Aeolis quadrangle

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MC-23 Aeolis 0–30° S 135–180° E Quadrangles Atlas

Article written by Jim Secosky. Jim is a retired science teacher who has used the Hubble Space Telescope, the Mars Global Surveyor, and HiRISE.

  • Labeled topo map of Aeolis quadrangle Colors indicate elevation

  • Image of the Aeolis Quadrangle (MC-23). The northern part contains Elysium Planitia. The northeastern part includes Apollinaris Patera. The southern part mostly contains heavily cratered highlands.


The Aeolis quadrangle is one of a series of 30 quadrangle maps of Mars used by the United States Geological Survey (USGS) Astrogeology Research Program. The Aeolis quadrangle is also referred to as MC-23 (Mars Chart-23).[1] The Aeolis quadrangle covers 180° to 225° W (180-135 E) and 0° to 30° south on Mars, and contains parts of the regions Elysium Planitia and Terra Cimmeria. A small part of the Medusae Fossae Formation lies in this quadrangle.

The name refers to the name of a floating western island of Aiolos, the ruler of the winds. In Homer's account, Odysseus received the west wind Zephyr here and kept it in bags, but the wind got out.[2]

It is famous as the site of two spacecraft landings: the Spirit Rover rover landing site (14.5718 S and 175.4785E {184.525 W }) in Gusev Crater|Gusev (January 4, 2004), and the Curiosity Rover rover in Gale Crater (4.591817 S and 137.440247 E {222.55973 W}) (August 6, 2012).[3] 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.


Wide view of Mt. Sharp 


                Wide view of Mt. Sharp as seen by Curiosity which is exploring Gale Crater


Major Features

A large, ancient river valley, called Ma'adim Vallis, enters at the south rim of Gusev Crater, so Gusev Crater was believed to be an ancient lake bed. However, later it was discovered that a volcanic flow covered up the lakebed sediments.[4] The covering material may have come from Apollinaris Patera, a large volcano, which lies directly north of Gusev Crater.[5] Gale Crater, in the northwestern part of the Aeolis quadrangle, is of special interest to geologists because it contains a 2–4 km (1.2–2.5 mile) high mound of layered sedimentary rocks, named Aeolis Mons, but later changed to "Mount Sharp" by NASA in honor of Robert P. Sharp (1911–2004), a planetary scientist of early Mars missions.[6] [7] [8] [9]

Some regions in the Aeolis quadrangle show inverted relief.[10] In these locations, a stream bed may be a raised feature, instead of a valley. The inverted former stream channels may be caused by the deposition of large rocks or due to cementation of material in the channel. In either case erosion would erode the surrounding land but leave the old channel as a raised ridge because the ridge will be more resistant to erosion

Yardangs are another feature found in this quadrangle They are generally visible as a series of parallel linear ridges, caused by the prevailing wind.

What we learned from the Spirit Rover

Many forms of evidence from Spirit’s instruments pointed to the past presence of water. Some minerals that were detected had to have water for their formation. Analysis of rock compositions supported the notion that the rocks have been slightly altered by tiny amounts of water. Outside coatings and cracks inside the rocks suggest water deposited minerals (maybe bromine compounds). [11]

The rock called "Adirondack." It was the first rock to be examined by Spirit
Cross-sectional drawing of a typical rock from the plains of Gusev crater. Most rocks contain a coating of dust and one or more harder coatings. Veins of water-deposited veins are visible, along with crystals of olivine. Veins may contain bromine salts.


