Eridania quadrangle

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Mars topography (MOLA dataset) HiRes (1).jpg
MC-29 Eridania 30–65° S 120–180° E Quadrangles Atlas
  • USGS-Mars-MC-29-EridaniaRegion-mola.png
  • PIA00189-MC-29-EridaniaRegion-19980605.jpg


The Eridania quadrangle once had a large lake. The region includes a wide variety of features that are widespread on Mars, but extremely rare on the Earth. Eridania has gullies, dust devil tracks, glaciers, craters, and gorgeous dunes. The region mainly includes heavily cratered highlands. Kepler Crater is the largest crater. Kepler Crater is named after Johannes Kepler who developed Kepler's laws of planetary motion.

In this article, some of the best pictures from a number of spacecraft will show what the landscape looks like in this region. The origins and significance of all features will be explained as they are currently understood.

The Eridania quadrangle is one of a series of 30 quadrangle maps of Mars used by the United States Geological Survey. The Eridania quadrangle is also referred to as MC-29 (Mars Chart-29).[1] The Eridania quadrangle lies between 30° and 65° south latitude and 180° and 240° west longitude (180-120 E). Most of the classic region named Terra Cimmeria is found within this quadrangle. It is named after a region on the Po River, Italy. The name was approved by the IAUP in 1958.Cite error: Closing </ref> missing for <ref> tag

Martian gullies

Labeled gully, as seen by HiRISE under HiWish program

Labeled gully, as seen by HiRISE under HiWish program


Martian gullies are small, incised networks of narrow channels and their associated downslope deposits. They are named for their resemblance to terrestrial gullies. First discovered on images from Mars Global Surveyor, they occur on steep slopes, especially on the walls of craters. Usually, each gully has an alcove at its head, a fan-shaped apron at its base, and a single thread of incised channel linking the two, giving the whole gully an hourglass shape.[2] They are believed to be relatively young because they have few, if any craters. On the basis of their form, aspects, positions, and location amongst and apparent interaction with supposedly ice-rich features, many researchers believed that the processes carving the gullies involve liquid water. However, with more observations and research this idea has changed. As soon as gullies were discovered, researchers began to image many gullies over and over, looking for possible changes. By 2006, some changes were found.[3] Later, with further analysis it was determined that the changes could have occurred with dry granular flows rather than being driven by flowing water.[4] [5] [6] With continued observations many more changes were found in Gasa Crater and others craters.[7] With more repeated observations, more and more changes were found; since the changes occur in the winter and spring, experts are tending to believe that gullies were formed from dry ice. Before-and-after images demonstrated the timing of this activity coincided with seasonal carbon-dioxide frost changes, and at temperatures that would not have allowed for liquid water. The conditions during gully formation are just about right to allow chunks of dry ice to slide down slopes. To aid the process is the fact that when dry ice frost changes to a gas, it may lubricate dry material to flow especially on steep slopes.[8] [9][10] In some years frost build up may be-as thick as 1 meter.

  • Gullies, as seen by HiRISE under HiWish program

  • Gullies

  • Wide view of gullies in a crater

  • Close view of gully Curved ridges may have formed by glaciers before the gullies were created.

  • Crater with gullies, as seen by HiRISE under HiWish program

  • Crater with gullies

  • Gullies, as seen by HiRISE Picture is about 1 km across.


Gasa Crater, as seen by CTX Note: Gasa Crater is the smaller crater. It is believed the impact that created Gasa occurred in a debris-covered glacier. Gasa Crater, as seen by CTX Note: Gasa Crater is the smaller crater. It is believed the impact that created Gasa occurred in a debris-covered glacier.


Gullies in Gasa Crater, as seen by HiRISE. 

                                    Gullies in Gasa Crater, as seen by HiRISE.

