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{{short description|NASA Mars rover, active from 2004 to 2010}}
{{Short description|NASA Mars rover, active from 2004 to 2010}}
{{italic title}}
{{Italic title}}
{{Use mdy dates|date=November 2022}}
{{Use mdy dates|date=November 2022}}
{{Use American English|date=March 2018}}
{{Use American English|date=March 2018}}
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| launch_mass = Total: 1,063 kg<br>* rover: 185 kg<br>* lander: 348 kg<br>* backshell/parachute: 209 kg<br>* heat shield: 78 kg<br>* cruise stage: 193 kg<br>* propellant: 50 kg<ref>{{cite web|title=Mars Exploration Rovers|url=http://mars.jpl.nasa.gov/mer/mission/spacecraft.html |work=[[NASA]] |access-date=December 6, 2018}}</ref>
| launch_mass = Total: 1,063 kg<br>* rover: 185 kg<br>* lander: 348 kg<br>* backshell/parachute: 209 kg<br>* heat shield: 78 kg<br>* cruise stage: 193 kg<br>* propellant: 50 kg<ref>{{cite web|title=Mars Exploration Rovers|url=http://mars.jpl.nasa.gov/mer/mission/spacecraft.html |work=[[NASA]] |access-date=December 6, 2018}}</ref>
| power = 140 [[watt]]s
| power = 140 [[watt]]s
| launch_date = {{start-date|June 10, 2003, 17:58:47 UTC}}<ref name="Spirit">{{cite web|url=https://solarsystem.nasa.gov/missions/spirit/in-depth/ |title=Spirit |publisher=NASA's Solar System Exploration website |access-date=December 2, 2022}}</ref><br>{{start-date|June 10, 2003, 1:58:47 p.m. EDT}}<ref name="NASA-Spirit">{{cite web|last=Nelson |first=Jon |title=Mars Exploration Rover – Spirit|url=http://www.jpl.nasa.gov/missions/details.php?id=5917 |work=[[NASA]] |access-date=February 2, 2014}}</ref><ref name="LaunchDetails">{{cite web|url=http://marsprogram.jpl.nasa.gov/mer/mission/launch_e.html |title=Launch Event Details – When did the Rovers Launch?|access-date=April 25, 2009}}</ref>
| launch_date = {{start-date|June 10, 2003, 17:58:47 UTC}}<ref name="Spirit">{{cite web|url=https://solarsystem.nasa.gov/missions/spirit/in-depth/ |title=Spirit |publisher=NASA's Solar System Exploration website |access-date=December 2, 2022}}</ref><br>{{start-date|June 10, 2003, 1:58:47 p.m. EDT}}<ref name="NASA-Spirit">{{cite web |last=Nelson |first=Jon |title=Mars Exploration Rover – Spirit |url=http://www.jpl.nasa.gov/missions/details.php?id=5917 |work=[[NASA]] |access-date=February 2, 2014 |archive-date=January 28, 2018 |archive-url=https://web.archive.org/web/20180128115920/https://www.jpl.nasa.gov/missions/details.php?id=5917 |url-status=dead }}</ref><ref name="LaunchDetails">{{cite web|url=http://marsprogram.jpl.nasa.gov/mer/mission/launch_e.html |title=Launch Event Details – When did the Rovers Launch?|access-date=April 25, 2009}}</ref>
| launch_rocket = [[Delta II]] 7925-9.5<ref name="LaunchDetails"/><ref>{{cite web |url=http://trs-new.jpl.nasa.gov/dspace/bitstream/2014/12837/1/01-1164.pdf |title=Mars Exploration Rover project, NASA/JPL document NSS ISDC 2001 27/05/2001 |page=5 |access-date=April 28, 2009 |url-status=dead |archive-url=https://web.archive.org/web/20100527044955/http://trs-new.jpl.nasa.gov/dspace/bitstream/2014/12837/1/01-1164.pdf |archive-date=May 27, 2010 }}</ref>
| launch_rocket = [[Delta II]] 7925-9.5<ref name="LaunchDetails"/><ref>{{cite web |url=http://trs-new.jpl.nasa.gov/dspace/bitstream/2014/12837/1/01-1164.pdf |title=Mars Exploration Rover project, NASA/JPL document NSS ISDC 2001 27/05/2001 |page=5 |access-date=April 28, 2009 |url-status=dead |archive-url=https://web.archive.org/web/20100527044955/http://trs-new.jpl.nasa.gov/dspace/bitstream/2014/12837/1/01-1164.pdf |archive-date=May 27, 2010 }}</ref>
| launch_site = [[Cape Canaveral Air Force Station|Cape Canaveral]] [[Cape Canaveral Air Force Station Space Launch Complex 17|SLC-17A]]
| launch_site = [[Cape Canaveral Air Force Station|Cape Canaveral]] [[Cape Canaveral Air Force Station Space Launch Complex 17|SLC-17A]]
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}}
}}


'''''Spirit''''', also known as '''MER-A''' ('''Mars Exploration Rover – A''') or '''MER-2''', is a [[Mars rover|Mars robotic rover]], active from 2004 to 2010.<ref name="NASA-Spirit" /> ''Spirit'' was operational on Mars for {{age in sols|2004|01|04|2010|03|22}} [[Timekeeping on Mars#Sols|sols]] or 3.3 Martian years ({{age in days|2004|01|24|2010|03|22}} [[days]]; <SMALL>''{{age in years and days|4 January 2004|22 March 2010}}''</SMALL>). It was one of two [[rover (space exploration)|rovers]] of [[NASA]]'s [[Mars Exploration Rover]] Mission managed by the [[Jet Propulsion Laboratory]] (JPL). Spirit landed successfully within the impact crater [[Gusev (Martian crater)|Gusev]] on [[Mars]] at 04:35 [[Ground UTC]] on January 4, 2004, three weeks before its twin, ''[[Opportunity (rover)|Opportunity]]'' (MER-B), which landed on the other side of the planet. Its name was chosen through a [[Sofi Collis|NASA-sponsored student essay competition]]. The rover got stuck in a "sand trap" in late 2009 at an angle that hampered recharging of its batteries; its last communication with Earth was on March 22, 2010.
'''''Spirit''''', also known as '''MER-A''' ('''Mars Exploration Rover – A''') or '''MER-2''', is a [[Mars rover|Mars robotic rover]], active from 2004 to 2010.<ref name="NASA-Spirit" /> ''Spirit'' was operational on Mars for {{age in sols|2004|01|04|2010|03|22}} [[Timekeeping on Mars#Sols|sols]] or 3.3 Martian years ({{age in days|2004|01|04|2010|03|22}} [[days]]; <SMALL>''{{age in years and days|4 January 2004|22 March 2010}}''</SMALL>). It was one of two [[rover (space exploration)|rovers]] of [[NASA]]'s [[Mars Exploration Rover]] Mission managed by the [[Jet Propulsion Laboratory]] (JPL). Spirit landed successfully within the impact crater [[Gusev (Martian crater)|Gusev]] on [[Mars]] at 04:35 [[Ground UTC]] on January 4, 2004, three weeks before its twin, ''[[Opportunity (rover)|Opportunity]]'' (MER-B), which landed on the other side of the planet. Its name was chosen through a [[Sofi Collis|NASA-sponsored student essay competition]]. The rover got stuck in a "sand trap" in late 2009 at an angle that hampered recharging of its batteries; its last communication with Earth was on March 22, 2010.


The rover completed its planned 90-[[Martian day|sol]] mission (slightly less than 92.5 Earth days). Aided by [[cleaning event]]s that resulted in more energy from its solar panels, ''Spirit'' went on to function effectively over twenty times longer than NASA planners expected. ''Spirit'' also logged {{convert|7.73|km|mi|1|abbr=on}} of driving instead of the planned {{convert|600|m|mi|1|abbr=on}},<ref>{{cite press release|url=http://marsrovers.jpl.nasa.gov/newsroom/pressreleases/20110525a.html|title=NASA Spirit Rover Completes Mission on Mars|publisher=[[Jet Propulsion Laboratory]]|date=May 25, 2011|access-date=May 26, 2011|archive-date=June 11, 2011|archive-url=https://web.archive.org/web/20110611060618/http://marsrovers.jpl.nasa.gov/newsroom/pressreleases/20110525a.html|url-status=dead}}</ref> allowing more extensive geological analysis of Martian rocks and planetary surface features. Initial scientific results from the first phase of the mission (the 90-sol prime mission) were published in a special issue of the journal [[Science (journal)|''Science'']].<ref>{{Cite journal |title=Special Issue: Spirit at Gusev Crater |journal=Science |volume=305 |issue=5685 |pages=737–900 |date=August 6, 2004 |url=https://www.science.org/toc/science/305/5685}}</ref>
The rover completed its planned 90-[[Martian day|sol]] mission (slightly less than 92.5 Earth days). Aided by [[cleaning event]]s that resulted in more energy from its solar panels, ''Spirit'' went on to function effectively over twenty times longer than NASA planners expected. ''Spirit'' also logged {{convert|7.73|km|mi|1|abbr=on}} of driving instead of the planned {{convert|600|m|mi|1|abbr=on}},<ref>{{cite press release|url=http://marsrovers.jpl.nasa.gov/newsroom/pressreleases/20110525a.html|title=NASA Spirit Rover Completes Mission on Mars|publisher=[[Jet Propulsion Laboratory]]|date=May 25, 2011|access-date=May 26, 2011|archive-date=June 11, 2011|archive-url=https://web.archive.org/web/20110611060618/http://marsrovers.jpl.nasa.gov/newsroom/pressreleases/20110525a.html|url-status=dead}}</ref> allowing more extensive geological analysis of Martian rocks and planetary surface features. Initial scientific results from the first phase of the mission (the 90-sol prime mission) were published in a special issue of the journal [[Science (journal)|''Science'']].<ref>{{Cite journal |title=Special Issue: Spirit at Gusev Crater |journal=Science |volume=305 |issue=5685 |pages=737–900 |date=August 6, 2004 |url=https://www.science.org/toc/science/305/5685}}</ref>
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though it continued to perform scientific research from its current location.<ref>{{cite press release|url=http://www.nasa.gov/mission_pages/mer/news/mer20100126.html|title=Now a Stationary Research Platform, NASA's Mars Rover Spirit Starts a New Chapter in Red Planet Scientific Studies|work=[[NASA]]|date=January 26, 2010|access-date=January 26, 2010|author1=Brown, Dwayne|author2=Webster, Guy|quote=Washington – After six years of unprecedented exploration of the Red Planet, NASA's Mars Exploration Rover ''Spirit'' no longer will be a fully mobile robot. NASA has designated the once-roving scientific explorer a stationary science platform after efforts during the past several months to free it from a sand trap have been unsuccessful.}}</ref>
though it continued to perform scientific research from its current location.<ref>{{cite press release|url=http://www.nasa.gov/mission_pages/mer/news/mer20100126.html|title=Now a Stationary Research Platform, NASA's Mars Rover Spirit Starts a New Chapter in Red Planet Scientific Studies|work=[[NASA]]|date=January 26, 2010|access-date=January 26, 2010|author1=Brown, Dwayne|author2=Webster, Guy|quote=Washington – After six years of unprecedented exploration of the Red Planet, NASA's Mars Exploration Rover ''Spirit'' no longer will be a fully mobile robot. NASA has designated the once-roving scientific explorer a stationary science platform after efforts during the past several months to free it from a sand trap have been unsuccessful.}}</ref>


The rover continued in a stationary science platform role until communication with ''Spirit'' stopped on March 22, 2010 (sol {{age in sols|2004|01|04|2010|03|22}}).<ref name="spirit-update">[http://marsrovers.jpl.nasa.gov/mission/status_spiritAll.html#sol2397 September 30 – October 5, 2010 Spirit Remains Silent at Troy] NASA. October 5, 2010.</ref><ref>A.J.S. Rayl [http://www.planetary.org/news/2010/1130_Mars_Exploration_Rovers_Update_Mission.html Mars Exploration Rovers Update] ''[[Planetary Society]]'' November 30, 2010</ref> JPL continued to attempt to regain contact until May 24, 2011, when NASA announced that efforts to communicate with the unresponsive rover had ended, calling the mission complete.<ref name="spirit contact conclusion2">{{cite web|last=Webster |first=Guy |title=NASA's Spirit Rover Completes Mission on Mars |url=http://www.nasa.gov/mission_pages/mer/news/mer20110525.html|date=May 25, 2011 |publisher=[[NASA]] |access-date=October 12, 2011 }}</ref><ref name="EOMannoucement">{{cite web|url=http://www.jpl.nasa.gov/news/news.php?feature=3013|title=NASA's Spirit Rover Completes Mission on Mars|website=NASA/JPL}}</ref><ref name="spirit contact conclusion1">{{cite web|title=NASA Concludes Attempts to Contact Mars Rover Spirit|url=http://www.jpl.nasa.gov/news/news.cfm?release=2011-156&cid=release_2011-156|publisher=NASA|access-date=May 25, 2011}}</ref><ref name="NASA_Abandon">{{cite news |last=Chang |first=Kenneth |title=NASA to Abandon Mars Spirit Rover |url=https://www.nytimes.com/2011/05/25/science/space/25rover.html |date=May 24, 2011|work=[[The New York Times]]}}</ref> A formal farewell took place at NASA headquarters shortly thereafter.
The rover continued in a stationary science platform role until communication with ''Spirit'' stopped on March 22, 2010 (sol {{age in sols|2004|01|04|2010|03|22}}).<ref name="spirit-update">[http://marsrovers.jpl.nasa.gov/mission/status_spiritAll.html#sol2397 September 30 – October 5, 2010 Spirit Remains Silent at Troy] NASA. October 5, 2010.</ref><ref>A.J.S. Rayl [http://www.planetary.org/news/2010/1130_Mars_Exploration_Rovers_Update_Mission.html Mars Exploration Rovers Update] {{Webarchive|url=https://web.archive.org/web/20120318214910/http://www.planetary.org/news/2010/1130_Mars_Exploration_Rovers_Update_Mission.html |date=March 18, 2012 }} ''[[Planetary Society]]'' November 30, 2010</ref> JPL continued to attempt to regain contact until May 24, 2011, when NASA announced that efforts to communicate with the unresponsive rover had ended, calling the mission complete.<ref name="spirit contact conclusion2">{{cite web |last=Webster |first=Guy |date=May 25, 2011 |title=NASA's Spirit Rover Completes Mission on Mars |url=http://www.nasa.gov/mission_pages/mer/news/mer20110525.html |archive-url=https://web.archive.org/web/20230207121910/https://www.nasa.gov/mission_pages/mer/news/mer20110525.html |archive-date=7 February 2023 |access-date=October 12, 2011 |publisher=[[NASA]]}}</ref><ref name="EOMannoucement">{{cite web|url=http://www.jpl.nasa.gov/news/news.php?feature=3013|title=NASA's Spirit Rover Completes Mission on Mars|website=NASA/JPL}}</ref><ref name="spirit contact conclusion1">{{cite web|title=NASA Concludes Attempts to Contact Mars Rover Spirit|url=http://www.jpl.nasa.gov/news/news.cfm?release=2011-156&cid=release_2011-156|publisher=NASA|access-date=May 25, 2011|archive-date=October 11, 2011|archive-url=https://web.archive.org/web/20111011190254/http://www.jpl.nasa.gov/news/news.cfm?release=2011-156&cid=release_2011-156|url-status=dead}}</ref><ref name="NASA_Abandon">{{cite news |last=Chang |first=Kenneth |title=NASA to Abandon Mars Spirit Rover |url=https://www.nytimes.com/2011/05/25/science/space/25rover.html |date=May 24, 2011|work=[[The New York Times]]}}</ref> A formal farewell took place at NASA headquarters shortly thereafter.