Spirit’s instruments found that rocks on the plains of Gusev are a type of basalt. They contain the minerals olivine, pyroxene, plagioclase, and magnetite. They look like volcanic basalt as they are fine-grained with irregular holes .[12] [13] Some soils showed fairly high levels of nickel; probably from meteorites.[14] Dust in Gusev Crater was determined to be the same as dust all around the planet. All the dust was magnetic. Since one of the magnets was able to completely divert all the dust, it was concluded that all Martian dust is magnetic.[15] Studies led scientists to conclude that magnetism was caused by the mineral magnetite-- especially magnetite that contained the element titanium. The spectra of the dust was similar to spectra of bright, low thermal inertia regions like Arabia and Tharsis that have been detected by orbiting satellites. Low thermal inertia means that the material does not hold its heat very long after the sun goes down. Generally, rocks have high thermal inertia, while sand has a low thermal inertia. A thin layer of dust, maybe less than one millimeter thick, covers all surfaces. Besides being magnetic, some part contains a small amount of chemically bound water.[16] [17] One type of soil, called Paso Robles, from the Columbia Hills, may be an evaporate deposit since it contains large amounts of sulfur, phosphorus, calcium, and iron.[18] Results from Spirits’ instruments of rocks on the plains show they contain the minerals pyroxene, olivine, plagioclase, and magnetite. The amounts and types of minerals found lead to a classification of primitive basalts—also called picritic basalts. They are comparable to ancient terrestrial rocks called basaltic komatiites. Rocks of the plains also resemble the basaltic shergottites, meteorites which came from Mars. [19] Plain’s rocks have been very slightly altered, probably by thin films of water that made them softer. Water also created veins of light colored material that may be bromine compounds, as well as coatings or rinds.[20] [21] It is commonly thought that Mars was first covered with the dark rock basalt. Over billions of years, the original rocks were broken down. By studying what minerals the beginning rocks turned into, we can tell how much water was involved and also the pH of the water. Coatings on the rocks may have taken place because they were buried and interacted with thin films of water and dust. One sign that they were altered was that it was easier to grind these rocks compared to the same types of rocks found on Earth. The first rock that Spirit studied was Adirondack. It turned out to be typical of the other rocks on the plains.

First color picture from Gusev crater. Rocks were found to be basalt. Everything was covered with a fine dust that Spirit determined was magnetic because of the mineral magnetite.


First color picture from Gusev crater. Rocks were found to be basalt. Everything was covered with a fine dust that Spirit determined was magnetic because of the mineral magnetite.


A variety of rocks were found and examined in the Columbia Hills.[22] All of the rocks in Columbia Hills show various degrees of alteration due to aqueous fluids.[23] They are enriched in the elements phosphorus, sulfur, chlorine, and bromine—all of which can be carried around in water solutions. The Columbia Hills’ rocks contain basaltic glass, along with varying amounts of olivine and sulfates.[24] [25] The olivine abundance varies indirectly with the sulfate abudance. This is exactly what is expected because water breaks down olivine but helps to produce sulfates.

Wide view from Bonneville Crater. Hills on right hills nicknamed the "Columbia Hills” where Spirit eventually drove to.

Wide view from Bonneville Crater Hills on right hills nicknamed the "Columbia Hills” where Spirit eventually drove to.


Clovis rock types are especially interesting because the Mössbauer spectrometer(MB) detected goethite in it.[26] Goethite forms only in the presence of water, so its discovery is the first direct evidence of past water in the Columbia Hills's rocks. In addition, the MB spectra of rocks and outcrops displayed a strong decline in olivine presence, [27] although the rocks probably once contained much olivine. Olivine breaks down in the presence of water; therefore, water must have been present to reduce the amount of Olivine.[28] Sulfate was found, and it needs water to be produced. The Independence class of rocks showed some signs of clay (perhaps montmorillonite a member of the smectite group). Anytime we find clay we know that water most have been around for a while. Towards the middle of the six-year mission (a mission that was supposed to last only 90 days), large amounts of pure silica were discovered in the soil. The silica could have come from the interaction of soil with acid vapors produced by volcanic activity in the presence of water or from water in a hot spring environment.[29]

The white material in the foreground is the silica rich soil that may be from hot springs.

A study of old data from the Miniature Thermal Emission Spectrometer, or Mini-TES and confirmed the presence of large amounts of carbonate-rich rocks, which means that regions of the planet may have once harbored water. As the Martian atmosphere contains mostly carbon dioxide, one would expect it to be changed into carbonates if water was available. Earth’s large limestone layers were made in this manner. The carbonates of Mars were discovered in an outcrop of rocks called "Comanche."[30] [31]

In Columbia Hills some very olivine-rich rocks were found. Later analysis suggested that these were formed from pyroclastic density currents in explosive volcanic eruptions. When this happens welded ignimbrite deposits result. The term ignimbrite is the rock formed in pyroclastic flows. Such flows are very hot and full of various sized particles. “Tuff” is another word for ignimbrite. Small pieces of rock from eruptions can weld themselves into ignimbrite when they are pushed together with more material settling on top. If this conclusion is correct then it may mean that there was much explosive eruptions in the past in many parts of Mars. Olivine-rich rocks are common on Mars.[32]

Discoveries from Curiosity

Cameras on Curiosity
Top of Mars Rover Curiosity's Remote Sensing Mast It holds two science instruments for studying the rover's surroundings and two stereo navigation cameras for use in driving the rover and planning rover explorations.


