File:Grosse-Lauter Bichishausen Schwaebische Alb.jpg
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[edit]DescriptionGrosse-Lauter Bichishausen Schwaebische Alb.jpg |
Deutsch: Tal der Großen Lauter bei Bichishausen mit Turm der 1735 im Barockstil erbauten, katholischen Pfarrkirche im Vordergrund. Am Horizont biegt die Lauter nach rechts in die große Schlinge, die sie um den nicht ganz abgeschnürten Umlaufberg beim Dorf Gundelfingen führt. Die im späten Pleistozän entstandene Weißjura-Felssohle des Lautertals wurde durch verschiedene vom Fluss mitgeführte Sedimente zu ihren jetzigen, breiten, flachen Form aufgefüllt. Zu oberst hat sich eine fruchtbare, humose und schluffig-tonige Schwemmschicht abgelagert. Darunter befindet sich eine unterschiedlich bis zu mehreren Metern dicke, im letzten Interglazial (Warmzeit) der Würmeiszeit gebildete Kalktuffbarre, die sich ab Bichishausen als Folge einer heute kaum noch wahrnehmbaren Gefällstufe ablagerte. Dieses geologisch markante Sediment setzte sich auch nach dem Horizont noch weitere 2 km ab - bis zur Mündung des Heiligentals, südlich des Fleckens Wittsteig. Vgl. das weitere Foto, auf welchen Gefällestufung und Kalktuffbarre gut erkennbar ist: Image:Kalktuff-Wasserfall_Grosse-Lauter_Schwaebische-Alb.jpg. English: View oft he valley of the Große Lauter in the village Bichishausen. The valley makes a loop to the right like an entrenched river does, leaving a rise or hill in the middle. The river has almost cut its loop, the height between the two closest parts is eroded down to mere few meters, the loop almost fully developed. The rock bottom of the river, eroded in late Pleistocene time is now filled up with layers of sediments - humus for agriculture, clayey silt and solidified tufa (CaCO3) of varying thickness. The layer of tufa sediment was detected in the river bed for more than 3 km – which is 2 km behind the horizon. For a well identifiable bank of tufa see the photo: Image:Kalktuff-Wasserfall_Grosse-Lauter_Schwaebische-Alb.jpg. The valley is extremely broader than the actual small river is now. This refers to the long earlier epochs, during which the river valley was eroded. The gradual slope behind the row of trees on the right has a rocky fluvial terrace, which was formed by an earlier river bed of late pleistocene time. |
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Author | Ustill |
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Camera manufacturer | Canon |
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Camera model | Canon EOS 350D DIGITAL |
Author | allwiki@ulrich.tichy.de |
Exposure time | 1/15 sec (0.066666666666667) |
F-number | f/32 |
ISO speed rating | 100 |
Date and time of data generation | 15:01, 8 May 2018 |
Lens focal length | 26 mm |
Online copyright statement | https://commons.wikimedia.org/wiki/File:Grosse-Lauter_Bichishausen_Schwaebische_Alb.jpg |
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City shown | Tübingen |
Width | 3,387 px |
Height | 2,253 px |
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Pixel composition | RGB |
Orientation | Normal |
Number of components | 11 |
Horizontal resolution | 72 dpi |
Vertical resolution | 72 dpi |
Data arrangement | chunky format |
Software used | Adobe Photoshop CS5 Windows |
File change date and time | 18:46, 20 May 2018 |
Exif version | 2.21 |
Date and time of digitizing | 15:01, 8 May 2018 |
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APEX exposure bias | −1 |
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Color space | sRGB |
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Focal plane resolution unit | inches |
Custom image processing | Normal process |
Exposure mode | Auto bracket |
White balance | Auto white balance |
Scene capture type | Standard |
Rating (out of 5) | 0 |
Date metadata was last modified | 20:46, 20 May 2018 |
Unique ID of original document | xmp.did:8CD1EFAD6F53E811A604CEB588DA5C5F |
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