==Mission overview==
[[File:LandingSiteR1.jpg|thumb|left|''Spirit'' landing site, as imaged by [[Mars Reconnaissance Orbiter|MRO]] (December 4, 2006); click image to enlarge]]
[[File:MOLA spirit.jpg|thumb|right|An overall view of MER-A ''Spirit'' landing site (denoted with a star)]]
The primary surface mission for ''Spirit'' was planned to last at least 90 [[Timekeeping on Mars|sols]]. The mission received several extensions and lasted about 2,208 sols. On August 11, 2007, ''Spirit'' obtained the second longest operational duration on the surface of Mars for a lander or rover at 1282 Sols, one sol longer than the [[Viking 2]] lander. Viking 2 was powered by a nuclear cell whereas ''Spirit'' is powered by solar arrays. Until ''Opportunity'' overtook it on May 19, 2010, the Mars probe with longest operational period was [[Viking 1]] that lasted for 2245 Sols on the surface of Mars. On March 22, 2010, ''Spirit'' sent its last communication, thus falling just over a month short of surpassing Viking 1's operational record. An archive of weekly updates on the rover's status can be found at the ''Spirit'' Update Archive.<ref name="SpiritUpdateArchive" />

''Spirit's'' total odometry is {{convert|7730.50|m|mi|2|sp=us}}.<ref>{{cite web |url=http://marsrovers.nasa.gov/mission/status_spiritAll.html |title=Spirit Updates |access-date=May 14, 2012 |archive-url=https://web.archive.org/web/20140228232506/http://marsrovers.nasa.gov/mission/status_spiritAll.html |archive-date=February 28, 2014 |url-status=dead }}</ref>


==Objectives==
==Objectives==
[[File:Lancement Spirit fusee Delta IIs 10062003.jpg|thumb|upright=1.0|Delta II lifting off with MER-A on June 10, 2003]]
[[File:Lancement Spirit fusee Delta IIs 10062003.jpg|thumb|upright=1.0|Delta II lifting off with MER-A on June 10, 2003]]
The scientific objectives of the Mars Exploration Rover mission were to:<ref>{{cite web|url=http://marsrovers.nasa.gov/science/objectives.html|title=Mars Exploration Rover Mission: Science|website=marsrovers.nasa.gov|access-date=July 25, 2008|archive-url=https://web.archive.org/web/20110914072307/http://marsrovers.nasa.gov/science/objectives.html|archive-date=September 14, 2011|url-status=dead}}</ref>


The scientific objectives of the Mars Exploration Rover mission were to:<ref>{{cite web |title=Objectives - NASA |url=https://mars.nasa.gov/mer/mission/science/objectives/ |website=mars.nasa.gov |access-date=23 April 2023}}</ref>
* Search for and characterize a variety of rocks and soils that hold clues to past water activity. In particular, samples sought will include those that have minerals deposited by water-related processes such as [[Precipitation (meteorology)|precipitation]], [[Water vapor|evaporation]], [[Sedimentary rock|sedimentary cementation]] or [[hydrothermal activity]].
* Determine the distribution and composition of minerals, rocks, and soils surrounding the landing sites.
* Determine what [[Geology of Mars|geologic processes]] have shaped the local terrain and influenced the chemistry. Such processes could include water or wind erosion, sedimentation, hydrothermal mechanisms, volcanism, and cratering.
* Perform calibration and validation of surface observations made by [[Mars Reconnaissance Orbiter]] instruments. This will help determine the accuracy and effectiveness of various instruments that survey [[Geology of Mars|Martian geology]] from orbit.
* Search for iron-containing minerals, identify and quantify relative amounts of specific mineral types that contain water or were formed in water, such as iron-bearing carbonates.
* Characterize the [[mineralogy]] and textures of rocks and soils and determine the processes that created them.
* Search for geological clues to the [[Environmental science|environmental conditions]] that existed when liquid water was present.
* Assess whether those environments were conducive to life.


*Search for and characterize a variety of rocks and soils that hold clues to past [[Water on Mars|water]] activity. In particular, samples sought include those that have minerals deposited by water-related processes such as [[Precipitation (meteorology)|precipitation]], [[Water vapor|evaporation]], [[Sedimentary rock|sedimentary cementation]], or [[hydrothermal activity]].
NASA sought evidence of life on Mars, beginning with the question of whether the Martian environment was ever suitable for life. Life forms known to science require water, so the history of [[water on Mars]] is a critical piece of knowledge. Although the Mars Exploration Rovers did not have the ability to detect life directly, they offered very important information on the habitability of the environment during the planet's history.
*Determine the distribution and composition of minerals, rocks, and soils surrounding the landing sites.

*Determine what [[Geology of Mars|geologic processes]] have shaped the local terrain and influenced the chemistry. Such processes could include water or wind erosion, sedimentation, hydrothermal mechanisms, volcanism, and cratering.
==Design and construction==
*Perform calibration and validation of surface observations made by [[Mars Reconnaissance Orbiter]] (MRO) instruments. This will help determine the accuracy and effectiveness of various instruments that survey Martian geology from orbit.

*Search for iron-containing minerals, and to identify and quantify relative amounts of specific mineral types that contain water or were formed in water, such as iron-bearing carbonates.
[[File:Mars Exploration Rover.jpg|thumb|right|Annotated rover diagram]]
*Characterize the [[mineralogy]] and textures of rocks and soils to determine the processes that created them.
[[File:MER Spirit Lander Pan Sol16-A18R1 br2.jpg|thumb|right|''Spirit'' rover images its lander on the surface of Mars on January 18/19, 2004 (''Spirit'' Sol 16)<ref>[http://marsrover.nasa.gov/gallery/press/spirit/20040121a.html NASA.gov] {{Webarchive|url=https://web.archive.org/web/20110721054024/http://marsrover.nasa.gov/gallery/press/spirit/20040121a.html |date=July 21, 2011 }}, MER-A 20040121a</ref>]]
*Search for geological clues to the environmental conditions that existed when liquid water was present.
[[File:Spirit rock abrasion tool.jpg|thumb|The piece of metal with the American flag on ''Spirit''{{'}}s rock abrasion tool is made of aluminum recovered from the site of the World Trade Center towers.]]
*Assess whether those environments were conducive to life.
{{main|Mars Exploration Rover}}
{{see also|Comparison of embedded computer systems on board the Mars rovers}}

''Spirit'' (and its twin, ''[[Opportunity rover|Opportunity]]'') are six-wheeled, [[solar panel|solar-powered]] robots standing {{convert|1.5|m|ft|sp=us}} high, {{convert|2.3|m|ft|sp=us}} wide and {{convert|1.6|m|ft|sp=us}} long and weighing {{convert|180|kg|lb}}. Six wheels on a [[rocker-bogie]] system enabled mobility over rough terrain. Each wheel had its own motor. The vehicle was steered at front and rear and was designed to operate safely at tilts of up to 30 degrees. The maximum speed was {{convert|5|cm/s|in/s|sp=us}};<ref>{{cite web|url=http://marsrovers.jpl.nasa.gov/mission/spacecraft_rover_wheels.html|title=Mars Exploration Rover Mission: The Mission|website=marsrovers.jpl.nasa.gov}}</ref> {{convert|0.18|km/h|mph|sp=us}}, although the average speed was about {{convert|1|cm/s|in/s|sp=us}}. Both ''Spirit'' and ''Opportunity'' have pieces of the fallen [[World Trade Center (1973–2001)|World Trade Center]]'s metal on them that were "turned into shields to protect cables on the drilling mechanisms".<ref>{{cite news|url=https://www.nytimes.com/2004/11/07/science/07mars.html?pagewanted=2 |title=Martian Robots, Taking Orders From a Manhattan Walk-Up |work=The New York Times |date=November 7, 2004 |access-date=April 9, 2009 | first=Kenneth | last=Chang}}</ref><ref>{{cite book|first=Steve|last=Squyres|title=Roving Mars: Spirit, Opportunity, and the Exploration of the Red Planet|publisher=Hyperion Press|year=2005|url=https://books.google.com/books?id=GQBRAAAAMAAJ&q=%22World+Trade+Center%22|pages=113–117 | isbn=978-1-4013-0149-1}}</ref>

The solar arrays generated about 140 watts for up to four hours per Martian day (sol) while rechargeable [[lithium ion batteries]] stored energy for use at night. ''Spirit's'' onboard computer used a 20&nbsp;MHz [[IBM RAD6000|RAD6000]] CPU with 128 MB of DRAM, 3 MB of EEPROM, and 256 MB of flash memory. The rover's [[operating temperature]] ranged from {{convert|-40|to|+40|C|F}}. [[Radioisotope heater unit]]s provided a base level of heating, assisted by electrical heaters when necessary. A gold film and a layer of silica [[aerogel]] provided insulation.

Communications depended on an omnidirectional low-gain antenna communicating at a low data rate and a steerable high-gain antenna, both in direct contact with Earth. A low-gain antenna was also used to relay data to spacecraft orbiting Mars.

===Science payload===

The science instruments included:

* [[Pancam|Panoramic Camera (Pancam)]] – examined the texture, color, mineralogy, and structure of the local terrain.
* [[Navcam|Navigation Camera (Navcam)]] – monochrome with a higher field of view but lower resolution, for navigation and driving.
* [[Mini-TES|Miniature Thermal Emission Spectrometer (Mini-TES)]] – identified promising rocks and soils for closer examination, and determined the processes that formed them.
* [[Hazcam]]s, two B&W cameras with 120 degree field of view, that provided additional data about the rover's surroundings.

The rover arm held the following instruments:

* [[Mössbauer spectrometer]] (MB) [[MIMOS II]] – used for close-up investigations of the mineralogy of iron-bearing rocks and soils.
* [[Alpha particle X-ray spectrometer]] (APXS) – close-up analysis of the abundances of elements that make up rocks and soils.
* Magnets – for collecting magnetic dust particles.
* Microscopic Imager (MI) – obtained close-up, high-resolution images of rocks and soils.
* [[Rock Abrasion Tool]] (RAT) – exposed fresh material for examination by instruments on board.


== Mission timeline ==
== Mission timeline ==
{{Main|Timeline of Spirit}}
[[Image:Columbia Hills from MER-A landing site PIA05200 br2.jpg|thumb|right|Annotated Columbia Hills panorama from the ''Spirit'' landing site]]
[[File:MOLA spirit.jpg|thumb|left|An overall view of MER-A ''Spirit'' landing site (denoted with a star)]]


''Opportunity'' and ''Spirit'' rovers were part of the [[Mars Exploration Rover]] program in the long-term [[Mars Exploration Program]]. The Mars Exploration Program's four principal goals were to determine if the potential for life exists on Mars (in particular, whether recoverable water may be found on Mars), to characterize the Mars climate and its geology, and then to prepare for a potential human mission to Mars. The Mars Exploration Rovers were to travel across the Martian surface and perform periodic geologic analyses to determine if water ever existed on Mars as well as the types of minerals available, as well as to corroborate data taken by the [[Mars Reconnaissance Orbiter]] (MRO).<ref name="nasa2">{{cite web |url=https://mars.nasa.gov/mer/mission/science/objectives/ |title=Mars Exploration Rover Mission Science Objectives |publisher=mars.nasa.gov |access-date=February 19, 2021}}</ref> Both rovers were designed with an expected 90 [[Martian day|sols]] (92 Earth days) lifetime, but each lasted much longer than expected. ''Spirit''{{'s}} mission lasted 20 times longer than its expected lifetime, and its mission was declared ended on May 25, 2011, after it got stuck in soft sand and expended its power reserves trying to free itself. ''Opportunity'' lasted 55 times longer than its 90 sol planned lifetime, operating for {{age in days|2004|01|25|2019|02|13}} days from landing to mission end. An archive of weekly updates on the rover's status can be found at the ''Opportunity'' Update Archive.<ref name="OpportunityUpdateArchive">{{cite web |url=http://marsrovers.jpl.nasa.gov/mission/status_opportunity.html |title=Opportunity Update Archive |publisher=NASA/JPL |access-date=May 4, 2009 |archive-url=https://web.archive.org/web/20090507050626/http://marsrovers.jpl.nasa.gov/mission/status_opportunity.html |archive-date=May 7, 2009 |url-status=live}}</ref>
=== 2004 ===
The ''Spirit'' Mars rover landed successfully on the surface of Mars on 04:35 [[Ground UTC|SCET]] on January 4, 2004. This was the start of its 90-sol mission, but solar cell cleaning events would mean it was the start of a much longer mission, lasting until 2010.


=== Launch and landing ===
==== Landing site: ''Columbia'' Memorial Station ====
[[File:Animation of Spirit around Sun.gif|thumb|Animation of ''Spirit'' orbit. <Br>{{legend2| Yellow| Sun}}{{·}}{{legend2| RoyalBlue| Earth}}{{·}}{{legend2|Lime| Mars}}{{·}}{{legend2|Magenta| Spirit }}]]
[[Image:Columbia Hills from MER-A landing site PIA05200 br2.jpg|thumb|right|Annotated Columbia Hills panorama from the ''Spirit'' landing site]]
The MER-A (''Spirit'') and MER-B (''Opportunity'') were launched on June 10, 2003 and July 7, 2003, respectively. Though both probes launched on [[Boeing]] [[Delta II]] 7925-9.5 rockets from [[Cape Canaveral Space Launch Complex 17]] (CCAFS SLC-17), MER-B was on the heavy version of that launch vehicle, needing the extra energy for [[Trans-Mars injection]]. The launch vehicles were integrated onto pads right next to each other, with MER-A on CCAFS SLC-17A and MER-B on CCAFS SLC-17B. The dual pads allowed for working the 15- and 21-day planetary launch periods close together; the last possible launch day for MER-A was June 19, 2003 and the first day for MER-B was June 25, 2003. NASA's [[Launch Services Program]] managed the launch of both spacecraft.
''Spirit'' was targeted to a site that appears to have been affected by liquid water in the past, the crater [[Gusev (Martian crater)|Gusev]], a possible former lake in a giant [[impact crater]] about {{convert|10|km|mi|1|abbr=on}} from the center of the target ellipse<ref>{{cite web|url=http://marsoweb.nas.nasa.gov/landingsites/mer2003/topsites/final/Gusev/|title=Gusev Crater: LandingSites|website=marsoweb.nas.nasa.gov}}</ref> at {{Coord|14.5718|S|175.4785|E|globe:mars_type:landmark}}.<ref>[http://www.spaceflightnow.com/mars/mera/040113exploration.html Spaceflightnow.com], Destination Mars, Rover headed toward hilly vista for martian exploration<!-- Bot generated title --></ref>


After the airbag-protected landing craft settled onto the surface, the rover rolled out to take panoramic images. These give scientists the information they need to select promising geological targets and drive to those locations to perform on-site scientific investigations. The panoramic image below shows a slightly rolling surface, littered with small rocks, with hills on the horizon up to {{convert|3|km|mi|sp=us}} away.<ref>{{cite web|url=http://antwrp.gsfc.nasa.gov/apod/ap040114.html|title=APOD: 2004 January 14 – A Mars Panorama from the Spirit Rover|website=antwrp.gsfc.nasa.gov}}</ref> The MER team named the landing site "''Columbia'' Memorial Station," in honor of the seven [[astronauts]] killed in the [[Space Shuttle Columbia disaster|Space Shuttle ''Columbia'' disaster]].
''Spirit'' successfully landed on the surface of Mars on 04:35 [[Spacecraft Event Time]] (SCET) on January 4, 2004. This was the start of its 90-sol mission, but solar cell cleaning events would mean it was the start of a much longer mission, lasting until 2010. ''Spirit'' was targeted to a site that appears to have been affected by liquid water in the past, the crater [[Gusev (Martian crater)|Gusev]], a possible former lake in a giant [[impact crater]] about {{convert|10|km|mi|1|abbr=on}} from the center of the target ellipse<ref>{{cite web|url=http://marsoweb.nas.nasa.gov/landingsites/mer2003/topsites/final/Gusev/|title=Gusev Crater: LandingSites|website=marsoweb.nas.nasa.gov}}</ref> at {{Coord|14.5718|S|175.4785|E|globe:mars_type:landmark}}.<ref>[http://www.spaceflightnow.com/mars/mera/040113exploration.html Spaceflightnow.com], Destination Mars, Rover headed toward hilly vista for martian exploration<!-- Bot generated title --></ref> After the airbag-protected landing craft settled onto the surface, the rover rolled out to take panoramic images. These give scientists the information they need to select promising geological targets and drive to those locations to perform on-site scientific investigations.<ref>{{cite web|url=http://antwrp.gsfc.nasa.gov/apod/ap040114.html|title=APOD: 2004 January 14 – A Mars Panorama from the Spirit Rover|website=antwrp.gsfc.nasa.gov}}</ref> The MER team named the landing site "''Columbia'' Memorial Station," in honor of the seven [[astronauts]] killed in the [[Space Shuttle Columbia disaster|Space Shuttle ''Columbia'' disaster]].


"Sleepy Hollow," a shallow depression in the Mars ground at the right side of the above picture, was targeted as an early destination when the rover drove off its lander platform. NASA scientists were very interested in this crater. It is {{convert|9|m|ft|sp=us}} across and about {{convert|12|m|ft|sp=us}} north of the lander.

==== First color image ====
[[File:Spirit's First Color Photograph Mars.jpg|thumb|right|First color image compiled from images by ''Spirit''; it was the highest resolution color image taken on another planet.]]
[[File:Spirit's First Color Photograph Mars.jpg|thumb|right|First color image compiled from images by ''Spirit''; it was the highest resolution color image taken on another planet.]]
To the right is the first color image derived from images taken by the panoramic camera on the Mars Exploration Rover ''Spirit''. It was the highest resolution image taken on the surface of another planet. According to the camera designer Jim Bell of [[Cornell University]], the panoramic mosaic consists of four pancam images high by three wide. The picture shown originally had a full size of 4,000 by 3,000 [[pixels]]. However, a complete pancam panorama is even 8 times larger than that, and could be taken in stereo (i.e., two complete pictures, making the resolution twice as large again.) The colors are fairly accurate. (For a technical explanation, see [http://areo.info/mer/ colors outside the range of the human eye].)

The MER pancams are black-and-white instruments. Thirteen rotating filter wheels produce multiple images of the same scene at different wavelengths. Once received on Earth, these images can be combined to produce color images.<ref>{{cite web|url=http://www.lyle.org/~markoff/methods.html|archive-url=https://web.archive.org/web/20050424065044/http://www.lyle.org/~markoff/methods.html|url-status=dead|title=MER color imagery, methods|archive-date=April 24, 2005}}</ref>

==== Sol {{age in sols|2004|01|04|2004|01|21}} flash memory management anomaly ====
On January 21, 2004 (sol {{age in sols|2004|01|04|2004|01|21}}), ''Spirit'' abruptly ceased communicating with mission control. The next day the rover radioed a 7.8 bit/s beep, confirming that it had received a transmission from Earth but indicating that the craft believed it was in a fault mode. Commands would only be responded to intermittently. This was described as a very serious anomaly, but potentially recoverable if it were a software or memory corruption issue rather than a serious hardware failure. ''Spirit'' was commanded to transmit engineering data, and on January 23 sent several short low-bitrate messages before finally transmitting 73 megabits via [[X band]] to ''[[Mars Odyssey]]''. The readings from the engineering data suggested that the rover was not staying in sleep mode. As such, it was wasting its battery energy and overheating – risk factors that could potentially destroy the rover if not fixed soon. On sol 20, the command team sent it the command SHUTDWN_DMT_TIL ("Shutdown Dammit Until") to try to cause it to suspend itself until a given time. It seemingly ignored the command.