Conglomerate rock called “Hottah" after Hottah Lake in Canada's Northwest Territories. Conglomerate is composed of rounded pebbles that had to be formed in running water.

Just days into its mission, Curiosity discovered strong evidence of an ancient streambed where water once flowed knee-deep. As the mission progressed, more and more signs of water accumulated. Some of the signs of past water were the physical appearance of rocks. [33] [34] [35] [36] Many were rounded which means that they must have traveled in moving water which knocked off their original rough edges.[37] [38] [39]

Fine-grained rocks such as mudstone suggested deep water was present in the past.[40] [41] [42] Clear proof of deltas was found. Deltas are formed when water carrying sediment enters a quiet body of water. As the water laden fluid hits the water it slows down and drops its sediment load, thereby causing a buildup of land.[43] [44] [45] [46] Gale Crater contains a number of fans and deltas that provide information about lake levels in the past. These formations are: Pancake Delta, Western Delta, Farah Vallis delta and the Peace Vallis Fan.[47]

In January, 2017, JPL scientists announced the discovery of mud cracks in Gale Crater. Such mud cracks form with the aid of water.[48] [49] [50]

It was even determined that Gale Crater has liquid water at times according to measurements made by Curiosity. Since the humidity goes to 100% at night, salts, similar to calcium perchlorate, will absorb water from the air and make brine in the soil. Liquid water results even though the temperature is very low because salts lower the freezing point of water. We use this idea to melt snow/ice by spreading salt on roads. The liquid brine produced in the night at Gale Crater evaporates after sunrise. [51] [52] The amount of water was not enough to support life; however, it could allow salts to move around in the soil.[53] [54]

Data from the rover’s Dynamic Albedo of Neutrons (DAN) suggested subsurface water, amounting to as much as 4% water content, down to a depth of 2 feet (60cm), between the Bradbury Landing site to the Yellowknife Bay area in the Glenelg terrain.[55] On top of the physical evidence for water was data gathered by the sophisticated instruments on Curiosity. Many of the minerals identified were hydrated which required water. Some of these hydrated minerals are actinolite, montmorillonite, saponite, jarosite, halloysite, szomolnokite and magnesite. In some places 40 vol% of the minerals were hydrous minerals. [56]

Rock layers in the Murray Buttes area in lower Mount Sharp 


                                            Rock layers in the Murray Buttes area in lower Mount Sharp


Of great significance was the presence of clay which not only requires long periods of water, but the water had to be of neutral pH. A neutral pH is much more conducive to life. Great amounts of past water had been suggested by most scientists based upon decades of data from both orbiting satellites and lander/rovers. Mariner 9, Viking 1, Viking 2, Mars Odyssey, Mars Global Surveyor, Mars Express, and Mars Reconnaissance Orbiter all have imaged features resembling river valleys.[57] [58] [59] [60] Many researchers believe there have been lakes on Mars. [61] [62] [63] Some have developed a argument for an ocean covering a full third of the planet.[64] [65] [66] [67] [68] [69] [70] [71]

The Mars rovers Spirit and Opportunity have found evidence for a watery past. And, the vast and varied amounts of data from Curiosity have sealed the case for a wet, early Mars. It is now accepted that a large, long-lived lake existed in Gale Crater.

The presence of water is a prerequisite for life. Hence, the case for life on Mars at present or at least in the past has been greatly strengthened by Curiosity’s explorations, experiments, and measurements. More details about the many studies and observations that support a lake in Gale Crater can be found in the Marspedia article on Curiosity and the Wikipedia article on Aeolis quadrangle[[1]].


This evenly layered rock photographed by the Mast Camera (Mastcam) on NASA's Curiosity Mars Rover shows a pattern typical of a lake-floor sedimentary deposit not far from where flowing water entered a lake.


Rock layers in the Murray Buttes area in lower Mount Sharp


Curiosity's laser-firing Chemistry and Camera (ChemCam) here at Garden City found calcium sulfate in some veins and magnesium sulfate in others. Some veins contained fluorine or varying amounts of iron.


Veins Veins form when fluids move through cracks in the rock. They are exposed here because erosion has removed the softer rock that the veins were in.

