Gusev (Martian crater)

Gusev

The Martian crater Gusev, with Ma'adim Vallis snaking into it
Planet Mars
Region Aeolis quadrangle
Coordinates 14°30′S 175°24′E / 14.5°S 175.4°E / -14.5; 175.4Coordinates: 14°30′S 175°24′E / 14.5°S 175.4°E / -14.5; 175.4[1]
Diameter 166 km
Eponym Matvey Gusev

Gusev is a crater on the planet Mars and is located at 14°30′S 175°24′E / 14.5°S 175.4°E / -14.5; 175.4. The crater is about 166 kilometers in diameter and formed approximately three to four billion years ago. It was named after Russian astronomer Matvei Gusev (1826–1866) in 1976.

A channel system named Ma'adim Vallis drains into it that probably carried liquid water, or water and ice, at some point in Mars' past. The crater appears to be an old crater lake bed, filled with sediments up to 3000 feet thick.[2] Some exposed outcrops appear to show faint layering, and some researchers also believe that landforms visible in images of the mouth of Ma'adim Vallis where it enters Gusev resemble landforms seen in some terrestrial river deltas. Deltas of this nature can take tens or hundreds of thousands of years to form on Earth, suggesting that the water flows may have lasted for long periods. Orbital images indicate that there may once have been a very large lake near the source of Ma'adim Vallis that could have provided the source of this water. It is not known whether this flow was slow and continuous, punctuated by sporadic large outbursts, or some combination of these patterns.

Panoramic photo taken by Spirit Rover on January 1, 2006 from the crater Gusev, looking up a slope and across rippled sand deposits in a dark field dubbed "El Dorado".

More recently, satellite images showed the trails of dust devils on Gusev's floor. The Spirit rover later photographed dust devils from the ground, and likely owes much of its longevity to dust devils cleaning its solar panels.

On January 3, 2004, Gusev was the landing site of the first of NASA's two Mars Exploration Rovers, named Spirit. It is hoped that the numerous smaller and more recent craters in this region will have exposed sedimentary material from early eras, although at first the region proved disappointing in its lack of available bedrock for study on the flat lava plains of the crater, Spirit's landing site. It eventually arrived at the Columbia Hills, however, and rocks examined in that region show that the Columbia Hills did have small amounts of briny (salty) water interacting with them in ancient times,[3] though nowhere near as much as Meridiani Planum, the landing area for Spirit's twin, Opportunity. However, in 2009, Spirit became stuck in the soil of the region, and in 2010 went offline after a harsh Martian winter. It is also considered a potential landing site for the Mars 2020 rover.

Spirit Rover's rocks and minerals discoveries on Mars

The rocks on the plains of Gusev are a type of basalt. They contain the minerals olivine, pyroxene, plagioclase, and magnetite, and they look like volcanic basalt as they are fine-grained with irregular holes (geologists would say they have vesicles and vugs).[4][5] Much of the soil on the plains came from the breakdown of the local rocks. Fairly high levels of nickel were found in some soils; probably from meteorites.[6] Analysis shows 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. All the rocks contain a fine coating of dust and one or more harder rinds of material. One type can be brushed off, while another needed to be ground off by the Rock Abrasion Tool (RAT).[7]

There are a variety of rocks in the Columbia Hills (Mars), some of which have been altered by water, but not by very much water.

The dust in Gusev Crater is the same as dust all around the planet. All the dust was found to be magnetic. Moreover, Spirit found the magnetism was caused by the mineral magnetite, especially magnetite that contained the element titanium. One magnet was able to completely divert all dust hence all Martian dust is thought to be magnetic.[8] The spectra of the dust was similar to spectra of bright, low thermal inertia regions like Tharsis and Arabia that have been detected by orbiting satellites. A thin layer of dust, maybe less than one millimeter thick covers all surfaces. Something in it contains a small amount of chemically bound water.[9][10]

Plains

Observations of rocks on the plains show they contain the minerals pyroxene, olivine, plagioclase, and magnetite. These rocks can be classified in different ways. The amounts and types of minerals make the rocks primitive basalts—also called picritic basalts. The rocks are similar to ancient terrestrial rocks called basaltic komatiites. Rocks of the plains also resemble the basaltic shergottites, meteorites which came from Mars. One classification system compares the amount of alkali elements to the amount of silica on a graph; in this system, Gusev plains rocks lie near the junction of basalt, picrobasalt, and tephite. The Irvine-Barager classification calls them basalts.[4] Plain’s rocks have been very slightly altered, probably by thin films of water because they are softer and contain veins of light colored material that may be bromine compounds, as well as coatings or rinds. It is thought that small amounts of water may have gotten into cracks inducing mineralization processes.[5][4] Coatings on the rocks may have occurred when rocks 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.

