Noctis Labyrinthus
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In this Viking 1 image, the canyons are filled with water ice fog from frost sublimated by the early morning sun. | |
| Coordinates | 7°00′S 102°12′W / 7.0°S 102.2°WCoordinates: 7°00′S 102°12′W / 7.0°S 102.2°W |
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| Length | 1,263.0 |
Noctis Labyrinthus, "the labyrinth of the night", is a region of Mars between Valles Marineris and the Tharsis upland.[1] It is located in the Phoenicis Lacus quadrangle. The region is notable for its maze-like system of deep, steep-walled valleys. The valleys and canyons of this region formed by faulting and many show classic features of grabens, with the upland plain surface preserved on the valley floor. In some places the valley floors are rougher, disturbed by landslides, and there are places where the land appears to have sunk down into pit-like formations.[2] It is thought that this faulting was triggered by volcanic activity in the Tharsis region.[3] Research described in December 2009 found a variety of minerals, including clays, sulfates, and hydrated silicas, in some of the layers.[4]
Gallery
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Noctis Labyrinthus in the lower right. The three large mountains on the left are Tharsis Montes
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Part of Noctis Labyrinthus taken with Mars Global Surveyor. Courtesy NASA/Malin Space Science Systems.
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Layers in the wall of Noctis Labyrinthus taken with Mars Global Surveyor. Courtesy NASA/Malin Space Science Systems.
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Layers in the lower portion of two neighbouring buttes within the Noctis Labyrinthus formation on Mars are visible in this image.
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Section of layers near top of Noctis Labyrinthus, as seen by HiRISE under HiWish program.
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Group of layers near the bottom of Noctis labyrinthus, as seen by HiRISE under HiWish program.
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Wide view of cliff with layers in Noctis Labyrinthus.
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Close-up of part of previous image of layers in Noctis Labyrinthus, as seen by HiRISE under HiWish program.
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Wide view of floor of Noctis Labyrinthus, as seen by HiRISE under HiWish program.
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Close-up of complex, dark dunes in the previous image of the floor of Noctis Labyrinthus, as seen by HiRISE under HiWish program.
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Close-up of some layers in wall of Noctis Labyrinthus, as seen by HiRISE under HiWish program.
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Layers on floor of Noctus Labyrinthus, as seen by HiRISE under HiWish program. Layers probably contain a variety of minerals that were formed with groundwater.
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Close-up of layers on floor of Noctus Labyrinthus, as seen by HiRISE under HiWish program. This is an enlargement from the center of the previous picture.
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Floor of Noctis Labyrinthus showing layered structures, as seen by HiRISE under HiWish program
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Layered mesa on floor of Noctis Labyrinthus, as seen by HiRISE under HiWish program Note: this is an enlargement of a previous image.
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Enlargement of edge of mesa on floor of Noctis Labyrinthus showing layers, as seen by HiRISE under HiWish program Note: this is an enlargement of a previous image.
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Enlargement of a light-toned structure on floor of Noctis Labyrinthus, as seen by HiRISE under HiWish program Note: this is an enlargement of a previous image.
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Light-toned butte on floor of Noctis Labyrinthus, as seen by HiRISE under HiWish program Note: this is an enlargement of a previous image.
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Thin dark layers on floor of Noctis Labyrinthus, as seen by HiRISE under HiWish program Note: this is an enlargement of a previous image.
References
- ↑ "Noctis Labyrinthus". USGS planetary nomenclature page. USGS. Retrieved 2013-10-17.
- ↑ http://cmex.ihmc.us/cmex/data/voviews/Canyons/Noctis.htm
- ↑ Mars Odyssey Mission THEMIS: Feature Image: Noctis Labyrinthus Landslides
- ↑ "Trough deposits on Mars point to complex hydrologic past". Sciencedaily.com. 2009-12-17. Retrieved 2013-07-16.
External links
- "Images from ESA Mars Express". European Space Agency. December 3, 2007. Retrieved 2007-12-03.
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