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Recent imaging of auroras on Mars have led to a correlation between auroras and remnant magnetization of susceptible minerals in Mars' crust, that create miniature magnetospheres. From observations, it appears that the majority of remaining magnetization of Mars' crustal minerals occurs in the southern hemisphere <ref>, , , , </ref>, with little to no remnant magnetization in the northern hemisphere. Another theory as to why the "spiders" formed in the southern region and not in the northern relates to how charged particles from solar radiation interact with magnetic field lines. Charged particles tend to flow along magnetic field lines. Due to the south polar remnant magnetic fields being significantly stronger than the small or non-existent northern magnetic fields, charged particles would interact different with the south pole than the north <ref></ref>. The fact that the south pole is aligned closer to the sun at perihelion, thus receiving more solar radiation and charged particles could factor in as well. Recent imaging of auroras on Mars have led to a correlation between auroras and remnant magnetization of susceptible minerals in Mars' crust, that create miniature magnetospheres. From observations, it appears that the majority of remaining magnetization of Mars' crustal minerals occurs in the southern hemisphere <ref>, , , , </ref>, with little to no remnant magnetization in the northern hemisphere. Another theory as to why the "spiders" formed in the southern region and not in the northern relates to how charged particles from solar radiation interact with magnetic field lines. Charged particles tend to flow along magnetic field lines. Due to the south polar remnant magnetic fields being significantly stronger than the small or non-existent northern magnetic fields, charged particles would interact different with the south pole than the north <ref></ref>. The fact that the south pole is aligned closer to the sun at perihelion, thus receiving more solar radiation and charged particles could factor in as well.


== Cultural References == == Cultural references ==
'']'' features the Martian spiders as unique flora on its mars themed maps.
David Bowie's Martian character Ziggy Stardust has a band named the 'Spiders from Mars' in ]. The two terms, however, are unrelated as the band was around long before the "spider" formations were discovered on Mars.

1997's ] features the Martian spiders as unique flora on its mars themed maps.


==References== ==References==

Revision as of 23:44, 2 August 2008

Original caption released with image: A delicate pattern, like that of a spider web, appears on top of the Mars residual polar cap, after the seasonal carbon-dioxide ice slab has disappeared. Next spring, these will likely mark the sites of vents when the carbon-dioxide ice cap returns. This Mars Global Surveyor, Mars Orbiter Camera image is about 3-kilometers wide (2-miles). Image courtesy of NASA/JPL-Caltech.

Martian "spiders" are geological formations thus far unique to the south polar region of Mars. These structures have not been found in the north polar region or any other region of Mars to date. They appear as the carbon dioxide ice cap at the Martian south pole sublimates into carbon dioxide gas during the Martian spring and the surface below is revealed.

The formations, when viewed individually, form a round lobed structure reminiscent of a spider web. They generally radiate outward in lobes from a central point . The central point is sometimes, but not always, a crater . The formation is similar in its branching appearance to diffusion-limited aggregation. Similar branching patterns are also seen in watershed erosion regimes as well as the branches, roots and leaf veins of plants.

Causes

It is not yet fully understood how the formations occur, or why they appear to only form in the south polar region. Theories include:

  1. Dry venting of CO2 gas and dust up joints.
  2. Head-ward erosion: Fluid derived from sub-surface layers is expelled up fissures eroding joints to create tributaries capped with mud-like material and/or ice.
  3. Modified Clathrate-hydrate model: Structures form as the outside of the flow chills.
  4. Hydrothermal-type sources, and
  5. Magma pressurizes overlying fluids, expelling mud-like material, hydrothermal fluids or basalt. Other explanations have been offered by NASA, astrophysicists, astrogeologists and astrobiologists including water erosion in Mars' history , carbon dioxide / sand geysers

It has also previously been suggested that these structures had a volcanic cause or were simply warm patches of bare ground, however recent thermal imaging by NASA has revealed that these structures are generally as cold as the dry ice that covers the area during the Martian southern hemispheric winter .

From the NASA press release (dated Aug 16, 2006) "An earlier theory proposed that the spots were patches of warm, bare ground exposed as the ice disappeared. However, the camera on Odyssey, which sees in both infrared and visible-light wavelengths, discovered that the spots are nearly as cold as the carbon dioxide ice, suggesting they were just a thin layer of dark material lying on top of the ice and kept chilled by it." The morphology of spiders appears to be controlled by bedding and local jointing of the rocks; implying that expelled fluids are derived from within a few hundred meters of the surface. Some spider-ravines modify, some destroy and others create crust in a dynamic near-surface process that extensively reworks the terrain creating/destroying surface layers. This process is rapid, happening in the space of a few days, weeks or months. .

Additional Information

It is not known why the "spider" formations appear to occur only in specific regions of Mars' south pole, but not in corresponding regions of Mars' north pole or other regions of the planet. There are, however, several differences between the Martian north and south poles which may factor in.

Mars' orbit around the sun is not symmetrical, nor circular. Mars has an elliptic orbit. At aphelion (the point in its orbit furthest from the sun), Mars is 249,228,730 km (154,863,553 mi) away from the sun. At perihelion (the point in its orbit closest to the sun), Mars is 206,644,545 km (128,402,967 mi) away from the sun. Mars reaches perihelion during the south polar summer and north polar winter. Mars reaches aphelion during the north polar summer and south polar winter. For this reason, the south pole receives considerably more direct energy from the sun during its summer than the north pole receives during its summer. The difference in energy received is due to the difference in intensity of radiated energy per square unit of surface area at the considerably different distances. One theory as to why the south pole develops "spiders" but the north does not relates to the difference in heating patterns of the carbon dioxide ice in the polar CO2 ice caps during the respective south and north polar springs and/or summers.

Recent imaging of auroras on Mars have led to a correlation between auroras and remnant magnetization of susceptible minerals in Mars' crust, that create miniature magnetospheres. From observations, it appears that the majority of remaining magnetization of Mars' crustal minerals occurs in the southern hemisphere , with little to no remnant magnetization in the northern hemisphere. Another theory as to why the "spiders" formed in the southern region and not in the northern relates to how charged particles from solar radiation interact with magnetic field lines. Charged particles tend to flow along magnetic field lines. Due to the south polar remnant magnetic fields being significantly stronger than the small or non-existent northern magnetic fields, charged particles would interact different with the south pole than the north . The fact that the south pole is aligned closer to the sun at perihelion, thus receiving more solar radiation and charged particles could factor in as well.

Cultural references

Total Annihilation features the Martian spiders as unique flora on its mars themed maps.

References

  1. (Spiders on Earth and Mars. AIG News #85, page 21.)
  2. Photographic examples: 1, 2, 3
  3. Simulations of Geyser-Type Eruptions in Cryptic Region of Mars' South Polar Cap, Spiders: Water Driven Erosive Structures in the Southern Hemisphere of Mars, Martian Spiders as feasible water-driven erosive structures.
  4. NASA Findings Suggest Jets Bursting From Martian Ice Cap, Simulation of Geyser-Type Eruptions in Cryptic Region of Mars' South Pole
  5. [http://www.jpl.nasa.gov/news/news.cfm?release=2006-100 NASA Findings Suggest Jets Bursting From Martian Ice Cap ]
  6. [http://spsr.utsi.edu/articles/ness.pdf Peter K Ness and Greg M Orme. Spider-Ravine Models and Plant-like Features on Mars - Possible Geophysical and Biogeophysical Modes of Origin and Planet-like Features on Mars JBIS, Vol. 55, pp.85-108.]
  7. Hundreds Of Auroras Detected On Mars, , , ,
  8. The Solar Wind at Mars

See also

External links

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