Dust devil tracks

Crater and dust devil tracks 

                                  Crater and dust devil tracks

Many areas on Mars, including Eridania, experience the passage of giant dust devils. A thin coating of fine bright dust covers most of the Martian surface. When a dust devil goes by it blows away the coating and exposes the underlying dark surface. Dust devils occur when the sun warms up the air near a flat, dry surface. The warm air then rises quickly through the cooler air and begins spinning while moving ahead. This spinning, moving cell may pick up dust and sand then leave behind a clean surface.[11] Dust devils have been seen from the ground and high overhead from orbit. They have even blown the dust off of the solar panels of the two Mars Exploration Rovers on Mars, thereby greatly extending their lives.[12] The twin Rovers were designed to last for 3 months, instead they lasted many years; Opportunity Rover explored Mars for over 14 years. The pattern of the tracks have been shown to change every few months.[13]

A study that combined data from the High Resolution Stereo Camera (HRSC) and the Mars Orbiter Camera (MOC) found that some large dust devils on Mars have a diameter of 700 meters and last at least 26 minutes.[14]


  • Kepler Crater showing dust devil tracks, as seen by Mars Global Surveyor

  • Pattern of large and small tracks made by giant dust devils as seen by Mars Global Surveyor, under the MOC Public Targeting Program. Location is 55.11 S and 196.63 W.

  • Campbell Crater, as seen by CTX camera (on Mars Reconnaissance Orbiter).

  • Dust devil tracks, as seen by CTX camera (on Mars Reconnaissance Orbiter). Note: this is an enlargement of the previous image of Campbell Crater.

Paleomagnetism

The Mars Global Surveyor (MGS) discovered magnetic stripes in the crust of Mars, especially in the Phaethontis and Eridania quadrangles (Terra Cimmeria and Terra Sirenum).[15] [16]

When molten rock containing magnetic material, such as hematite (Fe2O3), cools and solidifies in the presence of a magnetic field, it becomes magnetized and takes on the polarity of the background field. This magnetism is lost only if the rock is subsequently heated above a particular temperature (the Curie point which is 770  °C for iron). The magnetism left in rocks is a record of the magnetic field when the rock solidified.[17]

The magnetometer on MGS discovered 100 km wide stripes of magnetized crust running roughly parallel for up to 2000 km. These stripes alternate in polarity with the north magnetic pole of one pointing up from the surface and the north magnetic pole of the next pointing down.[18] When similar stripes were discovered on Earth in the 1960s, they were taken as evidence of plate tectonics. Researchers believe these magnetic stripes on Mars are evidence for a short, early period of plate tectonic activity.[19] When rocks became solid they retained the magnetism that existed at the time. A magnetic field of a planet is believed to be caused by fluid motions under the surface.[20] [21] [22] However, there are some differences, between the magnetic stripes on Earth and those on Mars. The Martian stripes are wider, much more strongly magnetized, and do not appear to spread out from a middle crustal spreading zone. Because the area containing the magnetic stripes is about 4 billion years old, it is believed that the global magnetic field probably lasted for only the first few hundred million years of Mars' life, when the temperature of the molten iron in the planet's core might have been high enough to mix it into a magnetic dynamo. There are no magnetic fields near large impact basins like Hellas. The shock of the impact may have erased the remnant magnetization in the rock. After the Hellas impact no magnetic fields existed. This fact tells us that there was only early magnetism.[23]

Some researchers have proposed that early in its history Mars exhibited a form of plate tectonics. At about 3.93 billion years ago Mars became a one plate planet with a superplume under Tharsis.[24] [25] [26]


Dunes

Dunes, including barchans are present in the Eridania quadrangle and in some pictures below. When there are perfect conditions for producing sand dunes, steady wind in one direction and just enough sand, barchan sand dunes form. Barchans have a gentle slope on the wind side and a much steeper slope on the lee side where horns or a notch often forms.[27] The whole dune may appear to move with the wind. Observing dunes on Mars can tell us how strong the winds are, as well as their direction. If pictures are taken at regular intervals, one may see changes in the dunes or possibly in ripples on the dune’s surface. On Mars dunes are often dark in color because they were formed from the common, volcanic rock basalt. In a dry environment, dark minerals in basalt, like olivine and pyroxene, do not break down as they do on Earth. Although rare, some dark sand is found on Hawaii which also has many volcanoes discharging basalt. Barchan is a Russian term because this type of dune was first seen in the desert regions of Turkistan.[28] Some of the wind on Mars is created when the dry ice at the poles is heated in the spring. At that time, the solid carbon dioxide (dry ice) sublimates or changes directly to a gas and rushes away at high speeds. Each Martian year 30% of the carbon dioxide in the atmosphere freezes out and covers the pole that is experiencing winter, so there is a great potential for strong winds.[29]

  • Hadley Crater, as seen by CTX camera (on Mars Reconnaissance Orbiter).