Columbia Hills

Scientists found a variety of rock types in the Columbia Hills, and they placed them into six different categories. The six are: Clovis, Wishbone, Peace, Watchtower, Backstay, and Independence. They are named after a prominent rock in each group. Their chemical compositions, as measured by APXS, are significantly different from each other.[11] Most importantly, all of the rocks in Columbia Hills show various degrees of alteration due to aqueous fluids.[12] 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.[13][14] The olivine abundance varies inversely with the amount of sulfates. This is exactly what is expected because water destroys olivine but helps to produce sulfates.

The Clovis group is especially interesting because the Mössbauer spectrometer(MB) detected goethite in it.[15] 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,[13] although the rocks probably once contained much olivine.[16] Olivine is a marker for the lack of water because it easily decomposes in the presence of water. Sulfate was found, and it needs water to form. Wishstone contained a great deal of plagioclase, some olivine, and anhydrate (a sulfate). Peace rocks showed sulfur and strong evidence for bound water, so hydrated sulfates are suspected. Watchtower class rocks lack olivine consequently they may have been altered by water. The Independence class showed some signs of clay (perhaps montmorillonite a member of the smectite group). Clays require fairly long term exposure to water to form. One type of soil, called Paso Robles, from the Columbia Hills, may be an evaporate deposit because it contains large amounts of sulfur, phosphorus, calcium, and iron.[17] Also, MB found that much of the iron in Paso Robles soil was of the oxidized, Fe+++ form, which would happen if water had been present.[9]

Towards the middle of the six-year mission (a mission that was supposed to last only 90 days), large amounts of pure silica were found 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.[18]

After Spirit stopped working scientists studied 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. The carbonates were discovered in an outcrop of rocks called "Comanche."[19][20]

In summary, Spirit found evidence of slight weathering on the plains of Gusev, but no evidence that a lake was there. However, in the Columbia Hills there was clear evidence for a moderate amount of aqueous weathering. The evidence included sulfates and the minerals goethite and carbonates which only form in the presence of water. It is believed that Gusev crater may have held a lake long ago, but it has since been covered by igneous materials. All the dust contains a magnetic component which was identified as magnetite with some titanium. Furthermore, the thin coating of dust that covers everything on Mars is the same in all parts of Mars.

Features within Gusev

Hills

Craters

Other

Landing site

Gusev crater was one of three candidates for a landing site for Mars 2020 as of 2017.[21] Specifically, Colombia Hills is being targeted, which was previously explored by Spirit rover.[22] Previously Gusev crater was selected and soft-landed on by the Spirit rover, which after several years of activity stopped communicating in 2010

Other landing site candidates for the Mars 2020 rover, by 2017, were Northeast Syrtis (Syrtis Major)and Jezero crater.[23]

Interactive Mars map

Acidalia Planitia Acidalia Planitia Alba Mons Amazonis Planitia Aonia Terra Arabia Terra Arcadia Planitia Arcadia Planitia Argyre Planitia Elysium Mons Elysium Planitia Hellas Planitia Hesperia Planum Isidis Planitia Lucas Planum Lyot Crater Noachis Terra Olympus Mons Promethei Terra Rudaux Crater Solis Planum Tempe Terra Terra Cimmeria Terra Sabaea Terra Sirenum Tharsis Montes Utopia Planitia Valles Marineris Vastitas Borealis Vastitas BorealisMap of Mars
Interactive imagemap of the global topography of Mars, overlain with locations of Mars landers and rovers (Red label = Rover; Blue label = Lander; bold red/blue = currently active). Hover your mouse to see the names of over 25 prominent geographic features, and click to link to them. Coloring of the base map indicates relative elevations, based on data from the Mars Orbiter Laser Altimeter on NASA's Mars Global Surveyor. Reds and pinks are higher elevation (+3 km to +8 km); yellow is 0 km; greens and blues are lower elevation (down to −8 km). Whites (>+12 km) and browns (>+8 km) are the highest elevations. Axes are latitude and longitude; Poles are not shown.
(See also: Mars map & Mars Memorials & Mars Memorials map) (view • discuss)
← Beagle 2 (2003)
Curiosity (2012) →
Deep Space 2 (1999) →
Mars 2 (1971) →
← Mars 3 (1971)
Mars 6 (1973) →
Polar Lander (1999) ↓
↑ Opportunity (2004)
← Phoenix (2008)
Schiaparelli EDM (2016) →
← Sojourner (1997)
Spirit (2004) ↑
Viking 1 (1976) →
Viking 2 (1976) →