The leading theory at the time was that the rover was stuck in a "reboot loop". The rover was programmed to reboot if there was a fault aboard. However, if there was a fault that occurred during reboot, it would continue to reboot forever. The fact that the problem persisted through reboot suggested that the error was not in RAM, but in either the [[flash memory]], the [[EEPROM]], or a hardware fault. The last case would likely doom the rover. Anticipating the potential for errors in the flash memory and EEPROM, the designers had made it so that the rover could be booted without ever touching the flash memory. The radio itself could decode a limited command set – enough to tell the rover to reboot without using flash. Without access to flash memory the reboot cycle was broken.

On January 24, 2004 (sol {{age in sols|2004|01|04|2004|01|24}}) the rover repair team announced that the problem was with ''Spirit'''s flash memory and the software that wrote to it. The flash hardware was believed to be working correctly but the file management module in the software was "not robust enough" for the operations the ''Spirit'' was engaged in when the problem occurred, indicating that the problem was caused by a software bug as opposed to faulty hardware. NASA engineers finally came to the conclusion that there were too many files on the file system, which was a relatively minor problem. Most of these files contained unneeded in-flight data. After realizing what the problem was, the engineers deleted some files, and eventually reformatted the entire flash memory system. On February 6 (sol {{age in sols|2004|01|04|2004|02|06}}), the rover was restored to its original working condition, and science activities resumed.<ref name="planetary">[https://web.archive.org/web/20110719212649/http://www.planetary.org/blog/article/00000702/ Planetary Blog].</ref>

==== First intentional grinding of a rock on Mars ====
[[File:Rat post grind.jpg|thumb|right|Digital camera (the [[Pancam]]) image of a Mars rock (called [[Adirondack (Mars)|Adirondack]]) taken after a [[Rock Abrasion Tool|RAT]] grind (the rock grinding tool)]]
For the first intentional grinding of a rock on Mars, the ''Spirit'' team chose a rock called "[[Adirondack (Mars)|Adirondack]]". To make the drive there, the rover turned 40 degrees in short arcs totaling {{convert|95|cm}}. It then turned in place to face the target rock and drove four short moves straightforward totaling {{cvt|1.9|m}}. Adirondack was chosen over another rock called "Sashimi", which was closer to the rover, as Adirondack's surface was smoother, making it more suitable for the [[Rock Abrasion Tool]] (aka "RAT").<ref>{{cite press release |last=Webster |first=Guy |date=January 19, 2004 |title=Spirit Drives to a Rock Called 'Adirondack' for Close Inspection |url=https://mars.jpl.nasa.gov/mer/newsroom/pressreleases/20040119a.html |publisher=NASA |access-date=January 2, 2018}}</ref>

''Spirit'' made a small depression in the rock, {{convert|45.5|mm}} in diameter and {{convert|2.65|mm}} deep. Examination of the freshly exposed interior with the rover's microscopic imager and other instruments confirmed that the rock is volcanic basalt.<ref>{{cite press release |last=Webster |first=Guy |date=February 9, 2004 |title=Mars Rover Pictures Raise 'Blueberry Muffin' Questions |url=https://mars.nasa.gov/mer/newsroom/pressreleases/20040209a.html |publisher=NASA |access-date=January 2, 2018}}</ref>

==== Humphrey rock ====
On March 5, 2004, NASA announced that ''Spirit'' had found hints of water history on Mars in a rock dubbed "Humphrey". [[Raymond Arvidson]], the McDonnell University Professor and chair of Earth and Planetary Sciences at [[Washington University in St. Louis]], reported during a NASA press conference: "If we found this rock on Earth, we would say it is a volcanic rock that had a little fluid moving through it." In contrast to the rocks found by the twin rover ''Opportunity'', this one was formed from [[magma]] and then acquired bright material in small crevices, which look like crystallized minerals. If this interpretation holds true, the minerals were most likely dissolved in water, which was either carried inside the rock or interacted with it at a later stage, after it formed.<ref>{{cite web|url=http://marsrovers.jpl.nasa.gov/newsroom/pressreleases/20040305a.html|title=Mars Exploration Rover|last=mars.nasa.gov|website=marsrovers.jpl.nasa.gov}}</ref>

==== Bonneville crater ====
On sol {{age in sols|2004|01|04|2004|03|11}} March 11, 2004, ''Spirit'' reached [[Bonneville (crater)|Bonneville crater]] after a {{convert|400|yd|m|adj=on|sp=us}} journey.{{Citation needed|date=January 2009}} This crater is about {{convert|200|m|yd|sp=us}} across with a floor about {{convert|10|m|yd|sp=us}} [[Crater depth|below]] the surface.<ref>{{cite conference |title=Surfical geology of the Spirit rover traverse in Gusev Crater: dry and desiccating since the Hesperian |url=http://www.lpi.usra.edu/meetings/earlymars2004/pdf/8055.pdf |conference=Second Conference on Early Mars (2004) |access-date=January 26, 2009 |author=Golombek|page=1 |quote=The rim is ~{{convert|3|m|ft|sp=us}} high and although the crater is shallow (~{{convert|10|m|ft|sp=us}} deep)|display-authors=etal}}</ref> JPL decided that it would be a bad idea to send the rover down into the crater, as they saw no targets of interest inside. ''Spirit'' drove along the southern rim and continued to the southwest towards the Columbia Hills.
{{wide image|PIA05591 Spirit's Destination (panorama).jpg|800px|Bonneville Crater}}

''Spirit'' reached Missoula crater on sol 105. The crater is roughly {{convert|100|yd|m|sp=us}} across and {{convert|20|yd|m|sp=us}} deep. Missoula crater was not considered a high priority target due to the older rocks it contained. The rover skirted the northern rim, and continued to the southeast.
It then reached Lahontan crater on sol 118, and drove along the rim until sol 120. Lahontan is about {{convert|60|yd|m|sp=us}} across and about {{convert|10|yd|m|sp=us}} deep. A long, snaking sand dune stretches away from its southwestern side, and ''Spirit'' went around it, because loose sand dunes present an unknown risk to the ability of the rover wheels to get traction.

==== Columbia Hills ====
[[File:MER STS-107 Memorial.JPG|thumb|''Spirit'' contains a memorial to the crew of the [[Space Shuttle Columbia|Space Shuttle ''Columbia'']]'s [[STS-107]] 2003 mission, which disintegrated upon reentry.]]
''Spirit'' drove from Bonneville crater in a direct line to the Columbia Hills. The route was only directly controlled by the engineers when the terrain was difficult to navigate; otherwise, the rover drove in an autonomous mode. On sol 159, ''Spirit'' reached the first of many targets at the base of the [[Columbia Hills (Mars)|Columbia Hills]] called West Spur. Hank's Hollow was studied for 23 sols. Within Hank's Hollow was the strange-looking rock dubbed "[[Pot of Gold (Mars)|Pot of Gold]]". Analysing this rock was difficult for ''Spirit'', because it lay in a slippery area. After a detailed analysis with the AXPS-and the Mößbauer instrument it was detected that it contains hematite.<ref>{{cite web | url = http://www.jpl.nasa.gov/news/news.cfm?release=2004-161 | title = Mars Rovers Surprises Continue | work = JPL website | access-date = October 6, 2006}}</ref> This kind of rock can be built in connection with water.

As the produced energy from the solar panels was lowering due to the setting Sun and dust the Deep Sleep Mode was introduced. In this mode the rover was shut down completely during the night in order to save energy, even if the instruments would fail.<ref>{{cite web|url=http://marsrovers.jpl.nasa.gov/mission/status_spiritAll_2004.html#sol171|title=Mars Exploration Rover Mission: All Spirit Updates|website=marsrovers.jpl.nasa.gov|access-date=November 21, 2013|archive-date=June 25, 2007|archive-url=https://web.archive.org/web/20070625030222/http://marsrovers.jpl.nasa.gov/mission/status_spiritAll_2004.html#sol171|url-status=dead}}</ref> The route was selected so that the rover's panels were tilted as much as possible towards the winter sunlight.

From here, ''Spirit'' took a northerly path along the base of the hill towards the target Wooly Patch, which was studied from sol 192 to sol 199. By sol 203, ''Spirit'' had driven southward up the hill and arrived at the rock dubbed "Clovis". Clovis was ground and analyzed from sol 210 to sol 225. Following Clovis came the targets of Ebenezer (Sols 226–235), Tetl (sol 270), Uchben and Palinque (Sols 281–295), and Lutefisk (Sols 296–303). From Sols 239 to 262, ''Spirit'' powered down for [[solar conjunction]], when communications with the Earth are blocked. Slowly, ''Spirit'' made its way around the summit of Husband Hill, and at sol 344 was ready to climb over the newly designated "Cumberland Ridge" and into "[[Larry's Lookout]]" and "Tennessee Valley". ''Spirit'' also did some communication tests with the ESA orbiter ''[[Mars Express]]'' though most of the communication was usually done with the NASA orbiters ''[[2001 Mars Odyssey|Mars Odyssey]]'' and ''[[Mars Global Surveyor]]''.

=== 2005 ===

==== Driving up to Husband Hill ====
''Spirit'' had now been on Mars for one Earth year and was driving slowly uphill towards the top of Husband Hill. This was difficult because there were many rocky obstacles and sandy parts. This led frequently to slippage and the route could not be driven as planned. In February, ''Spirit'''s computer received a software update in order to drive more autonomously.<ref>{{cite web|url=http://marsrovers.jpl.nasa.gov/mission/status_spiritAll_2005.html#sol416|title=Mars Exploration Rover Mission: All Spirit Updates|website=marsrovers.jpl.nasa.gov|access-date=November 21, 2013|archive-date=November 23, 2013|archive-url=https://web.archive.org/web/20131123195957/http://marsrovers.jpl.nasa.gov/mission/status_spiritAll_2005.html#sol416|url-status=dead}}</ref> On sol 371, ''Spirit'' arrived at a rock named "Peace" near the top of Cumberland Ridge. ''Spirit'' ground ''Peace'' with the RAT on sol 373. By sol 390 (mid-February 2005), ''Spirit'' was advancing towards "Larry's Lookout", by driving up the hill in reverse. The scientists at this time were trying to conserve as much energy as possible for the climb.

''Spirit'' also investigated some targets along the way, including the soil target, "Paso Robles", which contained the highest amount of salt found on the red planet. The soil also contained a high amount of [[phosphorus]] in its composition, however not nearly as high as another rock sampled by ''Spirit'', "Wishstone". One of the scientists working with ''Spirit,'' Dr. Steve Squyres, said of the discovery, "We're still trying to work out what this means, but clearly, with this much salt around, water had a hand here".<ref>{{Cite web|last1=mars.nasa.gov|last2=NASA|first2=JPL|title=Mars Exploration Rover|url=https://mars.nasa.gov/mer/|access-date=February 12, 2021|website=mars.nasa.gov}}</ref>

<gallery class="center">
Image:Pot of gold-Close-med.jpg|[[Pot of Gold (Mars)|Pot of Gold rock]]
Image:Gusev - Colina Husband.jpg|''Spirit'''s traverse up Husband Hill
Image:MarsSunset.jpg|Martian sunset by ''Spirit'' at Gusev crater, May 19, 2005.
</gallery>

==== Dust devils ====
On March 9, 2005 (probably during the Martian night), the rover's solar panel efficiency jumped from the original ~60% to 93%, followed on March 10, by the sighting of [[dust devils]]. NASA scientists speculated a dust devil must have swept the solar panels clean, possibly significantly extending the duration of the mission. This also marked the first time dust devils had been spotted by ''Spirit'' or ''Opportunity''. Dust devils had previously only been photographed by the ''[[Mars Pathfinder|Pathfinder]]'' probe.

Mission members monitoring ''Spirit'' on Mars reported on March 12, 2005 (sol {{age in sols|2004|01|04|2005|03|12}}), that a lucky encounter with a dust devil had cleaned the robot's solar panels. Energy levels dramatically increased and daily science work was anticipated to be expanded.<ref>{{cite web | last = David | first = Leonard | date = March 12, 2005 | url = http://www.space.com/missionlaunches/spirit_dust_050312.html | title = Spirit Gets A Dust Devil Once-Over | publisher = Space.com | access-date =December 1, 2006}}</ref>
[[File:Marsdustdevil2.gif|thumb|center|800px|Video of a dust devil on Mars, photographed by ''Spirit''. The counter in the bottom-left corner indicates time in seconds after the first photo was taken in the sequence. At the final frames, one can see that the dust devil has left a trail on the Martian surface. Four other dust devils also appear in the background.]]
{{clear}}

==== Husband Hill summit ====
As of August ''Spirit'' was only {{convert|100|m}} away from the top. Here it was found that Husband Hill has two summits, with one a little higher than the other. On August 21 (sol {{age in sols|2004|01|04|2005|08|24}}),<ref>{{cite web |title=Rover Update: 2005: All |url=https://mars.nasa.gov/mer/mission/rover-status/spirit/2005/all/#sol579 |website=mars.nasa.gov |access-date=April 23, 2020 |language=en}}</ref> ''Spirit'' reached the real summit of Husband Hill. The rover was the first spacecraft to climb atop a mountain on another planet. The whole distance driven totaled 4971 meters.
The summit itself was flat. ''Spirit'' took a 360 degree panorama in real color, which included the whole Gusev crater. At night the rover observed the moons [[Phobos (moon)|Phobos]] and [[Deimos (moon)|Deimos]] in order to determine their orbits better.<ref name="nasa_2010_189">{{cite web
|authors=Staff |title=NASA Rover Finds Clue to Mars' Past And Environment for Life |url=http://www.nasa.gov/mission_pages/mer/news/mer20100603.html |work=[[NASA]] |date=June 3, 2010 |access-date=May 25, 2011}}</ref> On sol 656 ''Spirit'' surveyed the Mars sky and the opacity of the atmosphere with its pancam to make a coordinated science campaign with the Hubble Space Telescope in Earth orbit.<ref>{{cite web|url=http://marsrovers.jpl.nasa.gov/mission/status_spiritAll_2005.html#sol655|title=Mars Exploration Rover Mission: All Spirit Updates|website=marsrovers.jpl.nasa.gov|access-date=November 21, 2013|archive-date=November 23, 2013|archive-url=https://web.archive.org/web/20131123195957/http://marsrovers.jpl.nasa.gov/mission/status_spiritAll_2005.html#sol655|url-status=dead}}</ref>

From the peak ''Spirit'' spotted a striking formation, which was dubbed "Home Plate". This was an interesting target, but ''Spirit'' would be driven later to the McCool Hill to tilt its solar panels towards the Sun in the coming winter. At the end of October the rover was driven downhill and to Home Plate. On the way down ''Spirit'' reached the rock formation named "Comanche" on sol 690. Scientists used data from all three spectrometers to find out that about one-fourth of the composition of Comanche is magnesium iron carbonate. That concentration is 10 times higher than for any previously identified carbonate in a Martian rock. Carbonates originate in wet, near-neutral conditions but dissolve in acid. The find at Comanche is the first unambiguous evidence from the Mars Exploration Mission rovers for a past Martian environment that may have been more favorable to life than the wet but acidic conditions indicated by the rovers' earlier finds.<ref>{{cite web|url=http://www.nasa.gov/mission_pages/mer/multimedia/gallery/comanche-no-label.html|title=NASA – Carbonate-Containing Martian Rocks (False Color)|website=www.nasa.gov}}</ref>

{{Wide image|Everest Panorama from Mars.jpg|1100px|View from the Summit taken by ''Spirit'' on August 23, 2005, as the rover completed the climb up Husband Hill.}}

=== 2006 ===

==== Driving to McCool Hill ====
In 2006 ''Spirit'' drove towards an area dubbed Home Plate, and reached it in February. For events in 2006 by NASA see [https://web.archive.org/web/20120318103913/http://marsrover.nasa.gov/mission/status_spirit_2006.html NASA Spirit Archive 2006]

''Spirit's'' next stop was originally planned to be the north face of [[McCool Hill]], where ''Spirit'' would receive adequate sunlight during the Martian winter. On March 16, 2006, JPL announced that ''Spirit's'' troublesome front wheel had stopped working altogether. Despite this, ''Spirit'' was still making progress toward McCool Hill because the control team programmed the rover to drive toward McCool Hill backwards, dragging its broken wheel.<ref>{{cite web|url=http://marsrovers.jpl.nasa.gov/mission/status_spiritAll.html#sol778|title=Mars Exploration Rover Mission: All Spirit Updates|website=marsrovers.jpl.nasa.gov}}</ref> In late March, ''Spirit'' encountered loose soil that was impeding its progress toward McCool Hill. A decision was made to terminate attempts to reach McCool Hill and instead park on a nearby ridge named Low Ridge Haven.

