Turmberg (Hausruck)
| Turmberg | ||
|---|---|---|
| height | 750 m above sea level A. | |
| location | Eberschwang , Geboltskirchen , Haag am Hausruck (summit), Upper Austria | |
| Mountains | Hausruck ( Northern Alpine Foreland ) | |
| Dominance | 1.2 km → Sulzberg | |
| Notch height | 35 m | |
| Coordinates | 48 ° 9 '36 " N , 13 ° 36' 39" 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) | |
The Turmberg is 750 m above sea level. A. high elevation of the northeastern Hausruck in Upper Austria .
history
The Turmberg is so named because there was a tower on it that fell into disrepair in the 1950s. The foundations can still be seen today.
Location and landscape
The Turmberg lies between Eberschwang ( Ried im Innkreis district ) and Geboltskirchen ( Grieskirchen district ). The summit lies in the municipality of Haag am Hausruck (which extends far south here).
The Turmberg, with its northern continuation of the ridge, the Schloßberg, forms the northeastern branch of the Hausruck and Kobernaußerwald train , and rises about 200-300 meters above the surrounding towns. The Hausruck side ridge runs south from the Turmberg (transformer station of the overhead line 720 m ) to the Sulzberg ( 770 m , directional radio station , road Eberschwang – Geboltskirchen pass height 719 m ), and then meets about 4 kilometers south of the Turmberg on the main east-west direction of the ridge.
To the west of the Turmberg lies the source basin of the Antiesen (to the Inn) near Eberschwang, in the east the numerous source ditches of the Trattnach (to the Innbach and Danube) around Geboltskirchen and Haag, making the hill part of the important watershed of the Danube river areas below / above Jochenstein .
The ridge itself is densely covered with spruce forest, the cultivated land around the villages of Vocking , Annex and Odelboding , Wiesing reaches a little over 600 meters above sea level.
geology
The Turmberg is made up 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 around 80–100 meters thick . It rests on the Ried layers , weakly fine sand clay marl of 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; the southern end of the only moderately thick coal hollow of the Hague Ridge is located under the Turmberg, for example .
Development
The Hausruck-Kobernaußerwald-Weitwanderweg (HKWW / 10HK) runs over the ridge of the Turmberg. Coming from the summer toboggan lift and the Hague lookout tower ( Luisenhöhe ) , it has access in all directions until Mattighofen . The little pronounced Turmberg summit itself does not form a vantage point.
Between Sulzberg and Turmberg, south of the transformer station, a way of the cross from the Annex and the wooden houses near Wiesing crosses the ridge.
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 .
