Stadlerberg
Stadlerberg | ||
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height | 637 m above sea level M. | |
location | Zürcher Unterland , between the Bachsertal and the plain with the Neeracherried | |
Mountains | Swiss plateau | |
Dominance | 3.6 km → Egg | |
Notch height | 132 m ↓ near Binzrüti in the municipality of Neerach | |
Coordinates | 676 219 / 265798 | |
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Type | Gravel terrace | |
rock | Gravel , cemented like a nail | |
Age of the rock | early Pleistocene |
The Stadlerberg is 637 m above sea level. M. high hill in Switzerland , which lies in the Zurich Unterland .
geography
The approximately three and a half kilometers long, wooded ridge separates the Bachsertal from the plain in which the Neeracherried lies. In the southeast, the Stadlerberg borders the Heitlig ( 533 m above sea level ), in the west on the Sanzenberg ( 566 m above sea level ), from which it is separated by the valley with the Sagibach flowing to Weiach . To the northeast, the Stadlerberg is separated from the Ämperg ( 514 m above sea level ) by the Kistenpass . The connecting road from Bachs to Stadel leads over the Stig ( 538 m above sea level ) ▼ called saddle of the Stadlerberg .
To the north of the Stadlerberg lies the village of Weiach and the village of Raat on the Kistenpass . East of the Stadlerberg are Windlach , Schüpfheim and the town of Stadel that gives it its name.
From a geological point of view, the Stadlerberg is a gravel terrace from the early Pleistocene , which probably consists of medium moraine material . It is located in the Molasse basin , which forms most of the Swiss plateau .
history
An observation tower ▼ has been located on the Stadlerberg since 1964 and is to be renewed in the next few years.
On November 14, 1990, the Alitalia flight 404 crashed on the Stadlerberg due to an instrument failure that was not noticed by the pilot. Not far from the crash site ▼ there is a memorial stone ▼ .
Individual evidence
- ↑ Higher gravel north of the camps. In: strati.ch. Retrieved July 18, 2020 .
- ↑ Gerhart Wagner: Ice Age Middle Moraines in Aargau . 2005, p. 20-21 , doi : 10.5169 / SEALS-173105 .