{{multiple image
| align = right
| direction = horizontal
| image1 = Home plate anim.gif
| width1 = {{#expr: (130 * 331 / 285 ) round 0}}
| alt1 =
| caption1 = Curious rock near edge of "Home Plate" with a jutting portion. (Animated GIF image for stereoscopic perception.)
| image2 = Spirit MRO.jpg
| width2 = {{#expr: (130 * 1205 / 904 ) round 0}}
| alt2 =
| caption2 = Picture of ''Spirit'' (September 29, 2006), including tracks, taken from the ''[[Mars Reconnaissance Orbiter]]''
}}
''Spirit'' arrived at the north west corner of [[Home Plate (Mars)|Home Plate]], a raised and layered outcrop on sol 744 (February 2006) after an effort to maximize driving. Scientific observations were conducted with ''Spirit's'' robotic arm.

==== Low Ridge Haven ====
[[File:PIA08576-Spirit Rover-Possible Meteorites at Low Ridge.jpg|thumb|upright=0.5|Possible meteorites found at Low Ridge (June 16, 2006)]]
Reaching the ridge on April 9, 2006, and parking on the ridge with an 11° incline to the north, ''Spirit'' spent the next eight months on the ridge, spending that time undertaking observations of changes in the surrounding area.<ref>{{cite web|url=http://www.nasa.gov/mission_pages/mars/missions/mer/mer-20060412.html|title=NASA – NASA Mars Rovers Head for New Sites After Studying Layers|website=www.nasa.gov}}</ref> No drives were attempted because of the low energy levels the rover was experiencing during the Martian winter. The rover made its first drive, a short turn to position targets of interest within reach of the robotic arm, in early November 2006, following the shortest days of winter and solar conjunction when communications with Earth were severely limited.

While at Low Ridge, ''Spirit'' imaged two rocks of similar chemical nature to that of ''Opportunity'''s [[Heat Shield Rock]], a [[meteorite]] on the surface of Mars. Named "Zhong Shan" for [[Sun Yat-sen]] and "Allan Hills" for the [[Allan Hills|location]] in [[Antarctica]] where several Martian meteorites have been found, they stood out against the background rocks that were darker. Further spectrographic testing is being done to determine the exact composition of these rocks, which may turn out to also be meteorites.

=== 2007 ===

==== Software upgrade ====
On January 4, 2007 (sol {{age in sols|2004|01|04|2007|01|04}}), both rovers received new flight software to the onboard computers. The update was received just in time for the third anniversary of their landing. The new systems let the rovers decide whether or not to transmit an image, and whether or not to extend their arms to examine rocks, which would save much time for scientists as they would not have to sift through hundreds of images to find the one they want, or examine the surroundings to decide to extend the arms and examine the rocks.<ref>{{cite news| url=http://www.cbc.ca/technology/story/2007/01/04/tech-mars.html | work=CBC News | title=Old rovers learn new tricks | date=January 4, 2007}}</ref>

====Silica Valley====
[[File:Spirit Mars Silica April 20 2007.jpg|thumb|right|Rover exposes silica-rich dust (April 20, 2007)]]
''Spirit'''s dead wheel turned out to have a silver lining. As it was traveling in March 2007, pulling the dead wheel behind, the wheel scraped off the upper layer of the Martian soil, uncovering a patch of ground that scientists say shows evidence of a past environment that would have been perfect for microbial life. It is similar to areas on Earth where water or steam from hot springs came into contact with volcanic rocks. On Earth, these are locations that tend to teem with bacteria, said rover chief scientist [[Steve Squyres]]. "We're really excited about this," he told a meeting of the American Geophysical Union (AGU). The area is extremely rich in [[Silicon dioxide|silica]]–the main ingredient of window glass. The researchers have now concluded that the bright material must have been produced in one of two ways. One: hot-spring deposits produced when water dissolved silica at one location and then carried it to another (i.e. a geyser). Two: acidic steam rising through cracks in rocks stripped them of their mineral components, leaving silica behind. "The important thing is that whether it is one hypothesis or the other, the implications for the former habitability of Mars are pretty much the same," Squyres explained to BBC News. Hot water provides an environment in which [[microbe]]s can thrive and the precipitation of that silica entombs and preserves them. Squyres added, "You can go to [[hot spring]]s and you can go to [[fumarole]]s and at either place on Earth it is teeming with life – [[Microorganism|microbial life]]."<ref name="Amos">{{cite news | last = Amos | first = Jonathan | title = Mars robot unearths microbe clue | work = NASA says its robot rover Spirit has made one of its most significant discoveries on the surface of Mars. |publisher=BBC News | date = December 11, 2007 | url = http://news.bbc.co.uk/2/hi/science/nature/7137793.stm | access-date =December 12, 2007 }}</ref><ref name="20071210a">{{cite web | last = Bertster | first = Guy | title = Mars Rover Investigates Signs of Steamy Martian Past | work = Press Release | publisher = Jet Propulsion Laboratory, Pasadena, California | date = December 10, 2007 | url = http://marsrovers.jpl.nasa.gov/newsroom/pressreleases/20071210a.html | access-date =December 12, 2007 }}</ref>

==== Global dust storm and Home Plate ====
During 2007, ''Spirit'' spent several months near the base of the Home Plate plateau. On sol 1306 ''Spirit'' climbed onto the eastern edge of the plateau. In September and October it examined rocks and soils at several locations on the southern half of the plateau. On November 6, ''Spirit'' had reached the western edge of Home Plate, and started taking pictures for a panoramic overview of the western valley, with Grissom Hill and Husband Hill visible. The panorama image was published on NASA's website on January 3, 2008, to little attention, until January 23, when an independent website published a magnified detail of the image that showed a rock feature a few centimeters high resembling a humanoid figure seen from the side with its right arm partially raised.<ref>[http://www.planetary.org/blog/article/00001305/ Planetary.org] {{Webarchive|url=https://web.archive.org/web/20120420040458/http://www.planetary.org/blog/article/00001305/ |date=April 20, 2012 }} Emily Lakdawalla, ''Teeny little Bigfoot on Mars'', January 23, 2008 | 12:41 PST | 20:41 UTC</ref><ref>{{Cite APOD |date=January 29, 2008 |title=Spirit's West Valley Panorama image |access-date=}}</ref>

[[File:Mars Spirit rover's solar panels covered with Dust - October 2007.jpg|thumb|right|Circular projection showing ''Spirit'''s solar panels covered in dust – October 2007]]
Towards the end of June 2007, a series of dust storms began clouding the Martian atmosphere with dust. The storms intensified and by July 20, both ''Spirit'' and ''Opportunity'' were facing the real possibility of system failure due to lack of energy. NASA released a statement to the press that said (in part) "We're rooting for our rovers to survive these storms, but they were never designed for conditions this intense".<ref>{{Cite press release| url=http://www.jpl.nasa.gov/news/news.cfm?release=2007-080| access-date=August 21, 2009| title=NASA Mars Rovers Braving Severe Dust Storms| date=July 27, 2007| publisher=[[Jet Propulsion Laboratory]]}}</ref> The key problem caused by the dust storms was a dramatic reduction in solar energy caused by there being so much dust in the atmosphere that it was blocking 99 percent of direct sunlight to ''Opportunity'', and slightly more to ''Spirit''.

Normally the solar arrays on the rovers are able to generate up to {{Convert|700|Wh}} of energy per [[Martian day]]. After the storms, the amount of energy generated was greatly reduced to {{Convert|128|Wh}}. If the rovers generate less than {{Convert|150|Wh}} per day they must start draining their batteries to run survival heaters. If the batteries run dry, key electrical elements are likely to fail due to the intense cold. Both rovers were put into the lowest-power setting in order to wait out the storms. In early August the storms began to clear slightly, allowing the rovers to successfully charge their batteries. They were kept in hibernation in order to wait out the remainder of the storm.<ref>{{Cite press release| url=http://marsrovers.jpl.nasa.gov/newsroom/pressreleases/20070807a.html| access-date=August 21, 2009| title=Martian Skies Brighten Slightly| date=August 7, 2007| publisher=[[Jet Propulsion Laboratory]]}}</ref>

=== 2008 ===

==== Hibernating ====
The main concern was the energy level for ''Spirit''. To increase the amount of light hitting the solar panels, the rover was parked in the northern part of Home Plate on as steep a slope as possible. It was expected that the level of dust cover on the solar panels would increase by 70 percent and that a slope of 30 degrees would be necessary to survive the winter. In February, a tilt of 29.9 degrees was achieved. Extra energy was available at times, and a high definition panorama named ''Bonestell'' was produced. At other times when there was only enough solar energy to recharge the batteries, communication with Earth was minimized and all unnecessary instruments were switched off. At winter solstice the energy production declined to 235 watt hours per sol.<ref>{{cite web|url=http://marsrovers.jpl.nasa.gov/mission/status_spiritAll_2008.html|title=Mars Exploration Rover Mission: All Spirit Updates|website=marsrovers.jpl.nasa.gov}}</ref>

==== Winter dust storm ====
On November 10, 2008, a large dust storm further reduced the output of the solar panels to {{Convert|89|Wh}} per day—a critically low level.<ref>{{Cite press release| url=http://marsrovers.nasa.gov/newsroom/pressreleases/20081110a.html |access-date=August 21, 2009|title=Dust Storm Cuts Energy Supply of NASA Mars Rover Spirit| date= November 10, 2008| publisher=[[Jet Propulsion Laboratory]]}}</ref> NASA officials were hopeful that ''Spirit'' would survive the storm, and that the energy level would rise once the storm had passed and the skies started clearing. They attempted to conserve energy by shutting down systems for extended periods of time, including the heaters. On November 13, 2008, the rover awoke and communicated with mission control as scheduled.<ref>{{Cite news| url=https://www.newscientist.com/article/dn16050-spirit-rover-recuperating-after-dust-storm.html| access-date=August 21, 2009 | title=Spirit rover recuperating after dust storm| date=November 14, 2009| first=Rachel| last=Courtland| publisher=[[New Scientist]]}}</ref>

From November 14, 2008, to November 20, 2008 (sols {{age in sols|2004|01|04|2008|11|14}} to {{age in sols|2004|01|04|2008|11|20}}), ''Spirit'' averaged {{Convert|169|Wh}} per day. The heaters for the thermal emission spectrometer, which used about {{Convert|27|Wh}} per day, were disabled on November 11, 2008. Tests on the thermal emission spectrometer indicate that it was undamaged, and the heaters would be enabled with sufficient energy.<ref>{{cite press release| url=http://marsrovers.jpl.nasa.gov/mission/status_spiritAll_2008.html#sol1730| access-date=August 21, 2009 |title=sol 1730–1736, November 14–20, 2008: Serious but Stable | date=November 20, 2008| publisher=[[Jet Propulsion Laboratory]]}}</ref> The [[solar conjunction]], where the Sun is between Earth and Mars, started on November 29, 2008, and communication with the rovers was not possible until December 13, 2008.<ref>{{cite press release| url=http://marsrovers.jpl.nasa.gov/mission/status_opportunityAll_2008.html#sol1709| access-date=August 21, 2009 |title=sol 1709–1715, November 13–19, 2008: Opportunity Prepares for Two Weeks of Independent Study | date= November 19, 2008| publisher=[[Jet Propulsion Laboratory]]}}</ref>

=== 2009 ===

==== Increased energy ====
On February 6, 2009, a beneficial wind blew off some of the dust accumulated on the panels. This led to an increase in energy output to {{Convert|240|Wh}} per day. NASA officials stated that this increase in energy was to be used predominantly for driving.<ref>{{cite web|access-date=February 17, 2009|url=http://marsrovers.jpl.nasa.gov/newsroom/pressreleases/20090212a.html |title=Spirit Gets Energy Boost from Cleaner Solar Panels |publisher=NASA/JPL }}</ref>

On April 18, 2009 (sol {{age in sols|2004|01|04|2009|04|18}}) and April 28, 2009 (sol {{age in sols|2004|01|04|2009|04|28}}) energy output of the solar arrays were increased by cleaning events.<ref>{{cite web |url=http://marsrovers.jpl.nasa.gov/mission/status_spiritAll.html#sol1879 |title=Another Reset and a Cleaning Event |publisher=NASA/JPL |date=April 22, 2009 |access-date=April 25, 2009 }}</ref><ref name="Update20090429">{{cite web|url=http://marsrovers.jpl.nasa.gov/mission/status_spiritAll.html#sol1886 |title=Well Behaved, Less Dusty, in Difficult Terrain |publisher=NASA/JPL |date=April 29, 2009 |access-date=May 4, 2009 }}</ref> The energy output of ''Spirit's'' solar arrays climbed from {{Convert|223|Wh}} per day on March 31, 2009, to {{Convert|372|Wh}} per day on April 29, 2009.<ref name="Update20090429" />

==== Sand trap ====
[[File:Spirit Sandbox Setup.jpg|thumb|right|Engineers attempt to replicate conditions in the laboratory of ''Spirit'''s entrapment on a rock and in fluffy material churned by the rover's left-front wheel.]]


On May 1, 2009 (sol {{age in sols|2004|01|04|2009|05|01}}), the rover became stuck in soft sand, the machine resting upon a cache of [[iron(III) sulfate]] ([[jarosite]]) hidden under a veneer of normal-looking soil. Iron sulfate has very little cohesion, making it difficult for the rover's wheels to gain traction.<ref>{{Cite news
On May 1, 2009 (sol {{age in sols|2004|01|04|2009|05|01}}), the rover became stuck in soft sand, the machine resting upon a cache of [[iron(III) sulfate]] ([[jarosite]]) hidden under a veneer of normal-looking soil. Iron sulfate has very little cohesion, making it difficult for the rover's wheels to gain traction.<ref>{{Cite news
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On January 26, 2010 (sol {{age in sols|2004|01|04|2010|01|26}}), after several months attempting to free the rover, NASA decided to redefine the mobile robot mission by calling it a stationary research platform. Efforts were directed in preparing a more suitable orientation of the platform in relation to the Sun in an attempt to allow a more efficient recharge of the platform's batteries. This was needed to keep some systems operational during the Martian winter.<ref>{{Cite news |title=Now A Stationary Research Platform, NASA's Mars Rover Spirit Starts a New Chapter in Red Planet Scientific Studies |url=http://www.jpl.nasa.gov/freespirit/ |date=January 26, 2010 |work=NASA |access-date=June 26, 2009 |archive-url=https://web.archive.org/web/20141129050447/http://www.jpl.nasa.gov/freespirit/ |archive-date=November 29, 2014 |url-status=dead }}</ref> On March 30, 2010, Spirit skipped a planned communication session and as anticipated from recent power-supply projections, had probably entered a low-power hibernation mode.<ref>{{Cite news |title=Spirit May Have Begun Months-Long Hibernation |url=http://marsrovers.jpl.nasa.gov/newsroom/pressreleases/20100331a.html |date=March 31, 2010 |work=NASA }}</ref>
JPL team members simulated the situation by means of a rover mock-up and computer models in an attempt to get the rover back on track. To reproduce the same [[soil mechanics|soil mechanical]] conditions on Earth as those prevailing on Mars under low [[Gravitation|gravity]] and under very weak atmospheric pressure, tests with a lighter version of a mock-up of ''Spirit'' were conducted at JPL in a special sandbox to attempt to simulate the [[cohesion (geology)|cohesion behavior]] of [[Consolidation (soil)|poorly consolidated soils]] under low gravity.<ref name="Free_Spirit">{{cite web|url=https://www.jpl.nasa.gov/freespirit/|title=Free Spirit - jpl.nasa.gov|website=www.jpl.nasa.gov}}</ref><ref>{{cite web |url=http://www.sphere.com/nation/article/to-rescue-rover-on-mars-nasa-practices-in-pasadena-sandbox/19273469 |title=A How a Sandbox Could Save Mars Rover |publisher=sphere.com |date=December 10, 2009 |archive-url=https://web.archive.org/web/20100117141008/http://www.sphere.com/nation/article/to-rescue-rover-on-mars-nasa-practices-in-pasadena-sandbox/19273469 |archive-date=January 17, 2010}}</ref> Preliminary extrication drives began on November 17, 2009.<ref name="SpiritUpdateArchive">{{cite web|url=http://marsrovers.jpl.nasa.gov/mission/status_spirit.html |title=Spirit Update Archive |publisher=NASA/JPL |access-date=May 4, 2009}}</ref>


