday home
Summit with a chalet
Summit obelisk
View to the Sotinski breg
Via Pomurje
Web links
- Description on the Rogašovci website (Slovenian)
Individual evidence
- ↑ a b Anita Žalik, Rok Ciglič, Petra Gostinčar & Klemen Gostič: Prikaz pokrajine s pomočjo geografske panorame na primeru Serdiškega in Sotinskega brega. In: 20. Zborovanje Slovenskih Geografov - Pomurje Trajnostni regionalni razvoj ob reki Muri , Ljutomer - Murska Sobota 2009, pp. 341–353 (Slovenian). Online PDF , accessed June 30, 2018.
- ↑ Martin Gross, Ingomar Fritz, Werner E. Piller, Ali Soliman, Mathias Harzhauser, Bernhard Hubmann, Bernd Moser, Robert Scholger, Thomas J. Suttner & Hans Peter Bojar: The Neogene of the Styrian Basin - Guide to Excursions. In: Joannea Geol. Paleont. 9, pp. 117-193. Online PDF , accessed June 30, 2018.
- ↑ Serdiški breg. Občina Rogašovci , accessed June 30, 2018 (Slovenian).
- ↑ Ivan Gams : Geomorfologija in Izraba Valley v Pomurju. In: Geografski zbornik , Volume 5 (1959), pp. 205-251. Online PDF (Slovenian), accessed June 30, 2018.
- ↑ Serdiški breg. Goričko Informativna Stran, accessed on June 30, 2018 (Slovenian).