  • Dunes on floor of Hadley Crater, as seen by CTX camera (on Mars Reconnaissance Orbiter). Note: this is an enlargement of the previous image of Hadley Crater.

Dark dunes Dark dunes are composed of the igneous rock basalt. The dark box in the center of the photo shows the area enlarged in the next image. The scale is 500 meters long.


Dark dunes, as seen by HiRISE under HiWish program. Dark dunes are composed of the igneous rock basalt. The dark box in the center of the photo shows the area enlarged in the next image. The scale is 500 meters long.


  • Close up of dark dunes The image is a little more than 1 km in its longest dimension. The location of this image is shown in the previous image.

  • Dunes


  • Wide view of dunes near craters

  • Close, color view of dunes

Glacial features

Glaciers, loosely defined as patches of currently or recently flowing ice, are thought to be present across large but restricted areas of the modern Martian surface, and are inferred to have been more widely distributed at times in the past.[30] [31] Some glaciers on Mars have lost most of their ice, but they can be identified by the shape of the piles debris they left behind (called moraine).

  • Glacial features in Arrhenius Crater, as seen by HiRISE under the HiWish program. Arrows point to old glaciers.

  • Old glaciers in Cruls Crater, as seen by HiRISE under HiWish program.

  • Romer Lake's Elephant Foot Glacier in the Earth's Arctic, as seen by Landsat 8. This picture shows several glaciers that have the same shape as many features on Mars that are believed to also be glaciers.

  • Flow (Glacier)

Lake

The Eridania Basin, located near 180 E and 30 South, is thought to have contained a large lake with a depth of 1 km in places.[32] [33] The basin is composed of a group of eroded and connected topographically impact basins. The lake has been estimated to have an area of 3,000,000 square kilometers. Water from this lake entered the channel called Ma'adim Vallis which starts at the lake's north boundary.[34] It is surrounded by valley networks that all end at the same elevation, suggesting that they emptied into a lake.[35] Magnessium-rich clay minerals and opaline silica have been detected in the area.[36] These minerals are consistent with the presence of a large lake.[37]

  • Map showing estimated water depth in different parts of Eridania Sea This map is about 530 miles across.

  • Features around Eridania Sea labeled

Later studies found many other minerals that support the contention that a lake existed here. The minerals detected must have water to be formed. The spectrometer CRISM, onboard the Mars Reconnaissance Orbiter, found thick deposits, greater than 400 meters thick, that contained the minerals saponite, talc-saponite, Fe-rich mica (for example, glauconite-nontronite), Fe- and Mg-serpentine, Mg-Fe-Ca-carbonate and probable Fe-sulphide. The Fe-sulphide probably formed in deep water from water heated by volcanoes. Analyses from the Mars Reconnaissance Orbiter provided evidence of ancient hydrothermal seafloor deposits in Eridania basin, suggesting that hydrothermal vents pumped mineral-laden water directly into this ancient Martian lake.[38] [39]

  • Deep-basin deposits from the floor of Eridania Sea. The mesas on the floor are there because they were protected against intense erosion by deep water/ice cover. CRISM is the spectroscope on Mars Reconnaissance Orbiter. CRISM showed minerals may be from seafloor hydrothermal deposits. Life may have originated in this sea.

Diagram showing how volcanic activity may have caused deposition of minerals on floor of Eridania Sea. Chlorides were deposited along the shoreline by evaporation.


Diagram showing how volcanic activity may have caused deposition of minerals on floor of Eridania Sea. Chlorides were deposited along the shoreline by evaporation.

Craters

  • Crater floor with the shape of an odd face The box indicates where the next picture is located.

  • Close-up of a portion of a crater wall indicated in the previous photo. There seems to be grooves in the wall.