Ma'adim Vallis

A large, ancient river valley, called Ma'adim Vallis, enters at the south rim of Gusev Crater, so Gusev Crater was believed to be an ancient lake bed. However, it seems that a volcanic flow covered up the lakebed sediments. Apollinaris Patera, a large volcano, lies directly north of Gusev Crater.[72] Recent studies lead scientists to believe that the water that formed Ma'adim Vallis originated in a complex of lakes.[73] [74] [75] The largest lake is located at the source of the Ma'adim Vallis outflow channel and extends into Eridania quadrangle and the Phaethontis quadrangle.[76] When this lake spilled over the low point in its boundary, a torrential flood would have moved north, carving the sinuous Ma'adim Vallis. At the north end of Ma'adim Vallis, the flood waters would have run into Gusev Crater.[77]

There is abundant evidence that water once flowed in river valleys 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. [78] [79] [80] [81]

Vallis (plural valles) is the Latin word for "valley". It is used in planetary geology for the naming of landform that look like old river valleys. The Viking Orbiters caused a revolution in our ideas about water on Mars; huge river valleys were found in many areas. Spacecraft cameras showed that floods of water broke through dams, carved deep valleys, eroded grooves into bedrock, and traveled thousands of kilometers.[82] [83] [84]

  • Section of Ma'adim Vallis as seen by HiRISE A more recent flow of water may have formed the smaller, deeper channel to the right.

Yardangs

Yardangs are common on Mars.[85] They are generally visible as a series of parallel linear ridges. Their parallel nature is thought to be caused by the direction of the prevailing wind.[86] Yardangs are common in the Medusae Fossae Formation on Mars.

Aeolis Mensae Yardangs, as seen by HiRISE. Scale bar is 500 meters long. An inverted stream channel is also visible

  • Medusae Fossae Formation southeast of Apollinaris Patera

  • Small yardangs


Gale Crater

View from the "Kimberley" formation on Mars taken by NASA's Curiosity rover. 

                                          View from the "Kimberley" formation on Mars taken by NASA's Curiosity rover.


Layers in Gale Crater on the Western flank of Mt. Sharp 

                                   Layers in Gale Crater on the Western flank of Mt. Sharp, as seen by HiRISE


Gale Crater, in the northwestern part of the Aeolis quadrangle, is of special interest to geologists because it contains a large mound of layered sedimentary rocks. At nearly 18,000 feet (3.4 miles, 5.5 kilometers) above the floor of Gale Crater, it is higher than any mountain in the continental United States.[87] This mound was first called Aeolis Mons, but is now named Mount Sharp in honor of Robert P. Sharp (1911–2004), a planetary scientist. The mound extends higher than the rim of the crater, so perhaps the layering covered an area much larger than the crater.[88] An alternative to this idea was published in 2019. Using various gravity measurements, the team concluded, "Mount Sharp formed largely in its current form as a free-standing mound within Gale."[89] [90] [91] [92]

These layers are a complex record of the past. The rock layers probably took millions of years to be laid down within the crater, then more time to be eroded to make them visible.[93] The 5 km high mound is probably the thickest single succession of sedimentary rocks on Mars.[94] The lower formation may date from near the Noachian age, while the upper layer, separated by an erosional unconformity, may be as young as the Amazonian period.[95] The lower formation may have formed the same time as parts of Sinus Meridiani and Mawrth Vallis. The mound that lies in the center of Gale Crater was created by winds. Because the winds eroded the mound on one side more than another, the mound is skewed to one side, rather than being symmetrical.[96] [97] The upper layer may be similar to layers in Arabia Terra. Sulfates and Iron oxides have been detected in the lower formation and anhydrous phases in the upper layer.[98] There is evidence that the first phase of erosion was followed by more cratering and more rock formation.[99] Also of interest in Gale Crater is Peace Vallis, officially named by the IAU on September 26, 2012,[100] which 'flows' down out of the Gale Crater hills to the Aeolis Palus below, and which seems to have been carved by flowing water.[101] [102]

  • Gale Crater with Aeolis Mons rising from the center. The noted Curiosity landing area is near Peace Vallis in Aeolis Palus. Curiosity landed in the northern part of the crater.

  • Peace Vallis and alluvial fan near the Curiosity rover landing ellipse and site (noted by +).

Aeolis Mons may have formed from the erosion of sediment layers that once filled Gale Crater.
Aeolis Mons as viewed from the Curiosity rover (August 9, 2012).
Layers at the base of Aeolis Mons - dark rock in inset is same size as the Curiosity rover.


