Dark slope streaks

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Dark Slope Streaks

Dark slope streaks, as seen by HiRISE


Perhaps, some of the prettiest landscapes on Mars, dark slope streaks are found on dust-covered slopes, particular near the equator.[1] However, much of their beauty is from the way pictures are processed. To a human standing on Mars, streaks would not appear very dark. Each image has the darkest part set to black, but the darkest thing may not really be that dark. Streaks are only about 10% darker than their surroundings. [2] Scientists do this to more easily see detail.

  • Close view of dark slope streaks

Appearance

Typically, streaks begin at a small point high on a steep slope, such as a crater wall.[3] And then they greatly widen and sometimes divide into finger-like extensions (digitation). Obstacles, such as boulders, may cause an individual streak to split into two separate streaks or eventually form a braided (anastomosing) pattern.[4] Many have a fan shape. [5]

  • Streak being affected by boulders Arrows indicate boulders and resulting effect on streak.

  • Close view of streak showing boulders causing streak to divide

Streaks may be hundreds of meters long with a width of 20 to 200 meters. Indeed, some can be over 2 kilometers long. [6] [7] [8]

How long do they last?

Thanks to the many excellent cameras that we have placed in orbit over many decades, we have a history of how the Martian surface changes. Dark slope streaks are some of the most changing parts of Mars. They were discovered in Viking Orbiter pictures from the 1970,[9] [10] When images from Mars Global Surveyor (MGS) and Mars Reconnaissance Orbiter (MRO) spacecraft are examined, the life history of streaks can be precisely determined.[11] [12] [13] [14] [15]

New slope streaks formed near Apollinaris Mons between February 1998 and November 1999, as seen by Mars Orbital Camera (MOC).

One analysis concluded that 70 streaks per day may form on the planet. The research team compared overlapping images from Mars Global Surveyor Mars Orbiter Camera that were spaced days to years apart. [16] Dark slope streaks are constantly forming and fading. The darker ones are the youngest. Fading is accomplished by settling of bright dust in the Martian atmosphere. When researches looked at a small area (Lycus Sulci) on Mars with both Viking images and recent CTX images from the Mars Reconnaissance Orbiter, they found that the ones seen in Viking photos were gone, however, new streaks have taken their place. Their calculations indicated that slope streaks last about 40 years [17] From time to time the entire globe of Mars is enveloped in a dust storm. Many, perhaps most streaks and other features are erased during those periods.[18] [19]

  • Young and old dark slope streaks with origins labeled.

  • Mars without a dust storm on June 2001 (on left) and with a global dust storm on July 2001 (on right), as seen by Mars Global Surveyor

What causes dark slope streaks?

Although many ideas have been put forward to explain slope streaks, the general opinion today is that they are simply avalanches of bright dust.[20] Nearly all of Mars is covered with a thin, bright dust. On steep slopes this layer of dust can move away and reveal a dark surface. The dark volcanic rock basalt lies under the lighter-toned dust which falls out of the atmosphere. With the long term observations from orbit, researchers have noticed that strikes by meteorites can start the process of slope formation.[21] [22] Moreover, even the air blast from an oncoming strike can trigger clusters of slopes to form.[23]

  • New dark slope streak that was triggered by an impact Location is the Arabia quadrangle

Other slope features

Several features are common on slopes on Mars. The surface of Mars is billions of years old in most places. Consequently, it has accumulated many steep slopes, especially in craters and canyons. Although streaks, gullies, and recurring slope lineae all occur on slopes, they have different origins. Martian gullies show up in certain zones. However, unlike dark slope streaks they go fairly deep into the surface and are not erased by falling dust over time. Their origin is still debated. For over a decade they were believed to be formed by recent, flowing water.

Image of gullies with main parts labeled. The main parts of a Martian gully are alcove, channel, and apron. Picture was taken by HiRISE under HiWish program.

[24] [25] [26] [27] Now, new observations suggest that gullies are being made today by chunks of dry ice moving down steep slopes in the spring. [28] [29] [30] [31] [32] [33] [34] [35] As the map below shows gullies and streaks are found in different areas on the planet.

