List of geotopes in Landshut

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This list contains the geotopes of the Lower Bavarian city ​​of Landshut in Bavaria . The list contains the official names and numbers of the Bavarian State Office for the Environment (LfU) as well as their geographical location. This list may not be complete. Around 3,400 geotopes (as of March 2020) are recorded in the Bavarian geotope register. The LfU does not consider some geotopes suitable for publication on the Internet. For example, some objects are not safely accessible or may only be entered to a limited extent for other reasons.

Surname image Geotope ID Municipality / location Geological unit of space description Area m² / extension m geology Digestion type value Protection status comment
Growing stone E by Schönbrunn Growing stone 2 (Landshut) .jpg
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 261R001 Landshut
position 		Paar-Isar region On a marl horizon within the northern full gravel, water emerges here. A short but beautiful so-called stone channel has formed at this small layer spring, ie the water flows in a channel made of tuff limestone. Both inorganic and organic processes play a role in the precipitation of the lime dissolved in the water. Spring mosses and various algae and microorganisms are involved in the construction of the channel. 2
7 × 0 		Type: Stone gutter, layer source
Type: Tufa-lime 		no information significant Natural monument, landscape protection area
Nagelfluhwand on Teufelssteg near Landshut 261R002 Landshut
position 		Paar-Isar region At the Isarleite in Landshut, the northern full gravel is due (Upper freshwater molasse). These are deposits from Miocene river systems. The calcareous gravel is cemented to Nagelfluh walls by limestone precipitation near the edge of the valley. Thanks to their greater stability than steep steps on the slope, they smell out. 150
30 × 5 		Type: Rock wall / slope
Type: Conglomerate 		Slope crack / rock wall significant Biosphere reserve
Schweinbachtal W from Schweinbach Geotope Schweinbachtal (Landshut) .jpg
more pictures
 261R003 Landshut
position 		Isar-Inn hill country The Schweinbachtal is a typical asymmetrical valley with the type of terrain that often occurs in the tertiary hill country, especially at north-south facing valley cuts. Due to the periglacial overburden, the valley cross-section is clearly asymmetrical with flat slopes exposed to the northeast and steep valley flanks sloping to the southwest. In the lower section of the valley, the original morphology has been changed due to anthropogenic influences (development, water and path construction). 200000
1000 × 200 		Type: Asymmetrical Valley
Type: Gravel 		no information significant Landscape protection area
Salzdorfer Tal NE of Kumhausen 261R004 Landshut
position 		Isar-Inn hill country Asymmetrical valley with bed springs along the bentonite horizon at 470 m above sea level. The relocation of the stream in the 19th century caused a significant change in the shape of the valley in a short time. 100000
1000 × 100 		Type: Asymmetrical Valley, Layer Source
Type: Gravel 		no information significant no protected area
Southern Isar valley slope (Carossahöhe) in Landshut 261R005 Landshut
position 		Paar-Isar region On the southern slope of the Isar, in the urban area of ​​Landshut, there are no remains of cold-age terraces. The slope is largely laid out in the northern gravel of the Upper Freshwater Molasse. The gravel is partially baked into conglomerate and favor the formation of steep slopes (261R003). Layer sources emerge from marl layers. Side valleys cut the slope as notch valleys (e.g. Bernlocher Schluchtweg), outcrops z. B. on the eastern edge of the city (Äuß. Münchner Str. 99). 500000
5000 × 100 		Type: Prallhang, Layerquelle, Härtling
Type: Conglomerate 		Slope crack / rock wall precious Landscape protection area, FFH area

See also

Individual evidence

  1. ↑ Data source: Bavarian State Office for the Environment, www.lfu.bayern.de, Geotoprecherche (accessed on September 16, 2017)