View from Mastcam on Curiosity showing sloping buttes and layered outcrops on lower Mount Sharp 


                      View from Mastcam on Curiosity showing sloping buttes and layered outcrops on lower Mount Sharp

Inverted Relief

Meandering Ridges that are probably inverted stream channels. Image taken with HiRISE.


Some places on Mars show inverted relief. In these locations, a stream bed may be a raised feature, instead of a valley. The inverted former stream channels may be caused by the deposition of large rocks or due to cementation. In either case erosion would erode the surrounding land but leave the old channel as a raised ridge because the ridge will be more resistant to erosion. Images here, taken with HiRISE, show sinuous ridges that may be old channels that have become inverted.[103] [104]

Stream channels in inverted relief and yardangs, as seen by HiRISE.
Sinuous Ridges within a branching fan in lower member of Medusae Fossae Formation

Fretted terrain

Parts of the Aeolis quadrangle contain fretted terrain which is characterized by cliffs, mesas, buttes, and straight-walled canyons. It contains scarps or cliffs that are 1 to 2 km in height. Valleys often have wide, flat floors.[105] [106]

Fretted terrain, as seen by CTX

Layered terrain as seen by HiRISE

Layered mesas, as seen by HiRISE under HiWish program Dark slope streaks are also visible.


Layered mesas, as seen by HiRISE under HiWish program Dark slope streaks are also visible.


Close view of layered small mesa with dark slope streak, as seen by HiRISE under HiWish program Box shows the size of a football field.


Close view of layered small mesa with dark slope streak, as seen by HiRISE under HiWish program Box shows the size of a football field.


Researchers, writing in Icarus, have described layered units in the Aeolis quadrangle. They concluded that a deposit that contains yardangs was formed after several other deposits. The yardangs contain a layered deposit called "rhythmite" which was thought to be formed with regular changes in the climate. Because the layers appear harden, a damp or wet environment probably existed at the time. The authors correlate these layered deposits to the upper layers of Gale crater’s mound (Mt. Sharp).[107] Many places on Mars show rocks arranged in layers. Sometimes the layers are of different colors. Light-toned rocks on Mars have been associated with hydrated minerals like sulfates. The Mars Rover Opportunity examined such layers close-up with several instruments. Some layers are probably made up of fine particles because they seem to break up into find dust. Other layers break up into large boulders so they are probably much harder. Basalt, a volcanic rock, is thought to exist the layers that form boulders. Basalt has been identified on Mars in many places.

Instruments on orbiting spacecraft have detected clay (also called phyllosilicate) in some layers. Recent research with an orbiting near-infrared spectrometer, which reveals the types of minerals present based on the wavelengths of light they absorb, found evidence of layers of both clay and sulfates in Columbus crater.[108] This is exactly what would appear if a large lake had slowly evaporated.[109] Moreover, because some layers contained gypsum, a sulfate which forms in relatively fresh water, life could have formed in the crater.[110] Scientists were excited about finding hydrated minerals such as sulfates and clays on Mars because they are usually formed in the presence of water.[111] Places that contain clays and/or other hydrated minerals would be good places to look for evidence of life.[112]

Rock can form layers in a variety of ways. Volcanoes, wind, or water can produce layers.[113] Layers can be hardened by the action of groundwater. Martian ground water probably moved hundreds of kilometers, and in the process it dissolved many minerals from the rock it passed through. When ground water surfaces in low areas containing sediments, water evaporates into the thin atmosphere and leaves behind minerals as deposits and/or cementing agents. Consequently, layers of dust could not later easily erode away since they were cemented together. On Earth, mineral-rich waters often evaporate forming large deposits of various types of salts and other minerals. Sometimes water flows through Earth's aquifers, and then evaporates at the surface just as is hypothesed for Mars. One location this occurs on Earth is the Great Artesian Basin of Australia.[114] On Earth the hardness of many sedimentary rocks, like sandstone, is largely due to the cement that was put in place as water passed through. Silica cement is very hard, while calcite is not as hard.

Layers
Layers and a field of small mounds Medusae Fossae Formation Location is East of Gale Crater in the Aeolis quadrangle.
Layered structure
Close view of mound with layers


Close view of cap rock breaking up into boulders, as seen by HiRISE underHiWish program


Very close view of individual blocks breaking off layer in a butte Blocks have angular shapes. Box shows size of football field.


Close view of blocks from a mesa Arrow shows a cube-shaped block that is the size of a house.

