http://SaturnianCosmology.Org/ mirrored file For complete access to all the files of this collection see http://SaturnianCosmology.org/search.php ========================================================== Caloris Basin From Wikipedia, the free encyclopedia The *Caloris Basin*, also called *Caloris Planitia*, is an impact crater on Mercury about 1,550 km in diameter ,^[1] <#cite_note-newscientist30012008-0> one of the largest impact basins in the solar system . Caloris is Latin for /heat / and the basin is so-named because the Sun is almost directly overhead every second time Mercury passes perihelion . The crater is surrounded by a ring of mountains about two kilometers tall. It is the largest known crater on Mercury. Contents [hide ] * 1 Appearance <#Appearance> * 2 Formation <#Formation> * 3 Antipodal chaotic terrain and global effects <#Antipodal_chaotic_terrain_and_global_effects> * 4 Emissions of gas <#Emissions_of_gas> * 5 References <#References> * 6 See also <#See_also> [edit ] Appearance MESSENGER 's first image of the unseen side of Mercury from a distance of about 17,000 miles (27,000 km) cropped to highlight Caloris. The rim is hard to discern as the Sun is directly overhead, preventing shadows. The Caloris Basin was discovered on images taken by the Mariner 10 probe in 1974. It was situated on the terminator — the line dividing the daytime and nighttime hemispheres — at the time the probe passed by, and so half of the crater could not be imaged. Later, on January 15 , 2008 , one of the first photos of the planet taken by the MESSENGER probe revealed the crater in its entirety. Comparison of the original size estimation of the Caloris Basin (in yellow) with the size estimation based on new images from the MESSENGER probe (in blue). The crater was initially estimated to be about 1,300 km (810 miles) in diameter, though this was increased to 1,550 km based on subsequent images taken by MESSENGER .^[1] <#cite_note-newscientist30012008-0> It is ringed by mountains up to 2 km high. Inside the crater walls, the floor of the crater is filled by lava plains, similar to the maria of the Moon . Outside the walls, material ejected in the impact which created the basin extends for 1,000 km, and concentric rings surround the crater. Pantheon Fossae in Caloris Basin In the center of the basin is a region containing numerous radial troughs that appear to be extensional faults , with a 40 km crater located near the center of the pattern. The exact cause of this pattern of troughs is not currently known.^[1] <#cite_note-newscientist30012008-0> The feature is named Pantheon Fossae .^[2] <#cite_note-1> [edit ] Formation Bodies in the inner solar system experienced a heavy bombardment of large rocky bodies in the first billion years or so of the solar system. The impact which created the Caloris basin must have occurred after most of the heavy bombardment had finished, because fewer impact craters are seen on its floor than exist on comparably-sized regions outside the crater. Similar impact basins on the Moon such as the Mare Imbrium and Mare Orientale are believed to have formed at about the same time, possibly indicating that there was a 'spike' of large impacts towards the end of the heavy bombardment phase of the early solar system.^[3] <#cite_note-2> Based on MESSENGER's photographs, Caloris' age has been determined to be between 3.8 and 3.9 billion years.^[1] <#cite_note-newscientist30012008-0> [edit ] Antipodal chaotic terrain and global effects Hilly, lineated terrain at the antipode of the Caloris Basin Close up of the Chaotic Terrain The giant impact believed to have formed Caloris may have had global consequences for the planet. At the exact antipode of the basin is a large area of hilly, grooved terrain, with few small impact craters that are known as the Chaotic Terrain (also 'Weird Terrain'). It is thought by some to have been created as seismic waves from the impact converged on the opposite side of the planet.^[4] <#cite_note-3> This hypothetical impact is also believed to have triggered volcanic activity on Mercury, resulting in the formation of smooth plains.^[5] <#cite_note-4> Surrounding Caloris Basin is a series of geologic formations thought to have been produced by the basin's ejecta, collectively called the Caloris Group . [edit ] Emissions of gas Mercury has a very tenuous and transient atmosphere, containing small amounts of hydrogen and helium captured from the solar wind , as well as heavier elements such as sodium and potassium . These are thought to originate within the planet, being 'out-gassed' from beneath its crust. The Caloris Basin has been found to be a significant source of sodium and potassium, indicating that the fractures created by the impact facilitate the release of gases from within the planet. The Weird Terrain is also a source of these gases.^[6] <#cite_note-5> [edit ] References 1. ^ ^/*a*/ <#cite_ref-newscientist30012008_0-0> ^/*b*/ <#cite_ref-newscientist30012008_0-1> ^/*c*/ <#cite_ref-newscientist30012008_0-2> ^/*d*/ <#cite_ref-newscientist30012008_0-3> Shiga, David (2008-01-30). "Bizarre spider scar found on Mercury's surface" . NewScientist.com news service. http://space.newscientist.com/article/dn13257-bizarre-spider-scar-found-on-mercurys-surface.html. 2. *^ <#cite_ref-1>* MESSENGER: MErcury Surface, Space ENvironment, GEochemistry, and Ranging 3. *^ <#cite_ref-2>* Gault, D. E.; Cassen, P.; Burns, J. A.; Strom, R. G. (1977). "Mercury". /Annual Review of Astronomy and Astrophysics/ *15*: 97–126. doi :10.1146/annurev.aa.15.090177.000525 . 4. *^ <#cite_ref-3>* Schultz, P. H.; Gault, D. E. (1975). "Seismic effects from major basin formations on the moon and Mercury". /The Moon/ *12*: 159–177. doi :10.1007/BF00577875 . 5. *^ <#cite_ref-4>* Kiefer, W. S.; Murray, B. C. (1987). "The formation of Mercury's smooth plains". /Icarus/ *72*: 477–491. doi :10.1016/0019-1035(87)90046-7 . 6. *^ <#cite_ref-5>* Sprague, A. L.; Kozlowski, R. W. H.; Hunten, D. M. (1990). "Caloris Basin: An Enhanced Source for Potassium in Mercury's Atmosphere". /Science/ *249* (4973): 1140–1142. doi :10.1126/science.249.4973.1140 . PMID 17831982 .