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24. marts 2024
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Schweinbachtal from Schweinbach > a geotope (excerpt from the Bavarian Environmental Atlas)
The Schweinbachtal is a typical asymmetrical valley with a terrain shape that often occurs in the Tertiary hill country, especially in valleys facing north-south. Due to the periglacial overprinting, the valley cross-section is clearly asymmetrical with flat slopes exposed to the northeast and steep valley sides sloping to the southwest. In the lower section of the valley, the original morphology has been changed by anthropogenic influences (building, water and road construction).
umweltatlas.bayern.de/standortauskunft/rest/reporting/sb_geotope/generate?additionallayerfieldvalue=261R003
The Schweinbachtal is a typical asymmetrical valley with a terrain shape that often occurs in the Tertiary hill country, especially in valleys facing north-south. Due to the periglacial overprinting, the valley cross-section is clearly asymmetrical with flat slopes exposed to the northeast and steep valley sides sloping to the southwest. In the lower section of the valley, the original morphology has been changed by anthropogenic influences (building, water and road construction).
umweltatlas.bayern.de/standortauskunft/rest/reporting/sb_geotope/generate?additionallayerfieldvalue=261R003
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