Claritas Fossae
Claritas Fossae is a densely-dissected highland terrain on the Tharsis Rise of Mars, located immediately south of the Tharsis Montes. The fossae of the Claritas Fossae region are many superposed swarms of graben.
Context
Claritas Fossae is a group of troughs in the Phoenicis Lacus and Thaumasia quadrangles of Mars, located at 31.5 S and 104.1 W. The structure is 2,050.0 km long and was named after a classical albedo feature name.[1] It was proposed that this area might be still tectonically active in relatively recent times.[2]
Geology
Long narrow depressions on Mars are called fossae. This term is derived from Latin; therefore fossa is singular and fossae is plural.[3] Troughs form when the crust is stretched until it breaks. The stretching can be due to the large weight of a nearby volcano. Fossae/pit craters are common near volcanoes in the Tharsis and Elysium regions.[4] A trough often has two breaks with a middle section moving down, leaving steep cliffs along the sides; such a trough is called a graben.[5]
Gallery
- Curved ridge that probably was formed by glacier, as seen by HiRISE under HiWish program
In culture
Claritas Fossae is the setting of the short story Loyal Soldier, part of the Mars Mars 2194 by Canadian author Jack Stornoway.
See also
- Fossa (geology)
- Geology of Mars
- HiRISE
- HiWish program
References
- ^ a b "Claritas Fossae". Gazetteer of Planetary Nomenclature. USGS Astrogeology Research Program. (Center Latitude: -27.89°, Center Longitude: 255.76°)
- ^ Pieterek, Bartosz; Brož, Petr; Hauber, Ernst (September 2024). "Recent faulting at the Claritas Rupes scarp on Mars". Icarus. 420: 116198. Bibcode:2024Icar..42016198P. doi:10.1016/j.icarus.2024.116198.
- ^ "Mars Art Gallery Martian Feature Name Nomenclature".
- ^ Skinner, J., L. Skinner, and J. Kargel. 2007. Re-assessment of Hydrovolcanism-based Resurfacing within the Galaxias Fossae Region of Mars. Lunar and Planetary Science XXXVIII (2007)
- ^ "HiRISE | Craters and Pit Crater Chains in Chryse Planitia (PSP_008641_2105)".
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