The last communication with the rover was March 22, 2010 (sol {{age in sols|2004|01|04|2010|03|22}})<ref>{{cite web|url=http://marsrovers.jpl.nasa.gov/mission/status_spiritAll.html#sol2533 |title=Spirit status |publisher=NASA |access-date=February 28, 2011}}</ref> and there is a strong possibility the rover's batteries lost so much energy at some point that the mission clock stopped. In previous winters the rover was able to park on a Sun-facing slope and keep its internal temperature above {{convert|−40|C|F}}, but since the rover was stuck on flat ground it is estimated that its internal temperature dropped to {{convert|−55|C|F}}. If ''Spirit'' had survived these conditions and there had been a cleaning event, there was a possibility that with the southern summer solstice in March 2011, solar energy would increase to a level that would wake up the rover.<ref>A.J.S. Rayl [http://www.planetary.org/news/2010/0731_Mars_Exploration_Rovers_Update_Spirit.html Spirit Sleeps Soundlessly, Opportunity Turns a Corner] {{Webarchive|url=https://web.archive.org/web/20120401234545/http://www.planetary.org/news/2010/0731_Mars_Exploration_Rovers_Update_Spirit.html |date=April 1, 2012 }} ''[[Planetary Society]]'' July 31, 2010</ref>
On December 17, 2009 (sol {{age in sols|2004|01|04|2009|12|17}}), the right-front wheel suddenly began to operate normally for the first three out of four rotations attempts. It was unknown what effect it would have on freeing the rover if the wheel became fully operational again. The right rear wheel had also stalled on November 28 (sol {{age in sols|2004|01|04|2009|11|28}}) and remained inoperable for the remainder of the mission. This left the rover with only four fully operational wheels.<ref>{{Cite news |title=Right-Front Wheel Rotations |url=http://marsrover.nasa.gov/spotlight/20091217a.html |date=December 17, 2009 |work=NASA |access-date=December 25, 2009 |archive-url=https://web.archive.org/web/20120318103830/http://marsrover.nasa.gov/spotlight/20091217a.html |archive-date=March 18, 2012 |url-status=dead }}</ref> If the team could not gain movement and adjust the tilt of the solar panels, or gain a beneficial wind to clean the panels, the rover would only be able to sustain operations until May 2010.<ref>{{Cite news |date=December 31, 2009 |title=NASA's Mars Rover has Uncertain Future as Sixth Anniversary Nears |url=http://marsrover.nasa.gov/spotlight/20091231a.html |access-date=January 1, 2010 |work=NASA |archive-url=https://web.archive.org/web/20120318103834/http://marsrover.nasa.gov/spotlight/20091231a.html |archive-date=March 18, 2012 |url-status=dead }}</ref>


''Spirit'' remains silent at its location, called "Troy," on the west side of Home Plate. There was no communication with the rover after March 22, 2010 (sol {{age in sols|2004|01|04|2010|03|22}}).<ref name="Distillations">{{cite journal |last1=Reisert |first1=Sarah |title=Life on Mars |journal=Distillations |date=2017 |volume=3 |issue=1 |pages=42–45 |url=https://www.sciencehistory.org/distillations/magazine/life-on-mars |access-date=April 13, 2018 |archive-date=March 25, 2019 |archive-url=https://web.archive.org/web/20190325082704/https://www.sciencehistory.org/distillations/magazine/life-on-mars |url-status=dead }}</ref>
=== 2010 ===


It is likely that ''Spirit'' experienced a low-power fault and had turned off all sub-systems, including communication, and gone into a deep sleep, trying to recharge its batteries. It is also possible that the rover had experienced a mission clock fault. If that had happened, the rover would have lost track of time and tried to remain asleep until enough sunlight struck the solar arrays to wake it. This state is called "Solar Groovy." If the rover woke up from a mission clock fault, it would only listen. Starting on July 26, 2010 (sol {{age in sols|2004|01|04|2010|07|26}}), a new procedure to address the possible mission clock fault was implemented.
==== Mars winter at Troy ====
{{wideimage|Free Spirit.jpg|1100px|Color panorama from "Troy" embedding location, Husband Hill in Center distance (compiled from images taken 14 May to 20 June 2009)}}


=== End of mission ===
On January 26, 2010 (sol {{age in sols|2004|01|04|2010|01|26}}), after several months attempting to free the rover, NASA decided to redefine the mobile robot mission by calling it a stationary research platform. Efforts were directed in preparing a more suitable orientation of the platform in relation to the Sun in an attempt to allow a more efficient recharge of the platform's batteries. This was needed to keep some systems operational during the Martian winter.<ref>{{Cite news |title=Now A Stationary Research Platform, NASA's Mars Rover Spirit Starts a New Chapter in Red Planet Scientific Studies |url=http://www.jpl.nasa.gov/freespirit/ |date=January 26, 2010 |work=NASA |access-date=June 26, 2009 |archive-url=https://web.archive.org/web/20141129050447/http://www.jpl.nasa.gov/freespirit/ |archive-date=November 29, 2014 |url-status=dead }}</ref> On March 30, 2010, Spirit skipped a planned communication session and as anticipated from recent power-supply projections, had probably entered a low-power hibernation mode.<ref>{{Cite news |title=Spirit May Have Begun Months-Long Hibernation |url=http://marsrovers.jpl.nasa.gov/newsroom/pressreleases/20100331a.html |date=March 31, 2010 |work=NASA }}</ref>
JPL continued attempts to regain contact with ''Spirit'' until May 25, 2011, when NASA announced the end of contact efforts and the completion of the mission.<ref name="spirit contact conclusion2"/><ref name="spirit contact conclusion1"/><ref name="universetoday-2011-05-25">{{cite news |url=https://www.universetoday.com/85923/end-of-the-road-for-spirit-rover/ |title=End of the Road for Spirit Rover |publisher=Universe Today | author=Atkinson, Nancy |date=May 25, 2011 |access-date=May 25, 2011 }}</ref>
According to NASA, the rover likely experienced excessively cold "internal temperatures" due to "inadequate energy to run its survival heaters" that, in turn, was a result of "a stressful Martian winter without much sunlight." Many critical components and connections would have been "susceptible to damage from the cold."<ref name="spirit contact conclusion1"/> Assets that had been needed to support ''Spirit'' were transitioned to support ''Spirit's'' then still-active twin, [[Opportunity rover|''Opportunity'']].<ref name="spirit contact conclusion2"/>


The primary surface mission for ''Spirit'' was planned to last at least 90 [[Timekeeping on Mars|sols]]. The mission received several extensions and lasted about 2,208 sols. On August 11, 2007, ''Spirit'' obtained the second longest operational duration on the surface of Mars for a lander or rover at 1282 Sols, one sol longer than the [[Viking 2]] lander. Viking 2 was powered by a nuclear cell whereas ''Spirit'' is powered by solar arrays. Until ''Opportunity'' overtook it on May 19, 2010, the Mars probe with longest operational period was [[Viking 1]] that lasted for 2245 Sols on the surface of Mars. On March 22, 2010, ''Spirit'' sent its last communication, thus falling just over a month short of surpassing Viking 1's operational record. An archive of weekly updates on the rover's status can be found at the ''Spirit'' Update Archive.<ref name="SpiritUpdateArchive">{{cite web|url=http://marsrovers.jpl.nasa.gov/mission/status_spirit.html |title=Spirit Update Archive |publisher=NASA/JPL |access-date=May 4, 2009}}</ref>
[[File:HomePlate.png|thumb|right|''Spirit'''s concluding journey around Homeplate and ending location.]]
The last communication with the rover was March 22, 2010 (sol {{age in sols|2004|01|04|2010|03|22}})<ref>{{cite web|url=http://marsrovers.jpl.nasa.gov/mission/status_spiritAll.html#sol2533 |title=Spirit status |publisher=NASA |access-date=February 28, 2011}}</ref> and there is a strong possibility the rover's batteries lost so much energy at some point that the mission clock stopped. In previous winters the rover was able to park on a Sun-facing slope and keep its internal temperature above {{convert|−40|C|F}}, but since the rover was stuck on flat ground it is estimated that its internal temperature dropped to {{convert|−55|C|F}}. If ''Spirit'' had survived these conditions and there had been a cleaning event, there was a possibility that with the southern summer solstice in March 2011, solar energy would increase to a level that would wake up the rover.<ref>A.J.S. Rayl [http://www.planetary.org/news/2010/0731_Mars_Exploration_Rovers_Update_Spirit.html Spirit Sleeps Soundlessly, Opportunity Turns a Corner] {{Webarchive|url=https://web.archive.org/web/20120401234545/http://www.planetary.org/news/2010/0731_Mars_Exploration_Rovers_Update_Spirit.html |date=April 1, 2012 }} ''[[Planetary Society]]'' July 31, 2010</ref>


''Spirit's'' total odometry is {{convert|7730.50|m|mi|2|sp=us}}.<ref>{{cite web |url=http://marsrovers.nasa.gov/mission/status_spiritAll.html |title=Spirit Updates |access-date=May 14, 2012 |archive-url=https://web.archive.org/web/20140228232506/http://marsrovers.nasa.gov/mission/status_spiritAll.html |archive-date=February 28, 2014 |url-status=dead }}</ref>
==== Communication attempts ====
''Spirit'' remains silent at its location, called "Troy," on the west side of Home Plate. There was no communication with the rover after March 22, 2010 (sol {{age in sols|2004|01|04|2010|03|22}}).<ref name="Distillations">{{cite journal|last1= Reisert |first1=Sarah |title=Life on Mars |journal=Distillations |date=2017|volume=3|issue=1 |pages=42–45 |url=https://www.sciencehistory.org/distillations/magazine/life-on-mars|access-date=April 13, 2018}}</ref>


==Design and construction==
It is likely that ''Spirit'' experienced a low-power fault and had turned off all sub-systems, including communication, and gone into a deep sleep, trying to recharge its batteries. It is also possible that the rover had experienced a mission clock fault. If that had happened, the rover would have lost track of time and tried to remain asleep until enough sunlight struck the solar arrays to wake it. This state is called "Solar Groovy." If the rover woke up from a mission clock fault, it would only listen. Starting on July 26, 2010 (sol {{age in sols|2004|01|04|2010|07|26}}), a new procedure to address the possible mission clock fault was implemented.
{{main|Mars Exploration Rover#Scientific instrumentation}}
[[File:Mars Exploration Rover.jpg|thumb|right|Annotated rover diagram]]
[[File:MER Pancam.JPG|thumb|right|upright|Pancam Mast Assembly (PMA)]]


''Spirit'' (and its twin, ''[[Opportunity (rover)|Opportunity]]'') are six-wheeled, [[solar panel|solar-powered]] robots standing {{convert|1.5|m|ft|sp=us}} high, {{convert|2.3|m|ft|sp=us}} wide and {{convert|1.6|m|ft|sp=us}} long and weighing {{convert|180|kg|lb}}. Six wheels on a [[rocker-bogie]] system enabled mobility over rough terrain. Each wheel had its own motor. The vehicle was steered at front and rear and was designed to operate safely at tilts of up to 30 degrees. The maximum speed was {{convert|5|cm/s|in/s|sp=us}};<ref>{{cite web|url=http://marsrovers.jpl.nasa.gov/mission/spacecraft_rover_wheels.html|title=Mars Exploration Rover Mission: The Mission|website=marsrovers.jpl.nasa.gov}}</ref> {{convert|0.18|km/h|mph|sp=us}}, although the average speed was about {{convert|1|cm/s|in/s|sp=us}}. Both ''Spirit'' and ''Opportunity'' have pieces of the fallen [[World Trade Center (1973–2001)|World Trade Center]]'s metal on them that were "turned into shields to protect cables on the drilling mechanisms".<ref>{{cite news|url=https://www.nytimes.com/2004/11/07/science/07mars.html?pagewanted=2 |title=Martian Robots, Taking Orders From a Manhattan Walk-Up |work=The New York Times |date=November 7, 2004 |access-date=April 9, 2009 | first=Kenneth | last=Chang}}</ref><ref>{{cite book|first=Steve|last=Squyres|title=Roving Mars: Spirit, Opportunity, and the Exploration of the Red Planet|publisher=Hyperion Press|year=2005|url=https://books.google.com/books?id=GQBRAAAAMAAJ&q=%22World+Trade+Center%22|pages=113–117 | isbn=978-1-4013-0149-1}}</ref>
Each sol, the Deep Space Network mission controllers sent a set of X-band "Sweep & Beep" commands. If the rover had experienced a mission clock fault and then had been awoken during the day, it would have listened during brief, 20-minute intervals during each hour awake. Due to the possible clock fault, the timing of these 20-minute listening intervals was not known, so multiple "Sweep & Beep" commands were sent. If the rover heard one of these commands, it would have responded with an X-band beep signal, updating the mission controllers on its status and allowing them to investigate the state of the rover further. But even with this new strategy, there was no response from the rover.


Solar arrays generated about 140 watts for up to fourteen hours per sol, while rechargeable [[lithium ion batteries]] stored energy for use at night. ''Spirit''{{'}}s onboard computer uses a 20&nbsp;MHz [[IBM RAD6000|RAD6000]] CPU with 128&nbsp;MB of DRAM and 3&nbsp;MB of EEPROM.<ref>{{cite web |title=The Rover's "Brains" - NASA |url=https://mars.nasa.gov/mer/mission/rover/brains/ |website=mars.nasa.gov |access-date=23 April 2023}}</ref> The rover's [[operating temperature]] ranges from {{convert|−40|to|+40|C|F}} and [[Radioisotope heater unit|radioisotope heaters]] provide a base level of heating, assisted by electrical heaters when necessary.<ref>{{cite web |title=The Rover's Temperature Controls - NASA |url=https://mars.nasa.gov/mer/mission/rover/temperature/ |website=mars.nasa.gov |access-date=23 April 2023}}</ref>
The rover had driven {{convert|7730.50|m|mi}} until it became immobile.<ref>{{cite web|url=http://marsrovers.jpl.nasa.gov/mission/status_spiritAll_2010.html#sol2335|title=Mars Exploration Rover Mission: All Spirit Updates|website=marsrovers.jpl.nasa.gov}}</ref>


Communications depended on an omnidirectional low-gain antenna communicating at a low data rate and a steerable high-gain antenna, both in direct contact with Earth. A low-gain antenna was also used to relay data to spacecraft orbiting Mars.<ref>{{cite web |title=The Rover's Antennas - NASA |url=https://mars.nasa.gov/mer/mission/rover/antennas/ |website=mars.nasa.gov |access-date=23 April 2023}}</ref>
=== 2011 ===


==== Mission end ====
===Science payload===
JPL continued attempts to regain contact with ''Spirit'' until May 25, 2011, when NASA announced the end of contact efforts and the completion of the mission.<ref name="spirit contact conclusion2"/><ref name="spirit contact conclusion1"/><ref name="universetoday-2011-05-25">{{cite news |url=https://www.universetoday.com/85923/end-of-the-road-for-spirit-rover/ |title=End of the Road for Spirit Rover |publisher=Universe Today | author=Atkinson, Nancy |date=May 25, 2011 |access-date=May 25, 2011 }}</ref>
According to NASA, the rover likely experienced excessively cold "internal temperatures" due to "inadequate energy to run its survival heaters" that, in turn, was a result of "a stressful Martian winter without much sunlight." Many critical components and connections would have been "susceptible to damage from the cold."<ref name="spirit contact conclusion1"/> Assets that had been needed to support ''Spirit'' were transitioned to support ''Spirit's'' then still-active [[Opportunity rover|''Opportunity'']] rover,<ref name="spirit contact conclusion2"/> and Mars rover ''[[Curiosity (rover)|Curiosity]]'' which is exploring Gale Crater and has been doing so for more than six years.<ref>{{Cite web|title=NASA's Opportunity Rover Mission on Mars Comes to End|url=https://mars.nasa.gov/news/8413/nasas-opportunity-rover-mission-on-mars-comes-to-end|last=mars.nasa.gov|website=NASA’s Mars Exploration Program|language=en|access-date=May 23, 2020}}</ref>


The science instruments included:<ref>{{cite web |title=The Rover's "Eyes" and Other "Senses" - NASA |url=https://mars.nasa.gov/mer/mission/rover/eyes-and-senses/ |website=mars.nasa.gov |access-date=23 April 2023}}</ref>
==Discoveries==
The 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 (geologists would say they have vesicles and vugs).<ref name="McSween2004">{{cite journal | last1 = McSween | first1 = HY| year = 2004 | title = Basaltic Rocks Analyzed by the Spirit Rover in Gusev Crater | journal = Science | volume = 305 | issue = 5685| pages = 842–845 | doi = 10.1126/science.3050842 | pmid = 15297668 | last2 = Arvidson | first2 = RE | last3 = Bell Jf | first3 = 3rd | last4 = Blaney | first4 = D | last5 = Cabrol | first5 = NA | last6 = Christensen | first6 = PR | last7 = Clark | first7 = BC | last8 = Crisp | first8 = JA | last9 = Crumpler | first9 = LS | display-authors=8 | bibcode = 2004Sci...305..842M}}</ref><ref name="Arvidson2004">{{cite journal | last1 = Arvidson | first1 = R. E. | year = 2004 | title = Localization and physical properties experiments conducted by Spirit at Gusev Crater| journal = Science | volume = 305 | issue = 5685| pages = 821–824 | doi = 10.1126/science.1099922 | pmid = 15297662 | last2 = Anderson | first2 = RC | last3 = Bartlett | first3 = P | last4 = Bell Jf | first4 = 3rd | last5 = Blaney | first5 = D | last6 = Christensen | first6 = PR | last7 = Chu | first7 = P | last8 = Crumpler | first8 = L | last9 = Davis | first9 = K | display-authors=8 |bibcode = 2004Sci...305..821A | s2cid = 31102951 }}</ref>
{{Wide image|PIA01907 fig1-MarsSpirit-200604c.jpg |1100px|Annotated panorama of rocks near ''Spirit'' (April, 2006).}}
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]].<ref>{{cite journal | doi = 10.1029/2005JE002555 | title = Alpha Particle X-Ray Spectrometer (APXS): Results from Gusev crater and calibration report | year = 2006 | last1 = Gellert | first1 = R. | last2 = Rieder | first2 = R. | last3 = Brückner | first3 = J. | last4 = Clark | first4 = B. C. | last5 = Dreibus | first5 = G. | last6 = Klingelhöfer | first6 = G. | last7 = Lugmair | first7 = G. | last8 = Ming | first8 = D. W. | last9 = Wänke | first9 = H. | display-authors=8 | journal = Journal of Geophysical Research | volume = 111 | issue = E2 | pages = n/a | bibcode=2006JGRE..111.2S05G| hdl = 2060/20080026124 | s2cid = 129432577 | hdl-access = free }}</ref>


* [[Pancam|Panoramic Camera (Pancam)]] – examined the texture, color, mineralogy, and structure of the local terrain.
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).<ref>{{cite journal | last1 = Christensen | first1 = P. | year = 2004| title = Initial Results from the Mini-TES Experiment in Gusev Crater from the Spirit Rover | journal = Science | volume = 305 | issue = 5685| pages = 837–842 | doi = 10.1126/science.1100564 | pmid = 15297667 | last2 = Ruff | first2 = SW | last3 = Fergason | first3 = RL | last4 = Knudson | first4 = AT | last5 = Anwar | first5 = S | last6 = Arvidson | first6 = RE | last7 = Bandfield | first7 = JL | last8 = Blaney | first8 = DL | last9 = Budney | first9 = C | display-authors=8 |bibcode = 2004Sci...305..837C | s2cid = 34983664 }}</ref>
* [[Navcam|Navigation Camera (Navcam)]] – monochrome with a higher field of view but lower resolution, for navigation and driving.
* [[Mini-TES|Miniature Thermal Emission Spectrometer (Mini-TES)]] – identified promising rocks and soils for closer examination, and determined the processes that formed them.
* [[Hazcam]]s, two B&W cameras with 120 degree field of view, that provided additional data about the rover's surroundings.