  • Surface on crater floor, as seen by HiRISE under HiWish program.

  • Martz Crater, as seen by CTXcamera (on Mars Reconnaissance Orbiter).

  • Gullies on central mound in Martz Crater, as seen by CTX camera (on Mars Reconnaissance Orbiter). Note: This is an enlargement of the previous image of Martz Crater.

Latitude dependent mantle

Much of the Martian surface is covered with a thick ice-rich, mantle layer that has fallen from the sky a number of times in the past.[40] [41][42] In some places a number of layers are visible in the mantle.[43] Some surfaces in Eridania are covered with this ice-rich mantling unit. In some places the surface displays a pitted or dissected texture; these textures are suggestive of material that once held ice that has since disappeared allowing the remaining soil to collapse into the subsurface.[44]

Close view of places covered and not covered by mantle layer which falls from the sky when climate changes 

  Close view of places covered and not covered by mantle layer which falls from the sky when climate changes


  • Wide view of crater with regions of latitude dependent mantle

  • Close view of crater with regions of latitude dependent mantle

Channels

There exists a great deal of evidence that water once flowed in river valleys and channels on Mars. Images of curved channels have been seen in images from Mars spacecraft dating back to the early seventies with the Mariner 9 orbiter.[45] [46] [47] [48] Vallis (plural valles) is the Latin word for 'valley. It is used in planetary geology for the naming of features on other planets, including what could be old river valleys that were discovered on Mars, when probes were first sent to Mars. The Viking Orbiters caused a revolution in our ideas about water on Mars; river valleys were found in many areas. Space craft cameras showed that floods of water broke through dams, carved deep valleys, eroded grooves into bedrock, and traveled thousands of kilometers.[49] [50] [51]

Channel cutting across trough, as seen by HiRISE under HiWish program The trough and channel are labeled. 

        Channel cutting across trough, as seen by HiRISE The trough and channel are labeled.


This channel has cut through some thick ground 

                        This channel has cut through some thick ground


  • Close view of channel that has cut deeply into the landscape

  • Channel on floor of crater

  • Channels, as seen by HiRISE under HiWish program

  • Channels These channels seem to disappear at times; they may be going under the ground for a time.

  • Channel on floor of a valley The small channel may have formed at some time after the larger valley; therefore, water may have been here more than once.

Other features in Eridania quadrangle

  • Map of Eridania quadrangle, with major craters labeled The small colored rectangles are spots that were imaged in high resolution with the Mars Global Surveyor camera.

  • Ariadne Colles Chaos The scale bar is 500 meters long.

  • Crater floor Rough surface was produced by ice leaving the ground. The crater has accumulated much ice that is covered by rocks and dirt.

  • Ridges exposed from under a dark layer

  • Layers

  • Layered feature in a crater

  • Layers in crater wall, as seen by HiRISE under HiWish program. Differeht colors mean different minerals.

Crater floor showing brain terrain, as seen by HiRISE under HiWish program Crater floor showing brain terrain, as seen by HiRISE under HiWish program Brain terrain, which looks like surface of a brain, occurs as ice leave the ground.

See also

Further reading

  • Lorenz, R. 2014. The Dune Whisperers. The Planetary Report: 34, 1, 8-14
  • Lorenz, R., J. Zimbelman. 2014. Dune Worlds: How Windblown Sand Shapes Planetary Landscapes. Springer Praxis Books / Geophysical Sciences.