  • Map showing locations of gullies (brown) and streaks (pink)

Like gullies and streaks, recurring slope lineae are seen on steep slopes, but they are smaller, more narrow, and straighter. Since they seem to lengthen as the temperature increases, they were believed to be involved with liquid water. [36] [37] [38] [39] [40] Nevertheless, later studies showed that very little water, if any, could be involved.[41] [42]

  • Recurrent slop lineae, as seen by HiRISE

References

  1. ↑ Chuang, F.C.; Beyer, R.A.; Bridges, N.T. (2010). Modification of Martian Slope Streaks by Eolian Processes. Icarus, 205 154–164.
  2. ↑ Sullivan, R. et al. 2001. Mass Movement Slope Streaks Imaged by the Mars Orbiter Camera. J. Geophys. Res., 106(E10), 23,607–23,633.
  3. ↑ Schorghofer, N.; Aharonson, O.; Khatiwala, S. 2002. Slope Streaks on Mars: Correlations with Surface Properties and the Potential Role of Water. Geophys. Res. Lett., 29(23), 2126.
  4. ↑ Chuang, F.C. et al. 2007. HiRISE Observations of Slope Streaks on Mars. Geophys. Res. Lett., 34 L20204.
  5. ↑ Sullivan, R. et al. 2001. Mass Movement Slope Streaks Imaged by the Mars Orbiter Camera. J. Geophys. Res., 106(E10), 23,607–23,633.
  6. ↑ Sullivan, R. et al. 2001. Mass Movement Slope Streaks Imaged by the Mars Orbiter Camera. J. Geophys. Res., 106(E10), 23,607–23,633.
  7. ↑ Chuang, F.C.; Beyer, R.A.; Bridges, N.T. 2010. Modification of Martian Slope Streaks by Eolian Processes. Icarus, 205 154–164.
  8. ↑ Baratoux, D. et al. 2006. The Role of the Wind-Transported Dust in Slope Streaks Activity: Evidence from the HRSC Data. Icarus, 183 30–45.
  9. ↑ Morris, E.C. (1982). Aureole Deposits of the Martian Volcano Olympus Mons. J. Geophys. Res., 87(B2), 1164–1178.
  10. ↑ Ferguson,H.M.; Lucchitta, B.K. (1984). Dark Streaks on Talus Slopes, Mars in Reports of the Planetary Geology Program 1983, NASA Tech. Memo., TM-86246, pp. 188–190. https://ntrs.nasa.gov/archive/nasa/casi.ntrs.nasa.gov/19840015363_1984015363.pdf.
  11. ↑ Sullivan, R. et al. (2001). Mass Movement Slope Streaks Imaged by the Mars Orbiter Camera. J. Geophys. Res., 106(E10), 23,607–23,633.
  12. ↑ Chuang, F.C. et al. 2007. HiRISE Observations of Slope Streaks on Mars. 'Geophys. Res. Lett. 34 L20204.
  13. ↑ Dundas, C. 2018. HIRISE OBSERVATIONS OF NEW MARTIAN SLOPE STREAKS. 49th Lunar and Planetary Science Conference 2018 (LPI Contrib. No. 2083). 2026.pdf
  14. ↑ Malin, M.C.; Edgett, K.S. (2001). Mars Global Surveyor Mars Orbiter Camera: Interplanetary cruise through primary mission. J. Geophys. Res., 106(E10), 23,429–23,570.
  15. ↑ Edgett, K.S.; Malin, M.C.; Sullivan, R.J.; Thomas, P.; Veverka, J. (2000). Dynamic Mars: New Dark Slope Streaks Observed on Annual and Decadal Time Scales. 31st Lunar and Planetary Science Conference, Abstract #1058. http://www.lpi.usra.edu/meetings/lpsc2000/pdf/1058.pdf.
  16. ↑ Aharonson, O.; Schorghofer, N.; Gerstell, M.F. (2003). Slope Streak Formation and Dust Deposition Rates on Mars. J. Geophys. Res., 108(E12), 5138, doi:10.1029/2003JE002123.
  17. ↑ Bergonio, J., K. Rottas, and N. Schorghofer. 2013. Properties of martian slope streak populations: 225. Icarus: 194-199.
  18. ↑ Aharonson, O.; Schorghofer, N.; Gerstell, M.F. 2003. S lope Streak Formation and Dust Deposition Rates on Mars. J. Geophys. Res., 108(E12), 5138, doi:10.1029/2003JE002123.
  19. ↑ Schorghofer, Aharonson, O.; Gerstell, M.F.; Tatsumi, L. 2007. Three Decades of Slope Streak Activity on Mars. Icarus: 191, 132–140. doi:10.1016/j.icarus.2007.04.026.
  20. ↑ Treiman, A.H.; Louge, M.Y. (2004). Martian Slope Streaks and Gullies: Origins as Dry Granular Flows. 35th Lunar and Planetary Science Conference, Abstract #1323. http://www.lpi.usra.edu/meetings/lpsc2004/pdf/1323.p
