File:Übergang der Lycus Sulci in Amazonis Planitia (53375301644).jpg
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The landscape of the Lycus Sulci, the “Lycian Furrows” in the northwest of the largest volcano on Mars, the 21.
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[edit]DescriptionÜbergang der Lycus Sulci in Amazonis Planitia (53375301644).jpg |
Deutsch: Die Landschaft der Lycus Sulci, der „Lykischen Furchen“ im Nordwesten des größten Vulkans auf dem Mars, dem 21,9 Kilometer hohen Olympus Mons, erzählt eine Geschichte des katastrophalen Abbrechens und Abrutschens der unteren, mehrere tausend Meter hohen Flanken des Olympus Mons in ferner Vergangenheit. Planetenforscher vermuten, dass die Rutschungen vor mehreren 100 Millionen Jahren durch große Mengen dünnflüssiger Lava ausgelöst wurden, die sich die Flanken des Olympus Mons hinunterschoben. Diese Lavaströme lagerten sich vermutlich auf Gesteinsschichten ab, die große Wassermengen in Form von Eis enthielten, ähnlich wie in Permafrostböden auf der Erde. Die vulkanische Hitze ließ dieses Eis schmelzen, so dass die Randbereiche des Vulkans instabil wurden, abbrachen und somit unglaublich große Massen an Gestein abrutschten und ins Vorland von Amazonis Planitia schoben.
Credit: ESA/DLR/FU Berlin (CC BY-SA 3.0 IGO) English: The landscape of the Lycus Sulci, the “Lycian Furrows” in the northwest of the largest volcano on Mars, the 21.9-kilometer-high Olympus Mons, tells a story of the catastrophic break-off and sliding of the lower, several thousand-meter-high flanks of Olympus Mons in the distance Past. Planetary researchers suspect that the slides were triggered several 100 million years ago by large amounts of thin lava that pushed down the flanks of Olympus Mons. These lava flows were probably deposited on rock layers that contained large amounts of water in the form of ice, similar to permafrost on Earth. The volcanic heat caused this ice to melt, so that the edge areas of the volcano became unstable and broke off, causing incredibly large masses of rock to slip and push into the foreland of Amazonis Planitia. Credit: ESA/DLR/FU Berlin (CC BY-SA 3.0 IGO) |
Date | Taken on 13 July 2023, 19:06:28 |
Source | Übergang der Lycus Sulci in Amazonis Planitia |
Author | DLR_de |
Flickr set InfoField | Mars Express |
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This image was originally posted to Flickr by DLR_de at https://flickr.com/photos/48213136@N06/53375301644. It was reviewed on 12 December 2023 by FlickreviewR 2 and was confirmed to be licensed under the terms of the cc-by-sa-2.0. |
12 December 2023
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current | 00:06, 12 December 2023 | ![]() | 1,920 × 1,080 (1.87 MB) | OptimusPrimeBot (talk | contribs) | #Spacemedia - Upload of https://live.staticflickr.com/65535/53375301644_7474bf34a3_o.jpg via Commons:Spacemedia |
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Camera manufacturer | Synthetic Camera |
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Camera model | Perspective Camera |
Exposure time | 0/1 sec (0) |
Date and time of data generation | 19:06, 13 July 2023 |
Lens focal length | 24 mm |
Author | Björn Schreiner 2023 @ FU Berlin |
Width | 1,920 px |
Height | 1,080 px |
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Compression scheme | LZW |
Pixel composition | RGB |
Orientation | Normal |
Number of components | 3 |
Horizontal resolution | 72 dpi |
Vertical resolution | 72 dpi |
Data arrangement | chunky format |
Software used | Adobe Photoshop CS6 (Windows) |
File change date and time | 11:17, 2 August 2023 |
Exposure Program | Manual |
Date and time of digitizing | 19:06, 13 July 2023 |
Color space | Uncalibrated |
Focal plane X resolution | 720 |
Focal plane Y resolution | 720 |
Focal plane resolution unit | 3 |
Date metadata was last modified | 13:17, 2 August 2023 |
Unique ID of original document | xmp.did:B70119009A21EE1196AFA1044090A15B |
IIM version | 1 |
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14e083020474e6d79bb57a7164492156a7a9e5d4
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