External links

References

  1. ↑ Davies, M.E.; Batson, R.M.; Wu, S.S.C. “Geodesy and Cartography” in Kieffer, H.H.; Jakosky, B.M.; Snyder, C.W.; Matthews, M.S., Eds. Mars. University of Arizona Press: Tucson, 1992.
  2. ↑ Malin, M., Edgett, K. 2000. Evidence for recent groundwater seepage and surface runoff on Mars. Science 288, 2330–2335.
  3. ↑ Malin, M., K. Edgett, L. Posiolova, S. McColley, E. Dobrea. 2006. Present-day impact cratering rate and contemporary gully activity on Mars. Science 314, 1573_1577.
  4. ↑ Kolb, et al. 2010. Investigating gully flow emplacement mechanisms using apex slopes. Icarus 2008, 132-142.
  5. ↑ McEwen, A. et al. 2007. A closer look at water-related geological activity on Mars. Science 317, 1706-1708.
  6. ↑ Pelletier, J., et al. 2008. Recent bright gully deposits on Mars wet or dry flow? Geology 36, 211-214.
  7. ↑ NASA/Jet Propulsion Laboratory. "NASA orbiter finds new gully channel on Mars." ScienceDaily. ScienceDaily, 22 March 2014. www.sciencedaily.com/releases/2014/03/140322094409.htm
  8. ↑ http://www.jpl.nasa.gov/news/news.php?release=2014-226
  9. ↑ http://hirise.lpl.arizona.edu/ESP_032078_1420
  10. ↑ http://www.space.com/26534-mars-gullies-dry-ice.html
  11. ↑ http://hirise.lpl.arizona.edu/PSP_00481_2410
  12. ↑ http://marsrovers.jpl.nasa.gov/gallery/press/spirit/20070412a.html
  13. ↑ https://web.archive.org/web/20111028015730/http://mars.jpl.nasa.gov/spotlight/kenEdgett.html
  14. ↑ Reiss | first1 = D. | display-authors = etal | year = 2011 | title = Multitemporal observations of identical active dust devils on Mars with High Resolution Stereo Camera (HRSC) and Mars Orbiter Camera (MOC) | url = | journal = Icarus | volume = 215 | issue = | pages = 358–369 | doi=10.1016/j.icarus.2011.06.011 |
  15. ↑ Barlow, N. 2008. Mars: An Introduction to its Interior, Surface and Atmosphere. Cambridge University Press
  16. ↑ ISBN|978-0-387-48925-4
  17. ↑ http://sci.esa.int/science-e/www/object/index.cfm?fobjectid=31028&fbodylongid=645
  18. ↑ ISBN|978-0-521-82956-4
  19. ↑ http://www.space.com/scienceastronomy/mars-plate-tectonics-recent-past-110103.html
  20. ↑ Connerney, J. et al. 1999. Magnetic lineations in the ancient crust of Mars. Science: 284. 794-798.
  21. ↑ Langlais, B. et al. 2004. Crustal magnetic field of Mars Journal of Geophysical Research 109: EO2008
  22. ↑ Connerney | first1 = J. | display-authors = etal | year = 2005 | title = Tectonic implications of Mars crustal magnetism | url = | journal = Proceedings of the National Academy of Sciences of the USA | volume = 102 | issue = | pages = 14970–14975 | doi=10.1073/pnas.0507469102| pmc = 1250232 | pmid=16217034|
  23. ↑ Acuna | first1 = M. | display-authors = etal | year = 1999 | title = Global distribution of crustal magnetization discovered by the Mars Global Surveyor MAG/ER Experiment | url = | journal = Science | volume = 284 | issue = | pages = 790–793 | doi=10.1126/science.284.5415.790| bibcode = 1999Sci...284..790A |
  24. ↑ Baker, V., et al. 2017. THE WATERY ORIGIN AND EVOLUTION OF MARS: A GEOLOGICAL PERSPECTIVE. Lunar and Planetary Science XLVIII (2017). 3015.pdf
  25. ↑ Baker, V. et al. 2004. TENTATIVE THEORIES FOR THE LONG-TERM GEOLOGICAL AND HYDROLOGICAL EVOLUTION OF MARS. Lunar and Planetary Science XXXV (2004) 1399.pdf.
  26. ↑ Baker, V., et al. 2002. A THEORY FOR THE GEOLOGICAL EVOLUTION OF MARS AND RELATED SYNTHESIS (GEOMARS). Lunar and Planetary Science XXXIII (2002). 1586pdf.