Linear ridge networks

Linear ridge networks are found in various places on Mars in and around craters.[115] Ridges often appear as mostly straight segments. They are hundreds of meters long, tens of meters high, and several meters wide. One of several theories for their formation is that impacts created fractures in the surface, these fractures later acted as channels for fluids. Fluids hardened into rock. With the passage of time, surrounding material was eroded away, thereby leaving hard ridges behind. Since the ridges occur in locations with clay, these formations could serve as a marker for clay which requires water for its formation.[116] [117] [118]

Ridges


Ridges, as seen by HiRISE under HiWish program Close view of ridges, as seen by HiRISE under HiWish program

Other features in Aeolis quadrangle

Channel, as seen by HiRISE under HiWish program


Apollinaris Patera, a volcano that lies directly north of Gusev Crate

See also

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. ↑ Blunck, J. 1982. Mars and its Satellites. Exposition Press. Smithtown, N.Y.
  3. ↑ Curiosity landed in the northern part of the crater; in some pictures it is hard to see where it landed. |author=NASA Staff |title=NASA Lands Car-Size Rover Beside Martian Mountain |url=http://www.jpl.nasa.gov/news/news.cfm?release=2012-230 |date=6 August 2012 |publisher=NASA/JPL
  4. ↑ http://www.msnbc.msn.com/id/6785665%7Ctitle=Spirit rover follows up on scientific surprises|date=4 January 2005|
  5. ↑ U.S. department of the Interior U.S. Geological Survey, Topographic Map of the Eastern Region of Mars M 15M 0/270 2AT, 1991
  6. ↑ http://www.nasa.gov/mission_pages/msl/multimedia/pia15292-Fig2.html%7Cdate=27 March 2012 |NASA
  7. ↑ Agle |first=D. C.|title='Mount Sharp' On Mars Links Geology's Past and Future|url=http://www.nasa.gov/mission_pages/msl/news/msl20120328.html%7Cdate=28 March 2012 |publisher=NASA
  8. ↑ =NASA's New Mars Rover Will Explore Towering 'http://www.space.com/15097-mars-mountain-sharp-curiosity-rover.html%7Cdate=29 March 2012 |publisher=Space.com
  9. ↑ USGS|title=Three New Names Approved for Features on Mars|url=https://astrogeology.usgs.gov/HotTopics/index.php?/archives/447-Three-New-Names-Approved-for-Features-on-Mars.html%7Cdate=16 May 2012|publisher=USGS|
  10. ↑ Ori, G., I. Di Pietro, F. Salese. 2015. A WATERLOGGED MARTIAN ENVIRONMENT: CHANNEL PATTERNS AND SEDIMENTARY ENVIRONMENTS OF THE ZEPHYRIA ALLUVIAL PLAIN. 46th Lunar and Planetary Science Conference (2015) 2527.pdf
  11. ↑ Christensen P (August 2004). "Initial Results from the Mini-TES Experiment in Gusev Crater from the Spirit Rover". Science. 305 (5685): 837–842.
  12. ↑ McSween, etal. 2004. "Basaltic Rocks Analyzed by the Spirit Rover in Gusev Crater". Science : 305. 842–845
  13. ↑ Arvidson R. E.; et al. (2004). "Localization and Physical Properties Experiments Conducted by Spirit at Gusev Crater". Science. 305 (5685): 821–824.
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  18. ↑ Ming,D., et al. 2006 Geochemical and mineralogical indicators for aqueous processes in the Columbia Hills of Gusev crater, Mars. J. Geophys. Res.111
  19. ↑ McSween, etal. 2004. "Basaltic Rocks Analyzed by the Spirit Rover in Gusev Crater". Science : 305. 842–845
  20. ↑ Arvidson R. E.; et al. (2004). "Localization and Physical Properties Experiments Conducted by Spirit at Gusev Crater". Science. 305 (5685): 821–824.
  21. ↑ McSween, etal. 2004. "Basaltic Rocks Analyzed by the Spirit Rover in Gusev Crater". Science : 305. 842–845
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Further reading

  • Grotzinger, J. and R. Milliken (eds.). 2012. Sedimentary Geology of Mars. SEPM.
  • Lakdawalla E | year = 2011 | title = Target: Gale Curiosity Will Soon Have a New Home | url = | journal = The Planetary Report | volume = 31 | issue = 4| pages = 15–21
  • Lakdawalla, E. 2018. The Design and Engineering of Curiosity: How the Mars Rover Performs its job. Springer Praxis Publishing. Chichester, UK

External links

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