Sirenum Fossae

From Wikipedia, the free encyclopedia
Jump to: navigation, search
Sirenum Fossae
Close up view to eastern part of Sirenum Fossae based on day THEMIS.png
Part of Sirenum Fossae based on THEMIS day-time image
Coordinates 34°54′S 160°54′W / 34.9°S 160.9°W / -34.9; -160.9Coordinates: 34°54′S 160°54′W / 34.9°S 160.9°W / -34.9; -160.9

Sirenum Fossae is a long trough in several quadrangles including Memnonia quadrangle and Phaethontis quadrangle of Mars, centered at 35.57° south latitude and 197.26° west longitude.[1] Sirenum Fossae is 2,735 km long and was named after a classical albedo feature name.[2] Troughs on Mars like this one are called Fossae. Sirenum Fossae is believed to have formed by movement along a pair of faults causing a center section to drop down. This kind of feature is called a graben.

Gullies[edit]

The pictures below show gullies in Sirenum Fossae. Gullies occur on steep slopes, especially on the walls of craters. Gullies are believed to be relatively young because they have few, if any craters. Moreover, they lie on top of sand dunes which themselves are considered to be quite young. Usually, each gully has an alcove, channel, and apron. Some studies have found that gullies occur on slopes that face all directions,[3] others have found that the greater number of gullies are found on poleward facing slopes, especially from 30-44 S.[4]

For years, many believed that gullies were formed by running water, but further observations demonstrate that they may be formed by frozen carbon dioxide (dry ice). Recent studies describe using the High Resolution Imaging Science Experiment (HiRISE) camera on MRO to examine gullies at 356 sites, starting in 2006. Thirty-eight of the sites showed active gully formation. Before-and-after images demonstrated the timing of this activity coincided with seasonal carbon dioxide frost and temperatures that would not have allowed for liquid water. When dry ice frost changes to a gas, it may lubricate dry material to flow especially on steep slopes.[5][6][7] In some years frost, perhaps as thick as 1 meter, triggers avalanches. This frost contains mostly dry ice, but also has tiny amounts of water ice.[8]

See also[edit]

References[edit]