  21. ↑ http://www.uahirise.org/epo/nuggets/dust-avalanche.pdf
  22. ↑ https://hirise.lpl.arizona.edu/ESP_054066_1920
  23. ↑ Kaylan J. Burleigh, Henry J. Melosh, Livio L. Tornabene, Boris Ivanov, Alfred S. McEwen, Ingrid J. Daubar. 2012. Impact air blast triggers dust avalanches on Mars Icarus: 217 (1) 194 doi:10.1016/j.icarus.2011.10.026
  24. ↑ Malin, M.; Edgett, K. (2000). "Evidence for recent groundwater seepage and surface runoff on Mars". Science. 288: 2330–2335.
  25. ↑ Luu, K., et al. 2018. GULLY FORMATION ON THE NORTHWESTERN SLOPE OF PALIKIR CRATER, MARS 49th Lunar and Planetary Science Conference 2018 (LPI Contrib. No. 2083). 2650.pdf
  26. ↑ Hamid, S., V. Gulick. 2018. GEOMORPHOLOGICAL ANALYSIS OF GULLIES ALONG WESTERN SLOPES OF PALIKIR CRATER. 49th Lunar and Planetary Science Conference 2018 (LPI Contrib. No. 2083). 2644.pdf
  27. ↑ Tyler Paladin, T., et al. 2018. INSIGHTS INTO THE FORMATION OF GULLIES IN ASIMOV CRATER, MARS. 49th Lunar and Planetary Science Conference 2018 (LPI Contrib. No. 2083). 2889.pdf
  28. ↑ Dundas, C., S. Diniega, A. McEwen. 2015. Long-term monitoring of martian gully formation and evolution with MRO/HiRISE. Icarus: 251, 244–263
  29. ↑ Fergason, R., C. Dundas, R. Anderson. 2015. IN-DEPTH REGIONAL ASSESSMENT OF THERMOPHYSICAL PROPERTIES OF ACTIVE GULLIES ON MARS. 46th Lunar and Planetary Science Conference. 2009.pdf
  30. ↑ Dundas, C. et al. 2016. HOW WET IS RECENT MARS? INSIGHTS FROM GULLIES AND RSL. 47th Lunar and Planetary Science Conference (2016) 2327.pdf.
  31. ↑ Vincendon, M. 2015. Identification of Mars gully activity types associated with ice composition.JGR:120, 1859–1879.
  32. ↑ Raack, J.; et al. (2015). "Present-day seasonal gully activity in a south polar pit (Sisyphi Cavi) on Mars". Icarus. 251: 226–243. Bibcode:2015Icar..251..226R. doi:10.1016/j.icarus.2014.03.040.
  33. ↑ http://www.uahirise.org/ESP_044327_1375
  34. ↑ C. Pilorget, C., F. Forget. 2015. "CO2 Driven Formation of Gullies on Mars." 46th Lunar and Planetary Science Conference. 2471.pdf
  35. ↑ Pilorget, C.; Forget, F. (2016). "Formation of gullies on Mars by debris flows triggered by CO2 sublimation". Nature Geoscience. 9: 65–69. Bibcode:2016NatGe...9...65P.
  36. ↑ McEwen, A. et al. 2011. Seasonal Flows on Warm Martian Slopes. Science, 333(6043), 740–743. doi:10.1126/science.1204816 PMID 21817049. http://www.sciencemag.org/content/333/6043/740.
  37. ↑ Mann, Adam (18 February 2014). "Strange Dark Streaks on Mars Get More and More Mysterious". Wired. Retrieved 18 February 2014.
  38. ↑ Chang, K. 2011. "Scientists Find Signs Water Is Flowing on Mars," New York Times, August 4, A13. https://www.nytimes.com/2011/08/05/science/space/05mars.html?_r=1&ref=marsplanet.
  39. ↑ HiRISE website. Seasonal Flows on Warm Martian Slopes. http://hirise.lpl.arizona.edu/sim/science-2011-aug-4.php.
  40. ↑ McEwen, A. Ojha L.; Dundas C.; Mattson, S.; Byrne S.; Wray J.; Cull S.; Murchie S. 2011. Transient Slope Lineae: Evidence for Summertime Briny Flows on Mars? 42nd Lunar and Planetary Science Conference, Abstract #2314. http://www.lpi.usra.edu/meetings/lpsc2011/pdf/2314.pdf.
  41. ↑ Dundas, C., et al. 2017. Granular Flows at Recurring Slope Lineae on Mars Indicate a Limited Role for Liquid Water. Nature Geoscience. Nov. 20. [1].
  42. ↑ Schaefer, E., et al. 2018. A case study of recurring slope lineae (RSL) at Tivat crater: Implications for RSL origins. Icarus: In press. https://doi.org/10.1016/j.icarus.2018.07.014

See also

External links

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