File:Geologische Strukturen im Gebiet Noctis Labyrinthus (53484482841).jpg
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In the southern Martian highlands, which are very rich in exciting geological phenomena, the Noctis Labyrinthus region, which was created by tectonic expansion processes, represents a very special area.
In dem an aufregenden geologischen Phänomenen sehr reichen südlichen Marshochland stellt die durch tektonische Dehnungsvorgänge entstandene Region Noctis Labyrinthus noch mal ein ganz besonderes Gebiet dar.
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[edit]DescriptionGeologische Strukturen im Gebiet Noctis Labyrinthus (53484482841).jpg |
Deutsch: In dem an aufregenden geologischen Phänomenen sehr reichen südlichen Marshochland stellt die durch tektonische Dehnungsvorgänge entstandene Region Noctis Labyrinthus noch mal ein ganz besonderes Gebiet dar. Im Text wird unter anderem auf die hier markierten geologischen Strukturen eingegangen: „graben structures“ sind tektonische Dehnungsstrukturen, bei denen Teile der Landschaft entlang von Bruchlinien abgesackt sind; „chaotic terrain“, also chaotisches Gebiet, ist ein Fachterminus für eine durch Erosionsprozesse gestaltete Landschaft, in der von der Erosion noch nicht vollkommen verwitterte Fels- oder Bergblöcke „chaotisch“ angeordnet sind; „very large ripples“ sind lange, hohe und 150 bis 200 Meter voneinander entfernte, senkrecht zur Windrichtung angeordnete Dünenkämme; „channel emerging“ zeigt einen von Wasser in den Talgrund erodiertes kleines Flusstal; „light toned materials“ sind helle Ablagerungen von hydratisierten, also vom Kontakt mit Wasser veränderte Mineralien; „large landslide“ zeigt die Überreste eines Bergrutsches entlang einer etwa 50 Kilometer langen und drei Kilometer hohen Abbruchkante.
Bild: 5/7, Credit: ESA/DLR/FU Berlin CCBY-SA 3.0 IGO English: In the southern Martian highlands, which are very rich in exciting geological phenomena, the Noctis Labyrinthus region, which was created by tectonic expansion processes, represents a very special area. The text deals, among other things, with the geological structures marked here: “graben structures” are tectonic expansion structures in which Parts of the landscape have sagged along fault lines; “Chaotic terrain” is a technical term for a landscape shaped by erosion processes in which rock or mountain blocks that have not yet been completely weathered by erosion are arranged “chaotically”; “very large ripples” are long, high dune ridges 150 to 200 meters apart and arranged perpendicular to the wind direction; “channel emerging” shows a small river valley eroded by water into the valley floor; “Light toned materials” are light-colored deposits of hydrated minerals, i.e. minerals that have been changed by contact with water; “Large landslide” shows the remains of a landslide along a cliff edge that is approximately 50 kilometers long and three kilometers high. Image: 5/7, Credit: ESA/DLR/FU Berlin CCBY-SA 3.0 IGO |
Date | Taken on 22 January 2024, 14:00:42 |
Source | Geologische Strukturen im Gebiet Noctis Labyrinthus |
Author | DLR_de |
Flickr set InfoField | Mars Express |
Flickr tags InfoField | marsexpress; mars |
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This image was originally posted to Flickr by DLR_de at https://flickr.com/photos/48213136@N06/53484482841. It was reviewed on 25 January 2024 by FlickreviewR 2 and was confirmed to be licensed under the terms of the cc-by-sa-2.0. |
25 January 2024
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Author | Björn Schreiner 2023 @ FU Berlin |
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