The rover arm held the following instruments:<ref>{{cite web |title=The Rover's "Arm" - NASA |url=https://mars.nasa.gov/mer/mission/rover/arm/ |website=mars.nasa.gov |access-date=23 April 2023}}</ref>
There are a variety of rocks in the [[Columbia Hills (Mars)|Columbia Hills]], some of which have been altered by water, but not by very much water.


* [[Mössbauer spectrometer]] (MB) [[MIMOS II]] – used for close-up investigations of the mineralogy of iron-bearing rocks and soils.
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.<ref>{{cite journal | last1 = Bertelsen | first1 = P. | year = 2004 | title = Magnetic Properties on the Mars Exploration Rover Spirit at Gusev Crater | journal = Science | volume = 305 | issue = 5685| pages = 827–829 | doi = 10.1126/science.1100112 | pmid = 15297664 | last2 = Goetz | first2 = W | last3 = Madsen | first3 = MB | last4 = Kinch | first4 = KM | last5 = Hviid | first5 = SF | last6 = Knudsen | first6 = JM | last7 = Gunnlaugsson | first7 = HP | last8 = Merrison | first8 = J | last9 = Nørnberg | first9 = P | display-authors=8 |bibcode = 2004Sci...305..827B | s2cid = 41811443 }}</ref> 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.<ref name="Bell">Bell, J (ed.) The Martian Surface. 2008. Cambridge University Press. {{ISBN|978-0-521-86698-9}}</ref><ref>{{cite journal | last1 = Gelbert | first1 = R. | year = 2004| title = Chemistry of Rocks and Soils in Gusev Crater from the Alpha Particle X-ray Spectrometer | journal = Science | volume = 305 | issue = 5685| pages = 829–832 |doi=10.1126/science.1099913 |bibcode = 2004Sci...305..829G | pmid=15297665| s2cid = 30195269 }}</ref>
* [[Alpha particle X-ray spectrometer]] (APXS) – close-up analysis of the abundances of elements that make up rocks and soils.
* Magnets – for collecting magnetic dust particles.
* Microscopic Imager (MI) – obtained close-up, high-resolution images of rocks and soils.
* [[Rock Abrasion Tool]] (RAT) – exposed fresh material for examination by instruments on board.


''Spirit'' was 'driven' by several operators throughout its mission.<ref name="sm2019">{{cite web |last1=Venkatraman |first1=Vijaysree |title=The space roboticist |url=https://www.science.org/content/article/space-roboticist |website=Science magazine |date=July 13, 2015 |access-date=February 14, 2019}}</ref>
===Plains===
{{Infobox feature on celestial object
|name = Adirondack
|image = [[File:Adirondacksquare.jpg|{{#expr: (200 * (316 / 196)) round 0}}px]] [[File:Rat post grind.jpg|right|{{#expr: (200 * (505 / 494)) round 0}}px]]
|caption = '''Above''': An [[24-bit color|approximate true-color]] view of Adirondack, taken by ''Spirit''{{'}}s pancam. (January 19, 2004)<br />'''Right''':Digital camera image (from ''Spirit''{{'}}s [[Pancam]]) of Adirondack after a [[Rock Abrasion Tool]] grind (February 6, 2004)
|type = Rock
|coordinates = {{coord|14.6|S|175.5|E|globe:mars_type:landmark|display=inline,title}}
}}


===Power===
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]].
{{main|Mars Exploration Rover#Power and electronic systems}}


The rover uses a combination of solar cells and a rechargeable chemical battery.<ref name="mars.nasa.gov">{{cite web|url=http://mars.nasa.gov/mer/technology/bb_power.html|title=Mars Exploration Rover Mission: Technology|work=nasa.gov|access-date=January 5, 2017|archive-url=https://web.archive.org/web/20161228213007/http://mars.nasa.gov/mer/technology/bb_power.html|archive-date=December 28, 2016|url-status=live}}</ref> This class of rover has two rechargeable [[Lithium battery|lithium batteries]], each composed of 8 cells with 8 [[Ampere hour|amp-hour]] capacity.<ref>{{cite web |url=https://mars.nasa.gov/mer/technology/bb_power.html |title=Power |access-date=September 20, 2018 |archive-url=https://web.archive.org/web/20170118021407/http://mars.nasa.gov/mer/technology/bb_power.html |archive-date=January 18, 2017 |url-status=live }}</ref> At the start of the mission the solar panels could provide up to around 900 watt-hours (Wh) per day to recharge the battery and power system in one Sol, but this could vary due to a variety of factors.<ref name="mars.nasa.gov"/> In [[Eagle crater]] the cells were producing about 840 Wh per day, but by Sol 319 in December 2004, it had dropped to 730 Wh per day.<ref>{{cite web|url=http://mars.nasa.gov/mer/mission/status_opportunityAll_2004.html#sol11|title=Mars Exploration Rover Mission: All Opportunity Updates|work=nasa.gov|access-date=January 5, 2017|archive-url=https://web.archive.org/web/20170201175441/http://mars.nasa.gov/mer/mission/status_opportunityAll_2004.html#sol11|archive-date=February 1, 2017|url-status=live}}</ref>
Rocks of the plains also resemble the basaltic [[shergottite]]s, meteorites that 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 [[tephrite]]. The Irvine-Barager classification calls them basalts.<ref name="McSween2004" />
Plains 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).<ref name="McSween2004" /><ref name="Arvidson2004" />
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.
<gallery widths="600px" heights="250px">
Image:Rockgusev.jpg|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 minerals are visible, along with crystals of [[olivine]]. Veins may contain bromine salts.
</gallery>


Like Earth, Mars has seasonal variations that reduce sunlight during winter. However, since the Martian year is longer than that of the Earth, the seasons fully rotate roughly once every 2 Earth years.<ref name="ReferenceA">{{cite web|url=http://mars.nasa.gov/news/whatsnew/index.cfm?FuseAction=ShowNews&NewsID=1885|title=Mars Rover Opportunity Busy Through Depth of Winter – Mars News|last=mars.nasa.gov|work=nasa.gov|access-date=January 5, 2017|archive-url=https://web.archive.org/web/20160726141458/http://mars.nasa.gov/news/whatsnew/index.cfm?FuseAction=ShowNews&NewsID=1885|archive-date=July 26, 2016|url-status=live}}</ref> By 2016, MER-B had endured seven Martian winters, during which times power levels drop which can mean the rover avoids doing activities that use a lot of power.<ref name="ReferenceA"/> During its first winter power levels dropped to under 300 Wh per day for two months, but some later winters were not as bad.<ref name="ReferenceA"/>
===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.<ref>{{cite journal | doi = 10.1029/2005JE002562 | title = Rocks of the Columbia Hills | year = 2006 | last1 = Squyres | first1 = Steven W. | last2 = Arvidson | first2 = Raymond E. | last3 = Blaney | first3 = Diana L. | last4 = Clark | first4 = Benton C. | last5 = Crumpler | first5 = Larry | last6 = Farrand | first6 = William H. | last7 = Gorevan | first7 = Stephen | last8 = Herkenhoff | first8 = Kenneth E. | last9 = Hurowitz | first9 = Joel | display-authors=8 | journal = Journal of Geophysical Research | volume = 111 | issue = E2 | pages = n/a | bibcode=2006JGRE..111.2S11S}}</ref> Most importantly, all of the rocks in Columbia Hills show various degrees of alteration due to aqueous fluids.<ref name="Ming2005JE002560">{{cite journal | doi = 10.1029/2005JE002560 | title = Geochemical and mineralogical indicators for aqueous processes in the Columbia Hills of Gusev crater, Mars | year = 2006 | last1 = Ming | first1 = D. W. | last2 = Mittlefehldt | first2 = D. W. | last3 = Morris | first3 = R. V. | last4 = Golden | first4 = D. C. | last5 = Gellert | first5 = R. | last6 = Yen | first6 = A. | last7 = Clark | first7 = B. C. | last8 = Squyres | first8 = S. W. | last9 = Farrand | first9 = W. H. | display-authors=8 | journal = Journal of Geophysical Research | volume = 111 | issue = E2 | pages = n/a | bibcode=2006JGRE..111.2S12M| hdl = 1893/17114 | hdl-access = free }}</ref>
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 [[sulfate]]s.<ref name="Schroder2005" /><ref>Christensen, P.R. (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, May 23–27, 2005 http://www.agu.org/meetings/sm05/waissm05.html {{Webarchive|url=https://web.archive.org/web/20130513050221/http://www.agu.org/meetings/sm05/waissm05.html |date=May 13, 2013 }}</ref>
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.


Another factor that can reduce received power is dust in the atmosphere, especially dust storms.<ref name="phys.org">{{cite web|url=http://phys.org/news/2016-10-europe-exomars-mission-middle-season.html|title=Europe's ExoMars mission arrives in the middle of dust season|work=phys.org|access-date=January 5, 2017|archive-url=https://web.archive.org/web/20161130091828/http://phys.org/news/2016-10-europe-exomars-mission-middle-season.html|archive-date=November 30, 2016|url-status=live}}</ref> Dust storms have occurred quite frequently when Mars is closest to the Sun.<ref name="phys.org"/> Global dust storms in 2007 reduced power levels for ''Opportunity'' and ''Spirit'' so much they could only run for a few minutes each day.<ref name="phys.org"/> Due to the [[Opportunity mission timeline#Dust storm|2018 dust storms]] on Mars, ''Opportunity'' entered [[Safe mode (spacecraft)|hibernation mode]] on June 12,<ref>[https://www.theverge.com/2018/6/13/17460314/nasa-opportunity-rover-mars-dust-storm-battery-drained NASA's Opportunity rover is in a deep sleep on Mars – but there's hope it will wake up again] {{Webarchive|url=https://web.archive.org/web/20180614021406/https://www.theverge.com/2018/6/13/17460314/nasa-opportunity-rover-mars-dust-storm-battery-drained |date=June 14, 2018 }}. Loren Grush, ''The Verge''. June 13, 2018.</ref><ref>{{Cite news|url=https://www.scientificamerican.com/article/as-massive-storm-rages-on-mars-opportunity-rover-falls-silent/|title=As Massive Storm Rages on Mars, Opportunity Rover Falls Silent|last=Malik|first=Tariq|work=Scientific American (Space.com)|access-date=June 13, 2018|language=en|archive-url=https://web.archive.org/web/20180613180214/https://www.scientificamerican.com/article/as-massive-storm-rages-on-mars-opportunity-rover-falls-silent/|archive-date=June 13, 2018|url-status=live}}</ref> but it remained silent after the storm subsided in early October.<ref name="Official updates">{{cite web|url=https://mars.nasa.gov/mer/mission/status_opportunityAll.html|title=Mars Exploration Rover Mission: All Opportunity Updates|website=mars.nasa.gov|access-date=February 10, 2018|archive-url=https://web.archive.org/web/20180325061258/https://mars.nasa.gov/mer/mission/status_opportunityAll.html|archive-date=March 25, 2018|url-status=live}}</ref>
Acid fog is believed to have changed some of the Watchtower rocks. This was in a {{convert|200|m|ft}} long section of Cumberland Ridge and the Husband Hill summit. Certain places became less crystalline and more amorphous. Acidic water vapor from volcanoes dissolved some minerals forming a gel. When water evaporated a cement formed and produced small bumps. This type of process has been observed in the lab when basalt rocks are exposed to sulfuric and hydrochloric acids.<ref>{{cite web|url=http://spaceref.com/mars/signs-of-acid-fog-found-on-mars.html|title=Signs of Acid Fog Found on Mars – SpaceRef|website=spaceref.com}}</ref><ref>{{cite web|url=https://gsa.confex.com/gsa/2015AM/webprogram/Paper266774.html|title=Abstract: In-situ Evidence for Alteration by Acid Fog on Husband Hill, Gusev Crater, Mars. (2015 GSA Annual Meeting in Baltimore, Maryland, USA (1–4 November 2015))|website=gsa.confex.com}}</ref><ref>COLE, Shoshanna B., et al. 2015. In-situ Evidence for Alteration by Acid Fog on Husband Hill, Gusev Crater, Mars. 2015 GSA Annual Meeting in Baltimore, Maryland, USA (November 1–4, 2015) Paper No. 94-10</ref>


==Discoveries==
The Clovis group is especially interesting because the [[Mössbauer spectrometer]] (MB) detected [[goethite]] in it.<ref>Klingelhofer, G., et al. (2005) Lunar Planet. Sci. XXXVI abstr. 2349</ref> 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,<ref name="Schroder2005">{{cite journal | last1 = Schroder | first1 = C. | year = 2005 | title = European Geosciences Union, General Assembly | journal = Geophysical Research Abstracts | volume = 7 | page = 10254 }}</ref>
although the rocks probably once contained much olivine.<ref>{{cite journal | doi = 10.1029/2005JE002584 | title = Mössbauer mineralogy of rock, soil, and dust at Gusev crater, Mars: Spirit's journey through weakly altered olivine basalt on the plains and pervasively altered basalt in the Columbia Hills | year = 2006 | last1 = Morris | first1 = R. V. | last2 = Klingelhöfer | first2 = G. | last3 = Schröder | first3 = C. | last4 = Rodionov | first4 = D. S. | last5 = Yen | first5 = A. | last6 = Ming | first6 = D. W. | last7 = De Souza | first7 = P. A. | last8 = Fleischer | first8 = I. | last9 = Wdowiak | first9 = T. | display-authors=8 | journal = Journal of Geophysical Research | volume = 111 | issue = E2 | pages = n/a | bibcode=2006JGRE..111.2S13M| hdl = 1893/17159 | hdl-access = free }}</ref> 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.
The 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 (geologists would say they have vesicles and vugs).<ref name="McSween2004">{{cite journal | last1 = McSween | first1 = HY| year = 2004 | title = Basaltic Rocks Analyzed by the Spirit Rover in Gusev Crater | journal = Science | volume = 305 | issue = 5685| pages = 842–845 | doi = 10.1126/science.3050842 | pmid = 15297668 | last2 = Arvidson | first2 = RE | last3 = Bell Jf | first3 = 3rd | last4 = Blaney | first4 = D | author4-link= Diana Blaney | last5 = Cabrol | first5 = NA | last6 = Christensen | first6 = PR | last7 = Clark | first7 = BC | last8 = Crisp | first8 = JA | last9 = Crumpler | first9 = LS | display-authors=8 | bibcode = 2004Sci...305..842M}}</ref><ref name="Arvidson2004">{{cite journal | last1 = Arvidson | first1 = R. E. | year = 2004 | title = Localization and physical properties experiments conducted by Spirit at Gusev Crater| journal = Science | volume = 305 | issue = 5685| pages = 821–824 | doi = 10.1126/science.1099922 | pmid = 15297662 | last2 = Anderson | first2 = RC | last3 = Bartlett | first3 = P | last4 = Bell Jf | first4 = 3rd | last5 = Blaney | first5 = D |author5-link= Diana Blaney | last6 = Christensen | first6 = PR | last7 = Chu | first7 = P | last8 = Crumpler | first8 = L | last9 = Davis | first9 = K | display-authors=8 |bibcode = 2004Sci...305..821A | s2cid = 31102951 }}</ref>
{{Wide image|PIA01907 fig1-MarsSpirit-200604c.jpg|1100px|Annotated panorama of rocks near ''Spirit'' (April, 2006)}}
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.
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]].<ref>{{cite journal | doi = 10.1029/2005JE002555 | title = Alpha Particle X-Ray Spectrometer (APXS): Results from Gusev crater and calibration report | year = 2006 | last1 = Gellert | first1 = R. | last2 = Rieder | first2 = R. | last3 = Brückner | first3 = J. | last4 = Clark | first4 = B. C. | last5 = Dreibus | first5 = G. | last6 = Klingelhöfer | first6 = G. | last7 = Lugmair | first7 = G. | last8 = Ming | first8 = D. W. | last9 = Wänke | first9 = H. | display-authors=8 | journal = Journal of Geophysical Research | volume = 111 | issue = E2 | pages = n/a | bibcode=2006JGRE..111.2S05G| hdl = 2060/20080026124 | s2cid = 129432577 | hdl-access = free }}</ref>
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.<ref name="Ming2005JE002560" />
Also, MB found that much of the iron in Paso Robles soil was of the oxidized, Fe<sup>3+</sup> form, which would happen if water had been present.<ref name="Bell" />