  27. ↑ Pye|first=Kenneth|title=Aeolian Sand and Sand Dunes|year=2008|publisher=Springer|isbn=9783540859109|
  28. ↑ http://www.britannica.com/EBchecked/topic/53068/barchan
  29. ↑ Mellon, J. T. |author2=Feldman, W. C. |author3=Prettyman, T. H. |title=The presence and stability of ground ice in the southern hemisphere of Mars|journal=Icarus|year=2003|volume=169|issue=2|pages=324–340|
  30. ↑ Carr. "The Surface of Mars" Series: Cambridge Planetary Science (No. 6). ISBN|978-0-511-26688-1. Michael H. Carr, United States Geological Survey, Menlo Park
  31. ↑ Kieffer, H., et al. 1992. Mars. University of Arizona Press. Tucson. ISBN|0-8165-1257-4
  32. ↑ Irwin | first1 = R. | display-authors = etal | year = 2004| title = 2004 | doi = 10.1029/2004je002287 | journal = J. Geophys. Res. | volume = 109 | issue = | page = E12009 |
  33. ↑ https://www.uahirise.org/ESP_047916_1420
  34. ↑ Michalski, J., E. Noe Dobrea1, C. Weitz. 2015. Mg-rich clays and silica-bearing deposits in Eridania basin: Possible evidence for ancient sea deposits in Mars. 46th Lunar and Planetary Science Conference. 2754.pdf
  35. ↑ Baker, D., J. Head. 2014. 44th LPSC, abstract #1252
  36. ↑ Cuadros | first1 = J. | display-authors = etal | year = 2013 | title = Crystal-chemistry of interstratified Mg/Fe-clay minerals from seafloor hydrothermal sites| url = | journal = Chem. Geol. | volume = 360–361 | issue = | pages = 142–158 | doi=10.1016/j.chemgeo.2013.10.016|
  37. ↑ Michalski, J., E. Noe Dobrea1, C. Weitz. 2015. Mg-rich clays and silica-bearing deposits in Eridania basin: Possible evidence for ancient sea deposits in Mars. 46th Lunar and Planetary Science Conference. 2754.pdf
  38. ↑ https://www.jpl.nasa.gov/news/news.php?feature=6966 Mars Study Yields Clues to Possible Cradle of Life]. NASA News, 6 October 2017.
  39. ↑ Ancient hydrothermal seafloor deposits in Eridania basin on Mars | year=2017 | journal=Nat Commun | page=15978 | last1 = Michalski | first1 = JR | last2 = Dobrea | first2 = EZN | last3 = Niles | first3 = PB | last4 = Cuadros | first4 = J|
  40. ↑ Hecht, M. 2002. Metastability of water on Mars. Icarus 156, 373–386
  41. ↑ Mustard, J., et al. 2001. Evidence for recent climate change on Mars from the identification of youthful near-surface ground ice. Nature 412 (6845), 411–414.
  42. ↑ Pollack, J., D. Colburn, F. Flaser, R. Kahn, C. Carson, and D. Pidek. 1979. Properties and effects of dust suspended in the martian atmosphere. J. Geophys. Res. 84, 2929-2945.
  43. ↑ http://www.uahirise.org/ESP_048897_2125
  44. ↑ http://hirise.lpl.arizona.edu/PSP_006736_1325
  45. ↑ Baker, V. 1982. The Channels of Mars. Univ. of Tex. Press, Austin, TX
  46. ↑ Baker, V., R. Strom, R., V. Gulick, J. Kargel, G. Komatsu, V. Kale. 1991. Ancient oceans, ice sheets and the hydrological cycle on Mars. Nature 352, 589–594.
  47. ↑ Carr, M. 1979. Formation of Martian flood features by release of water from confined aquifers. J. Geophys. Res. 84, 2995–300.
  48. ↑ Komar, P. 1979. Comparisons of the hydraulics of water flows in Martian outflow channels with flows of similar scale on Earth. Icarus 37, 156–181.
  49. ↑ Kieffer|title=Mars|url=https://books.google.com/books?id=NoDvAAAAMAAJ%7Caccessdate=7 March 2011|date=1992|publisher=University of Arizona Press|
  50. ↑ Raeburn, P. 1998. Uncovering the Secrets of the Red Planet Mars. National Geographic Society. Washington D.C.
  51. ↑ Moore, P. et al. 1990. The Atlas of the Solar System. Mitchell Beazley Publishers NY, NY.
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