Schloßberg (Hausruck)
| Schlossberg | ||
|---|---|---|
| height | 712 m above sea level A. | |
| location | Eberschwang , St. Marienkirchen aH , Geiersberg , Haag aH , Geboltskirchen ; (1) Upper Austria | |
| Mountains | Hausruck ( Northern Alpine Foreland ) | |
| Coordinates | 48 ° 10 ′ 13 ″ N , 13 ° 36 ′ 30 ″ E | |
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| rock | Hausruckschotter ( foreland molasse , geozone molasse basin ) | |
| Age of the rock | ~ 10–7 million (Unter Pannon / Pontien ) | |
| Development | Hausruck-Kobernaußerwald long-distance hiking trail (HKWW / 10HK) | |
| particularities |
(1)Summit in accordance with St. Marienkirchen Kiesgrube, Bayer. Boundary stone (1603)
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The Schloßberg is 712 m above sea level. A. high elevation of the northeastern Hausruck in Upper Austria .
Location and landscape
The Schloßberg is located between Eberschwang ( Ried im Innkreis district ) and Haag am Hausruck ( Grieskirchen district ), south of St. Marienkirchen am Hausruck .
The ridge forms the north-eastern branch of the Hausruck and Kobernaußerwald train , which extends into the Inn and Hausruckviertel hill country , and rises about 200 meters above the surrounding towns. The Hausruck side ridge runs south from the Schloßberg to the Sulzberg (750 m), and then meets the main east-west direction of the range of hills about 6 kilometers south of the Turmberg. To the north, the train splits into the Pilgershamer Ridge with the Pilgershamer Forst , and the Hague Ridge , which ends in the Luisenhöhe above Haag. Between these arise the St. Marienkirchner Bach (to Antiesen ) and the Pram near Kruglug (municipality of Geiersberg ), in the east the numerous source ditches of the Trattnach (to Innbach and Danube) around Geboltskirchen and Haag, making the Schloßberg an important watershed of the river areas below the Danube / heard above Jochenstein .
The ridge itself is densely covered with spruce forest, the cultivated land around the villages of Vocking (municipality of Eberschwang) , Pilgersham (St. Marienkirchen) and Schernham (Geiersberg), Ditting and Letten (Haag) and Odelboding (municipality of Geboltskirchen ) reach just over 600 Meters above sea level.
history
The name of the mountain is based on a refuge from the Magyar storm period (900–950) between the first and second Bavarian settlement waves of the early Middle Ages.
Until 1780 the western Innbaiern (today's Innviertel ) belonged to the Duchy of Bavaria , in the east was the country of Austria ob der Enns (later Archduchy, now Upper Austria) - the Innviertel only came to Austria with the Peace of Teschen in 1779 Habsburg . On the Schloßberg there is a Bavarian boundary stone from 1603 ( ⊙ ), which still marks the municipality boundaries Eberschwang - St. Marienkirchen - Geiersberg.
Geology and mining
The summit of the Schloßberg consists of the moderately cemented Hausruck gravel top layer of the Hausruck-Kobernaußerwald , which was deposited here about 10–7 million years ago (Unter Pannon to Pontium ) as erosion material from the Alps, and is about 40 meters thick. The substructure consists of the Ried layers , slightly fine sandy clay marl from the Innviertel series , which were deposited about 10 million years ago on the edge of the Paratethys . In between, the Hausruck was a brackish to freshwater region or even land, either primarily consisting of sequoia forests, or these were brought in as driftwood from the south. From this, a brown coal layer has formed between the bedrock and the gravel cover , which extends from under the Schloßberg as a coal hollow, Haager Back North, to Hague.
The Schernham gravel pit (Niederndorfer Kieswerke-Transportbeton GesmbH) exists in the Geiersberg area ; the rest of the Schloßberg has been a water reserve for the surrounding communities since 1994 .
Development
The Hausruck-Kobernaußerwald-Weitwanderweg (HKWW / 10HK) runs over the Schloßberg. Coming from the summer toboggan lift and the Hague observation tower ( Luisenhöhe ) , it has access in all directions to Mattighofen . There is also a walking path from Vocking-Ortacker up.
The Schloßberg opens up views of the Inn and Hausruck districts in some clearings and fields .
literature
- Kurt Czudra: Sedimentological analysis and deposit model of the Miocene coal troughs of the Upper Austrian Molasse . In: Geologische Bundesanstalt (Hrsg.): Jahrb. Geol. B.-A. tape 121 issue 1. Vienna October 1978, p. 123–154 ( pdf , geologie.ac.at - with special consideration of the Turmberg-Schloßberg area).
See also specialist literature for the articles Hausruck and Hausruck and Kobernaußerwald
Individual evidence
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↑ Water Rights Act 1959 - WRG 1959StF: Federal Law Gazette No. 215/1959 (WV) Appendix F CatchmentareasAppendix. 6 (ris.bka, plan cannot be shown!).
In-depth: Andreas Scheidleder, Günter Eisenkölb, Gabriela Vincze, Helga Lindinger, Franko Humer, Claudia Schramm, Elisabeth Stadler (employees), Federal Environment Agency:Danube planning area to Jochenstein. Ed .: Federal Ministry of Agriculture, Forestry, Environment and Water Management, Section VII / 1. (doc, eionet.eu.int). ( Page no longer available , search inweb archives) Info: The link was automatically marked as defective. Please check the link according to the instructions and then remove this notice. Planning area Danube below Jochenstein. Catchment area Danube (incl. Elbe). In:Results report. Project inventory according to Articles 3 and 5 WFD, creation of maps, tables and texts; Work package location and boundaries of groundwater bodies (incl. WGEV measuring network). Part B. Vienna February 2005 (doc, eionet.eu.int [accessed on October 9, 2010] short titleWFD mapsBMLFUW-UW.3.2.5 / 0008-VII / 2/2004). ( Page no longer available , search inweb archives) Info: The link was automatically marked as defective. Please check the link according to the instructions and then remove this notice. - ↑ Lit. Czudra: Sedimentological analysis . 1978, 7th deposition model and paleogeographical situation of the coal hollows , p. 146 ff .
- ↑ Czudra: sedimentological analysis . 1978, 6. Extent and position of the coal hollow in the Hague Ridge and Fig. 19: Panel diagram of the coal hollow in the "Haager Back N" , p. 143 ff. resp. 150 .