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).<ref>{{cite journal | last1 = Christensen | first1 = P. | year = 2004| title = Initial Results from the Mini-TES Experiment in Gusev Crater from the Spirit Rover | journal = Science | volume = 305 | issue = 5685| pages = 837–842 | doi = 10.1126/science.1100564 | pmid = 15297667 | last2 = Ruff | first2 = SW | last3 = Fergason | first3 = RL | last4 = Knudson | first4 = AT | last5 = Anwar | first5 = S | last6 = Arvidson | first6 = RE | last7 = Bandfield | first7 = JL | last8 = Blaney | first8 = DL |author8-link= Diana Blaney | last9 = Budney | first9 = C | display-authors=8 |bibcode = 2004Sci...305..837C | s2cid = 34983664 }}</ref>
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.<ref name="Sky & Telescope">{{cite web|url=http://www.skyandtelescope.com/news/19177609.html|title=Mars Rover Uncovers Ancient Hot Springs|publisher=SkyandTelescope.com|date=May 22, 2008|access-date=August 1, 2012}}</ref> 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.<ref>{{cite web|url=http://www.nasa.gov/mission_pages/mer/mer-20070521.html|title=NASA – Mars Rover Spirit Unearths Surprise Evidence of Wetter Past|website=www.nasa.gov}}</ref>


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."<ref>{{cite web|url=https://www.sciencedaily.com/releases/2010/06/100603140959.htm|title=Outcrop of long-sought rare rock on Mars found}}</ref><ref>{{cite journal | doi = 10.1126/science.1189667 | title = Identification of Carbonate-Rich Outcrops on Mars by the Spirit Rover | year = 2010 | last1 = Morris | first1 = R. V. | last2 = Ruff | first2 = S. W. | last3 = Gellert | first3 = R. | last4 = Ming | first4 = D. W. | last5 = Arvidson | first5 = R. E. | last6 = Clark | first6 = B. C. | last7 = Golden | first7 = D. C. | last8 = Siebach | first8 = K. | last9 = Klingelhofer | first9 = G. | display-authors=8 | journal = Science | volume = 329 | issue = 5990 | pages = 421–4 | pmid = 20522738 |bibcode = 2010Sci...329..421M | s2cid = 7461676 }}</ref>
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.<ref>{{cite journal | last1 = Bertelsen | first1 = P. | year = 2004 | title = Magnetic Properties on the Mars Exploration Rover Spirit at Gusev Crater | journal = Science | volume = 305 | issue = 5685| pages = 827–829 | doi = 10.1126/science.1100112 | pmid = 15297664 | last2 = Goetz | first2 = W | last3 = Madsen | first3 = MB | last4 = Kinch | first4 = KM | last5 = Hviid | first5 = SF | last6 = Knudsen | first6 = JM | last7 = Gunnlaugsson | first7 = HP | last8 = Merrison | first8 = J | last9 = Nørnberg | first9 = P | display-authors=8 |bibcode = 2004Sci...305..827B | s2cid = 41811443 }}</ref> 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.<ref name="Bell">Bell, J (ed.) The Martian Surface. 2008. Cambridge University Press. {{ISBN|978-0-521-86698-9}}</ref><ref>{{cite journal | last1 = Gelbert | first1 = R. | year = 2004| title = Chemistry of Rocks and Soils in Gusev Crater from the Alpha Particle X-ray Spectrometer | journal = Science | volume = 305 | issue = 5685| pages = 829–832 |doi=10.1126/science.1099913 |bibcode = 2004Sci...305..829G | pmid=15297665| s2cid = 30195269 }}</ref>

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 that 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 that 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.


==Astronomy==
==Astronomy==
{{see also|Astronomy on Mars}}
{{see also|Astronomy on Mars}}
{{multiple image
{{multiple image
| align = right
| align = right
| image1 = PIA05547-Spirit Rover-Earth seen from Mars.png
| image1 = PIA05547-Spirit Rover-Earth seen from Mars.png
| width1 = {{#expr: (200 * (1194 / 1007)) round 0}}
| width1 = {{#expr: (200 * (1194 / 1007)) round 0}}
| alt1 =
| alt1 =
| caption1 = [[Earth]] from Mars
| caption1 = [[Earth]] from Mars
| image2 = Phobos & Deimos full thumb.png
| image2 = Phobos & Deimos full thumb.png
| width2 = {{#expr: (200 * (200 / 213)) round 0}}
| width2 = {{#expr: (200 * (200 / 213)) round 0}}
| alt2 =
| alt2 =
| caption2 = Night sky of Mars showing [[Deimos (moon)|Deimos]] (left) and [[Phobos (moon)|Phobos]] (right) in front of [[Sagittarius (constellation)|Sagittarius]], as seen by [[Mars Exploration Rover]] ''Spirit'' on August 26, 2005. For full animation see [[:Image:Phobos & Deimos full.gif]]
| caption2 = Night sky of Mars showing [[Deimos (moon)|Deimos]] (left) and [[Phobos (moon)|Phobos]] (right) in front of [[Sagittarius (constellation)|Sagittarius]], as seen by [[Mars Exploration Rover]] ''Spirit'' on August 26, 2005. For full animation, see [[:Image:Phobos & Deimos full.gif]].
| footer =
| footer =
}}
}}
''Spirit'' pointed its cameras towards the sky and observed a [[astronomical transit|transit]] of the [[Sun]] by Mars' [[natural satellite|moon]] [[Deimos (moon)|Deimos]] (see [[Transit of Deimos from Mars]]). It also took the [[First photos of Earth from space|first photo of Earth from the surface of another planet]] in early March 2004.
''Spirit'' pointed its cameras towards the sky and observed a [[astronomical transit|transit]] of the [[Sun]] by Mars' [[natural satellite|moon]] [[Deimos (moon)|Deimos]] (see [[Transit of Deimos from Mars]]). It also took the [[First photos of Earth from space|first photo of Earth from the surface of another planet]] in early March 2004.
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Scientific instruments also experienced degradation as a result of exposure to the harsh Martian environment and use over a far longer period than had been anticipated by the mission planners. Over time, the diamond in the resin grinding surface of the [[Rock Abrasion Tool]] wore down, after that the device could only be used to brush targets.<ref>{{cite web|url=http://www.news.cornell.edu/releases/rover/Roverextension.html|title=NASAʼs Mars rovers and Steve Squyres keep going and going – Cornell Chronicle|website=www.news.cornell.edu}}</ref> All of the other science instruments and engineering cameras continued to function until contact was lost; however, towards the end of ''Spirit'''s life, the [[MIMOS II]] [[Mössbauer spectrometer]] took much longer to produce results than it did earlier in the mission because of the decay of its [[cobalt]]-57 gamma ray source that has a half life of 271 days.
Scientific instruments also experienced degradation as a result of exposure to the harsh Martian environment and use over a far longer period than had been anticipated by the mission planners. Over time, the diamond in the resin grinding surface of the [[Rock Abrasion Tool]] wore down, after that the device could only be used to brush targets.<ref>{{cite web|url=http://www.news.cornell.edu/releases/rover/Roverextension.html|title=NASAʼs Mars rovers and Steve Squyres keep going and going – Cornell Chronicle|website=www.news.cornell.edu}}</ref> All of the other science instruments and engineering cameras continued to function until contact was lost; however, towards the end of ''Spirit'''s life, the [[MIMOS II]] [[Mössbauer spectrometer]] took much longer to produce results than it did earlier in the mission because of the decay of its [[cobalt]]-57 gamma ray source that has a half life of 271 days.


== Legacy and honors ==
==Honors==
[[File:MarsSunsetCut.jpg|thumb|right|Martian sunset in 2005 by ''Spirit'']]


===To rover===
To commemorate ''Spirit'''s great contribution to the [[exploration of Mars]], the [[asteroid]] [[37452 Spirit]] has been named after it.<ref>{{cite web|url=http://marsrovers.nasa.gov/spotlight/20041011.html|title=Mars Exploration Rover Mission: Spotlight|website=marsrovers.nasa.gov|access-date=June 30, 2006|archive-url=https://web.archive.org/web/20080511042036/http://marsrovers.nasa.gov/spotlight/20041011.html|archive-date=May 11, 2008|url-status=dead}}</ref> The name was proposed by [[Ingrid van Houten-Groeneveld]] who along with [[Cornelis Johannes van Houten]] and [[Tom Gehrels]] discovered the asteroid on September 24, 1960.
To commemorate ''Spirit'''s great contribution to the [[exploration of Mars]], the [[asteroid]] [[37452 Spirit]] has been named after it.<ref>{{cite web|url=http://marsrovers.nasa.gov/spotlight/20041011.html|title=Mars Exploration Rover Mission: Spotlight|website=marsrovers.nasa.gov|access-date=June 30, 2006|archive-url=https://web.archive.org/web/20080511042036/http://marsrovers.nasa.gov/spotlight/20041011.html|archive-date=May 11, 2008|url-status=dead}}</ref> The name was proposed by [[Ingrid van Houten-Groeneveld]] who along with [[Cornelis Johannes van Houten]] and [[Tom Gehrels]] discovered the asteroid on September 24, 1960.

[[Reuben H. Fleet Science Center]] and the [[Liberty Science Center]] also have an IMAX show called ''Roving Mars'' that documents the journey of both ''Spirit'' and ''Opportunity'', using both CG and actual imagery.

January 4, 2014, was celebrated as the tenth anniversary of its landing on many news sites, despite nearly four years since loss of communications.<ref name=spacef>{{cite web|url=http://www.spaceflightnow.com/news/n1401/03spirit/#.Usha7iddhCo|title=Spaceflight Now – Mars Exploration Rovers – Revered Spirit rover landed on Mars a decade ago|website=www.spaceflightnow.com}}</ref>


To honor the rover, the JPL team named an area near [[Endeavour (crater)|Endeavour Crater]] explored by the [[Opportunity (rover)|''Opportunity'' rover]], 'Spirit Point'.<ref name="NASA-20110810">{{cite web |last1=Greicius |first1=Tony |last2=Dunbar |first2=Brian |title=Arrival at 'Spirit Point' by Mars Rover Opportunity |url=http://www.nasa.gov/mission_pages/mer/multimedia/gallery/pia14509.html |date=August 10, 2011 |work=[[NASA]] |access-date=February 2, 2014 }}</ref>
To honor the rover, the JPL team named an area near [[Endeavour (crater)|Endeavour Crater]] explored by the [[Opportunity (rover)|''Opportunity'' rover]], 'Spirit Point'.<ref name="NASA-20110810">{{cite web |last1=Greicius |first1=Tony |last2=Dunbar |first2=Brian |title=Arrival at 'Spirit Point' by Mars Rover Opportunity |url=http://www.nasa.gov/mission_pages/mer/multimedia/gallery/pia14509.html |date=August 10, 2011 |work=[[NASA]] |access-date=February 2, 2014 }}</ref>


[[Documentary]] film, ''[[Good Night Oppy]]'', about the ''Opportunity'', ''Spirit'', and their long missions, was directed by [[Ryan White (filmmaker)|Ryan White]], and included support from JPL and [[Industrial Light & Magic]]. It was released in 2022.<ref>{{cite web |last1=Ross |first1=Rollo |title='Good Night Oppy' about NASA's rover mission may make you cry |url=https://www.reuters.com/lifestyle/science/good-night-oppy-about-nasas-rover-mission-may-make-you-cry-2022-11-22/ |website=Reuters |access-date=23 April 2023 |language=en |date=22 November 2022}}</ref>
===From rover===
On January 27, 2004 (sol {{age in sols|2004|01|04|2004|01|27}}) NASA memorialized the crew of [[Apollo 1]] by naming three hills to the north of "''Columbia'' Memorial Station" as the [[Apollo 1 Hills]]. On February 2, 2004 (sol {{age in sols|2004|01|04|2004|02|02}}) the astronauts on Space Shuttle ''Columbia''{{'}}s [[STS-107|final mission]] were further memorialized when NASA named a set of hills to the east of the landing site the [[Columbia Hills (Mars)|Columbia Hills Complex]], denoting seven peaks in that area as "Anderson", "Brown", "Chawla", "Clark", "Husband", "McCool", and "Ramon" in honour of the crew; NASA has submitted these geographical feature names to the [[International Astronomical Union|IAU]] for approval.


==Gallery==
==Gallery==
The rover could take pictures with its different cameras, but only the PanCam camera had the ability to photograph a scene with different color filters. The panorama views were usually built up from PanCam images. ''Spirit'' transferred 128,224 pictures in its lifetime.<ref>{{cite web|url=http://marsrovers.jpl.nasa.gov/gallery/all/spirit.html|title=Mars Exploration Rover|last=mars.nasa.gov|website=marsrovers.jpl.nasa.gov}}</ref>
The rover could take pictures with its different cameras, but only the PanCam camera had the ability to photograph a scene with different color filters. The panorama views were usually built up from PanCam images. ''Spirit'' transferred 128,224 pictures in its lifetime.<ref>{{cite web|url=http://marsrovers.jpl.nasa.gov/gallery/all/spirit.html|title=Mars Exploration Rover|last=mars.nasa.gov|website=marsrovers.jpl.nasa.gov}}</ref>


=== Views ===
<gallery>
File:Bonneville Crater look back.jpg|Looking back from Bonneville crater to the landing site
File:Mars rock Mimi by Spirit rover.jpg|[[False color]] image of "Mimi".
</gallery>

=== Panoramas ===
{{Wide image|missoula spirit.jpg|800px|Missoula Crater (Sol 105, April 19, 2004)}}
{{Wide image|missoula spirit.jpg|800px|Missoula Crater (Sol 105, April 19, 2004)}}
{{Wide image|Lahontan Crater.jpg|800px|Lahontan crater on sol 120}}
{{Wide Image|Spirit Lookout L256t-A413R1 br2.jpg|800px|Color panorama taken from "Larry's Lookout". On the far left is "Tennessee Valley" and on the right, rover tracks.}}
{{Wide Image|Spirit Lookout L256t-A413R1 br2.jpg|800px|Color panorama taken from "Larry's Lookout". On the far left is "Tennessee Valley" and on the right, rover tracks.}}
{{Wide image|Main Apollo Hills.jpg|800px|Annotated Apollo Hills panorama from the ''Spirit'' landing site}}
{{Wide image|Main Apollo Hills.jpg|800px|Annotated Apollo Hills panorama from the ''Spirit'' landing site}}
{{Wide image|PIA10214.jpg|800px|''Spirit'''s West Valley panorama (color not rectificated for media). NASA'S Mars Exploration Rover ''Spirit'' captured this westward view from atop a low plateau where ''Spirit'' spent the closing months of 2007.}}

=== Microscopic images ===
<gallery>
File:Spirit Rat Mazatzal.jpg|Close-up of the rock ''Mazatzal'', which was ground with the Rock Abrasion Tool on sol 82
File:GongGong.jpg|Erosive effect of winds on hardened lava.
</gallery>

=== From orbit ===
<gallery>
File:Spirit tracks.gif|Rover tracks up to sol 85 from ''[[Mars Global Surveyor]]''
File:Spirit MRO.jpg|''Spirit'' on September 29, 2006, beside Home Plate <ref>{{cite web|url=http://photojournal.jpl.nasa.gov/catalog/PIA01879|title=Catalog Page for PIA01879|website=photojournal.jpl.nasa.gov}}</ref>
</gallery>

=== Maps ===
[[File:SpiritTraverseMap.jpg|thumb|center|500px|{{center|Map of the movement of the ''Spirit'' rover,<br>from January 2004 landing thru to April 2008.<br>(see image above, at [[#Mars winter at Troy]], for remaining movement)}}]]
{{Features and artificial objects on Mars}}


==See also==
==See also==
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* [[Viking program]]
* [[Viking program]]
* [[List of software bugs#Space|List of software bugs related to space exploration]]
* [[List of software bugs#Space|List of software bugs related to space exploration]]
* [[Comparison of embedded computer systems on board the Mars rovers]]
* [[Zhurong (rover)|''Zhurong'' (rover)]]
* [[Zhurong (rover)|''Zhurong'' (rover)]]
}}
}}
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==References==
==References==
{{reflist|30em}}
{{Reflist}}


==External links==
==External links==
{{commons|Mars Exploration Rover}}
{{Commons|Mars Exploration Rover}}