See also

References

  1. ↑ "Gusev". Gazetteer of Planetary Nomenclature. USGS Astrogeology Research Program.
  2. ↑ Burnham, Robert (9 April 2014). "Gusev Crater once held a lake after all, says ASU Mars scientist". Arizona State University. Retrieved 2014-04-10.
  3. ↑ "Aqueous processes at Gusev crater inferred from physical properties of rocks and soils along the Spirit traverse". AGU.
  4. 1 2 3 McSween; et al. (2004). "Basaltic Rocks Analyzed by the Spirit Rover in Gusev Crater". Science. 305: 842–845. Bibcode:2004Sci...305..842M. PMID 15297668. doi:10.1126/science.3050842.
  5. 1 2 Arvidson, R. E.; et al. (2004). "Localization and Physical Properties Experiments Conducted by Spirit at Gusev Crater". Science. 305: 821–824. Bibcode:2004Sci...305..821A. PMID 15297662. doi:10.1126/science.1099922.
  6. ↑ Gelbert, R.; et al. (2006). "The Alpha Particle X-ray Spectrometer (APXS): results from Gusev crater and calibration report". Journal of Geophysical Research: Planets. 111. Bibcode:2006JGRE..111.2S05G. doi:10.1029/2005je002555.
  7. ↑ Christensen, P. (August 2004). "Initial Results from the Mini-TES Experiment in Gusev Crater from the Spirit Rover". Science. 305 (5685): 837–842. Bibcode:2004Sci...305..837C. PMID 15297667. doi:10.1126/science.1100564.
  8. ↑ Bertelsen, P.; et al. (2004). "Magnetic Properties on the Mars Exploration Rover Spirit at Gusev Crater". Science. 305 (5685): 827–829. Bibcode:2004Sci...305..827B. PMID 15297664. doi:10.1126/science.1100112.
  9. 1 2 Bell, J., ed. (2008). The Martian Surface. Cambridge University Press. ISBN 978-0-521-86698-9.
  10. ↑ Gelbert, R.; et al. "Chemistry of Rocks and Soils in Gusev Crater from the Alpha Particle X-ray Spectrometer". Science. 305: 829–32. Bibcode:2004Sci...305..829G. PMID 15297665. doi:10.1126/science.1099913.
  11. ↑ Squyres, S.; et al. (2006). "Rocks of the Columbia Hills". Journal of Geophysical Research: Planets. 111. Bibcode:2006JGRE..111.2S11S. doi:10.1029/2005je002562.
  12. ↑ Ming, D.; et al. (2006). "Geochemical and mineralogical indicators for aqueous processes in the Columbia Hills of Gusev crater". Journal of Geophysical Research: Planets. 111. Bibcode:2006JGRE..111.2S12M. doi:10.1029/2005je002560.
  13. 1 2 Schroder, C.; et al. (2005). European Geosciences Union, General Assembly, Geophysical Research abstr. 7: 10254. Missing or empty |title= (help)
  14. ↑ Christensen, P.R. (23–27 May 2005). "Mineral Composition and Abundance of the Rocks and Soils at Gusev and Meridiani from the Mars Exploration Rover Mini-TES Instruments". AGU Joint Assembly.
  15. ↑ Klingelhofer, G.; et al. (2005). Lunar Planet. Sci. XXXVI: abstr. 2349. Missing or empty |title= (help)
  16. ↑ Morris, S.; et al. "Mossbauer mineralogy of rock, soil, and dust at Gusev crater, Mars: Spirit’s journal through weakly altered olivine basalt on the plains and pervasively altered basalt in the Columbia Hills". Journal of Geophysical Research: Planets. 111. Bibcode:2006JGRE..111.2S13M. doi:10.1029/2005je002584.
  17. ↑ Ming, D.; et al. (2006). "Geochemical and mineralogical indicators for aqueous processes in the Columbia Hills of Gusev crater, Mars". Journal of Geophysical Research: Planets. 111. Bibcode:2006JGRE..111.2S12M. doi:10.1029/2005je002560.
  18. ↑ "Mars Rover Spirit Unearths Surprise Evidence of Wetter Past". NASA. 2007-05-21.
  19. ↑ "Outcrop of long-sought rare rock on Mars found". Science Daily. doi:10.1126/science.1189667.
  20. ↑ Morris, Richard V.; Ruff, Steven W.; Gellert, Ralf; Ming, Douglas W.; Arvidson, Raymond E.; Clark, Benton C.; Golden, D. C.; Siebach, Kirsten; et al. (3 June 2010). "Identification of Carbonate-Rich Outcrops on Mars by the Spirit Rover". Science. 329 (5990): 421–4. Bibcode:2010Sci...329..421M. PMID 20522738. doi:10.1126/science.1189667.
  21. ↑ "Scientists Shortlist Three Landing Sites for Mars 2020". NASA/JPL. Retrieved 2017-02-15.
  22. ↑ "Scientists Shortlist Three Landing Sites for Mars 2020". NASA/JPL. Retrieved 2017-02-15.
  23. ↑ "Scientists Shortlist Three Landing Sites for Mars 2020". NASA/JPL. Retrieved 2017-02-15.
  24. ↑ Benford, Gregory (1999). The Martian Race. New York: Warner Aspect. ISBN 0-446-52633-9. LCCN 99-049124.
  25. ↑ Davies, Russell T; Ford, Phil (March 3, 2009). "The Waters of Mars" (PDF). BBC Books. p. 9. Archived from the original (PDF) on May 8, 2013. Retrieved June 2, 2014.
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