File:170818-2 Filstal mit Hausener Wand mit Bad Überkingen, Blick Richtung Nordost.jpg

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Deutsch: Die eigentliche „Hausener Wand" am Südwesthang des Michelsbergs ist ein ehemaliger Bergsturz von großer geologischer Bedeutung und zeigt in eindrucksvoller Weise die Schichten des Weißen Jura a bis d.

Die Wechselfolge der Kalk- und Mergelkomplexe, insbesondere im Weißen Jura g, sowie die Bildung der Schwammkalke im Weißen Jura d, ist dort vortrefflich zu beobachten.

Am Hangfuß sind die Schichtpakete des Bergsturzes als Rutschungen abgelagert.

Quelle: LUBW
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Author R.kaelcke

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current12:40, 1 May 2018Thumbnail for version as of 12:40, 1 May 20184,000 × 2,657 (10.55 MB)R.kaelcke (talk | contribs)User created page with UploadWizard

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