=== JPL, MSSS, and NASA links ===
=== JPL, MSSS, and NASA links ===
* [http://marsrovers.jpl.nasa.gov/home/index.html JPL's Mars Exploration Rover Mission home page]
* [http://marsrovers.jpl.nasa.gov/home/index.html JPL's Mars Exploration Rover Mission home page]
* [http://www.jpl.nasa.gov/missions/mer/daily.cfm (obsolete JPL Mars Exploration Rover home page)]
* [http://www.jpl.nasa.gov/missions/mer/daily.cfm (obsolete JPL Mars Exploration Rover home page)] {{Webarchive|url=https://web.archive.org/web/20080713085838/http://www.jpl.nasa.gov/missions/mer/daily.cfm |date=July 13, 2008 }}
* [https://web.archive.org/web/20031216084933/http://www.solarsystem.nasa.gov/missions/profile.cfm?MCode=MER_A ''Spirit'' Mission Profile] by [http://solarsystem.nasa.gov NASA's Solar System Exploration]
* [http://photojournal.jpl.nasa.gov/spacecraft/Spirit Planetary Photojournal], NASA JPL's Planetary Photojournal for ''Spirit''
* [http://photojournal.jpl.nasa.gov/spacecraft/Spirit Planetary Photojournal], NASA JPL's Planetary Photojournal for ''Spirit''
* [http://www.nasa.gov/multimedia/nasatv/MM_NTV_Breaking.html NASA TV Special Events Schedule] for MER News Briefings at JPL
* [http://www.nasa.gov/multimedia/nasatv/MM_NTV_Breaking.html NASA TV Special Events Schedule] {{Webarchive|url=https://web.archive.org/web/20141221085634/http://www.nasa.gov/multimedia/nasatv/MM_NTV_Breaking.html |date=December 21, 2014 }} for MER News Briefings at JPL
* [http://www.jpl.nasa.gov/mer2004/mission-status/index.html Mission Status updates from NASA JPL]
* [http://www.jpl.nasa.gov/mer2004/mission-status/index.html Mission Status updates from NASA JPL] {{Webarchive|url=https://web.archive.org/web/20041204055044/http://www.jpl.nasa.gov/mer2004/mission-status/index.html |date=December 4, 2004 }}
* [[s:NASA MER press briefings|Wikisource:NASA MER press briefings]]
* [[s:NASA MER press briefings|Wikisource:NASA MER press briefings]]
* [https://web.archive.org/web/20080509150241/http://www.msss.com/mars_images/moc/2004/01/23/ Finding ''Spirit'': high resolution images of landing site (''Mars Global Surveyor'' – Mars Orbiter Camera)]
* [https://web.archive.org/web/20141129050447/http://www.jpl.nasa.gov/freespirit/ JPL's site devoted to the efforts to free ''Spirit'']
* [http://pds-geosciences.wustl.edu/meran MER Analyst's Notebook], Interactive access to mission data and documentation
* [http://pds-geosciences.wustl.edu/meran MER Analyst's Notebook], Interactive access to mission data and documentation


===Other links===
===Other links===
* [http://spaceflightnow.com/mars/mera/status.html SpaceFlightNow Spaceflightnow.com], Status Page last updated May 2004
* [http://spaceflightnow.com/mars/mera/status.html SpaceFlightNow Spaceflightnow.com], Status Page last updated May 2004
* [https://web.archive.org/web/20040202122109/http://marsbase.net/ Marsbase.net], a site that tracks time on Mars.
* [https://web.archive.org/web/20040105221927/http://mars.telascience.org/ MAESTRO – public version of rover simulation software] (requires download, last update October 25, 2004)
* [http://athena.cornell.edu/ Cornell's rover site: Athena] last update 2006
* [http://athena.cornell.edu/ Cornell's rover site: Athena] last update 2006
* [http://www.roving-mouse.com/planetary/Mars/Atlas/clickable-globe.html Finding ''Spirit'': interactive Mars atlas based on Viking images: you can zoom in/out and pan images, to find your preferred site. ''Spirit'' approximate position is 14.82°S (= −14.82°N), 184.85°W (= 5.15°E)] (not working as of June 4, 2008)
* [http://www.roving-mouse.com/planetary/Mars/Atlas/clickable-globe.html Finding ''Spirit'': interactive Mars atlas based on Viking images: you can zoom in/out and pan images, to find your preferred site. ''Spirit'' approximate position is 14.82°S (= −14.82°N), 184.85°W (= 5.15°E)] (not working as of June 4, 2008)
* [http://www.google.com/mars/#lat=-14.569960&lon=175.469512&zoom=12&map=infrared&q=spacecraft Google map with ''Spirit'' landing site marked]
* [http://www.google.com/mars/#lat=-14.569960&lon=175.469512&zoom=12&map=infrared&q=spacecraft Google map with ''Spirit'' landing site marked]
* [https://web.archive.org/web/20040203203120/http://www.axonchisel.net/etc/space/mars-exp-rover-highlights.html (AXCH) 2004 Mars Exploration Rovers Highlights] – News, status, technical info, history, and more.
* [https://www.newscientist.com/article.ns?id=dn7140 ''New Scientist'' on ''Spirit'' Dust Devils] {{Webarchive|url=https://web.archive.org/web/20080508195141/http://www.newscientist.com/article.ns?id=dn7140 |date=May 8, 2008 }}, March 15, 2005
* [https://www.newscientist.com/article.ns?id=dn7140 ''New Scientist'' on ''Spirit'' Dust Devils] {{Webarchive|url=https://web.archive.org/web/20080508195141/http://www.newscientist.com/article.ns?id=dn7140 |date=May 8, 2008 }}, March 15, 2005
* [https://www.newscientist.com/article/dn8944-mars-rovers-broken-wheel-is-beyond-repair.html ''New Scientist'' on ''Spirit'' wheel status], April 3, 2006
* [https://www.newscientist.com/article/dn8944-mars-rovers-broken-wheel-is-beyond-repair.html ''New Scientist'' on ''Spirit'' wheel status], April 3, 2006
* [http://www.unmannedspaceflight.com/index.php?showforum=1 Unmanned Spaceflight.com discussion on ''Spirit''] <small>as of 2008-06-04 last updated 2008-06-04</small>
* [http://www.unmannedspaceflight.com/index.php?showforum=1 Unmanned Spaceflight.com discussion on ''Spirit''] <small>as of 2008-06-04 last updated 2008-06-04</small>
*[http://nasatech.net/Mars-Columbia/index.html Full-page, High-res spherical panorama of ''Spirit'' in the Columbia Hills], <small>nasatech.net, Nov 23 to December 5, 2005 (long download, uses [[Java (software platform)|Java]])</small>
*[http://nasatech.net/Mars-Summit_Husband/index.html Full-page, High-res spherical panorama of ''Spirit'' at the summit of Husband Hill], <small>nasatech.net, Nov 23 to December 5, 2005 (long download, uses [[Java (software platform)|Java]])</small>
* [https://xkcd.com/695/ XKCD cartoon on ''Spirit'']
* [https://www.flickr.com/photos/136797589@N04/33019896621/in/photostream/ High-resolution video] by Seán Doran that zooms in on ''Spirit''{{'}}s final location
* [https://www.flickr.com/photos/136797589@N04/33019896621/in/photostream/ High-resolution video] by Seán Doran that zooms in on ''Spirit''{{'}}s final location
* [http://www.planetary.org/explore/space-topics/space-missions/mer-updates/2011/ Archive] of MER progress reports by A.J.S. Rayl at planetary.org
* [http://www.planetary.org/explore/space-topics/space-missions/mer-updates/2011/ Archive] of MER progress reports by A.J.S. Rayl at planetary.org
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{{NASAMER}}
{{NASAMER}}
{{Features visited by Spirit rover}}
{{Features visited by Spirit rover}}
{{Mars rovers}}
{{NASA navbox|state=collapsed}}
{{NASA navbox|state=collapsed}}
{{Mars spacecraft}}
{{Mars spacecraft}}
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{{DEFAULTSORT:Spirit Rover}}
{{DEFAULTSORT:Spirit Rover}}
[[Category:Space probes launched in 2003]]
[[Category:2003 robots]]
[[Category:2003 robots]]
[[Category:2004 on Mars]]
[[Category:Aeolis quadrangle]]
[[Category:Aeolis quadrangle]]
[[Category:Derelict landers (spacecraft)]]
[[Category:Derelict landers (spacecraft)]]
[[Category:Mars Exploration Rover mission|*]]
[[Category:Mars Exploration Rover mission|*]]
[[Category:Missions to Mars]]
[[Category:Mars robots]]
[[Category:Mars rovers]]
[[Category:Mars rovers]]
[[Category:Missions to Mars]]
[[Category:Robots of the United States]]
[[Category:Robots of the United States]]
[[Category:Six-wheeled robots]]
[[Category:Six-wheeled robots]]
[[Category:Soft landings on Mars]]
[[Category:Solar-powered robots]]
[[Category:Solar-powered robots]]
[[Category:Spacecraft launched by Delta II rockets]]
[[Category:Space probes launched in 2003]]
[[Category:Spacecraft decommissioned in 2011]]
[[Category:Spacecraft decommissioned in 2011]]
[[Category:Soft landings on Mars]]
[[Category:Spacecraft launched by Delta II rockets]]
[[Category:2004 on Mars]]
[[Category:Mars robots]]

Latest revision as of 21:33, 6 May 2024

Spirit
The Mars Exploration Rover-2 (MER-2) during testing for mobility and maneuverability
Mission typeRover
OperatorNASA
COSPAR ID2003-027A Edit this at Wikidata
SATCAT no.27827Edit this on Wikidata
WebsiteMars Exploration Rover
Mission durationPlanned: 90 Martian solar days (~92 Earth days)
Operational: 2269 days from landing to last contact (2208 sols)
Mobile: 1944 Earth days landing to final embedding (1892 sols)
Total: 2695 days from landing to mission end (2623 sols)
Launch to last contact: 6 years, 9 months, 12 days
Spacecraft properties
Spacecraft typeMars Exploration Rover
Launch massTotal: 1,063 kg
* rover: 185 kg
* lander: 348 kg
* backshell/parachute: 209 kg
* heat shield: 78 kg
* cruise stage: 193 kg
* propellant: 50 kg[1]
Dry mass185 kilograms (408 lb) (Rover only)
Power140 watts
Start of mission
Launch dateJune 10, 2003, 17:58:47 UTC (2003-06-10UTC17:58:47)[2]
June 10, 2003, 1:58:47 p.m. EDT (2003-06-10UTC17:58:47)[3][4]
RocketDelta II 7925-9.5[4][5]
Launch siteCape Canaveral SLC-17A
End of mission
DeclaredMay 25, 2011 (2011-05-26)[3]
Last contactMarch 22, 2010
Orbital parameters
Reference systemHeliocentric (transfer)
Mars rover
Spacecraft componentRover
Landing dateJanuary 4, 2004, 04:35 UTC SCET
MSD 46216 03:35 AMT
Landing site14°34′06″S 175°28′21″E / 14.5684°S 175.472636°E / -14.5684; 175.472636 (Spirit rover)[6]
Distance driven7.73 km (4.8 mi)

The launch patch for Spirit, featuring Marvin the Martian
NASA Mars rovers
 

Spirit, also known as MER-A (Mars Exploration Rover – A) or MER-2, is a Mars robotic rover, active from 2004 to 2010.[3] Spirit was operational on Mars for 2208 sols or 3.3 Martian years (2269 days; 6 years, 77 days). It was one of two rovers of NASA's Mars Exploration Rover Mission managed by the Jet Propulsion Laboratory (JPL). Spirit landed successfully within the impact crater Gusev on Mars at 04:35 Ground UTC on January 4, 2004, three weeks before its twin, Opportunity (MER-B), which landed on the other side of the planet. Its name was chosen through a NASA-sponsored student essay competition. The rover got stuck in a "sand trap" in late 2009 at an angle that hampered recharging of its batteries; its last communication with Earth was on March 22, 2010.

The rover completed its planned 90-sol mission (slightly less than 92.5 Earth days). Aided by cleaning events that resulted in more energy from its solar panels, Spirit went on to function effectively over twenty times longer than NASA planners expected. Spirit also logged 7.73 km (4.8 mi) of driving instead of the planned 600 m (0.4 mi),[7] allowing more extensive geological analysis of Martian rocks and planetary surface features. Initial scientific results from the first phase of the mission (the 90-sol prime mission) were published in a special issue of the journal Science.[8]

On May 1, 2009 (5 years, 3 months, 27 Earth days after landing; 21 times the planned mission duration), Spirit became stuck in soft sand.[9] This was not the first of the mission's "embedding events" and for the following eight months NASA carefully analyzed the situation, running Earth-based theoretical and practical simulations, and finally programming the rover to make extrication drives in an attempt to free itself. These efforts continued until January 26, 2010, when NASA officials announced that the rover was likely irrecoverably obstructed by its location in soft sand,[10] though it continued to perform scientific research from its current location.[11]

The rover continued in a stationary science platform role until communication with Spirit stopped on March 22, 2010 (sol 2208).[12][13] JPL continued to attempt to regain contact until May 24, 2011, when NASA announced that efforts to communicate with the unresponsive rover had ended, calling the mission complete.[14][15][16][17] A formal farewell took place at NASA headquarters shortly thereafter.

Objectives[edit]

Delta II lifting off with MER-A on June 10, 2003

The scientific objectives of the Mars Exploration Rover mission were to:[18]

  • Search for and characterize a variety of rocks and soils that hold clues to past water activity. In particular, samples sought include those that have minerals deposited by water-related processes such as precipitation, evaporation, sedimentary cementation, or hydrothermal activity.
  • Determine the distribution and composition of minerals, rocks, and soils surrounding the landing sites.
  • Determine what geologic processes have shaped the local terrain and influenced the chemistry. Such processes could include water or wind erosion, sedimentation, hydrothermal mechanisms, volcanism, and cratering.
  • Perform calibration and validation of surface observations made by Mars Reconnaissance Orbiter (MRO) instruments. This will help determine the accuracy and effectiveness of various instruments that survey Martian geology from orbit.
  • Search for iron-containing minerals, and to identify and quantify relative amounts of specific mineral types that contain water or were formed in water, such as iron-bearing carbonates.
  • Characterize the mineralogy and textures of rocks and soils to determine the processes that created them.
  • Search for geological clues to the environmental conditions that existed when liquid water was present.
  • Assess whether those environments were conducive to life.

Mission timeline[edit]

Annotated Columbia Hills panorama from the Spirit landing site
An overall view of MER-A Spirit landing site (denoted with a star)

Opportunity and Spirit rovers were part of the Mars Exploration Rover program in the long-term Mars Exploration Program. The Mars Exploration Program's four principal goals were to determine if the potential for life exists on Mars (in particular, whether recoverable water may be found on Mars), to characterize the Mars climate and its geology, and then to prepare for a potential human mission to Mars. The Mars Exploration Rovers were to travel across the Martian surface and perform periodic geologic analyses to determine if water ever existed on Mars as well as the types of minerals available, as well as to corroborate data taken by the Mars Reconnaissance Orbiter (MRO).[19] Both rovers were designed with an expected 90 sols (92 Earth days) lifetime, but each lasted much longer than expected. Spirit's mission lasted 20 times longer than its expected lifetime, and its mission was declared ended on May 25, 2011, after it got stuck in soft sand and expended its power reserves trying to free itself. Opportunity lasted 55 times longer than its 90 sol planned lifetime, operating for 5498 days from landing to mission end. An archive of weekly updates on the rover's status can be found at the Opportunity Update Archive.[20]

Launch and landing[edit]

Animation of Spirit orbit.
   Sun ·    Earth ·    Mars ·    Spirit

The MER-A (Spirit) and MER-B (Opportunity) were launched on June 10, 2003 and July 7, 2003, respectively. Though both probes launched on Boeing Delta II 7925-9.5 rockets from Cape Canaveral Space Launch Complex 17 (CCAFS SLC-17), MER-B was on the heavy version of that launch vehicle, needing the extra energy for Trans-Mars injection. The launch vehicles were integrated onto pads right next to each other, with MER-A on CCAFS SLC-17A and MER-B on CCAFS SLC-17B. The dual pads allowed for working the 15- and 21-day planetary launch periods close together; the last possible launch day for MER-A was June 19, 2003 and the first day for MER-B was June 25, 2003. NASA's Launch Services Program managed the launch of both spacecraft.

Spirit successfully landed on the surface of Mars on 04:35 Spacecraft Event Time (SCET) on January 4, 2004. This was the start of its 90-sol mission, but solar cell cleaning events would mean it was the start of a much longer mission, lasting until 2010. Spirit was targeted to a site that appears to have been affected by liquid water in the past, the crater Gusev, a possible former lake in a giant impact crater about 10 km (6.2 mi) from the center of the target ellipse[21] at 14°34′18″S 175°28′43″E / 14.5718°S 175.4785°E / -14.5718; 175.4785.[22] After the airbag-protected landing craft settled onto the surface, the rover rolled out to take panoramic images. These give scientists the information they need to select promising geological targets and drive to those locations to perform on-site scientific investigations.[23] The MER team named the landing site "Columbia Memorial Station," in honor of the seven astronauts killed in the Space Shuttle Columbia disaster.

First color image compiled from images by Spirit; it was the highest resolution color image taken on another planet.

On May 1, 2009 (sol 1892), the rover became stuck in soft sand, the machine resting upon a cache of iron(III) sulfate (jarosite) hidden under a veneer of normal-looking soil. Iron sulfate has very little cohesion, making it difficult for the rover's wheels to gain traction.[24][25]

On January 26, 2010 (sol 2155), after several months attempting to free the rover, NASA decided to redefine the mobile robot mission by calling it a stationary research platform. Efforts were directed in preparing a more suitable orientation of the platform in relation to the Sun in an attempt to allow a more efficient recharge of the platform's batteries. This was needed to keep some systems operational during the Martian winter.[26] On March 30, 2010, Spirit skipped a planned communication session and as anticipated from recent power-supply projections, had probably entered a low-power hibernation mode.[27]

The last communication with the rover was March 22, 2010 (sol 2208)[28] and there is a strong possibility the rover's batteries lost so much energy at some point that the mission clock stopped. In previous winters the rover was able to park on a Sun-facing slope and keep its internal temperature above −40 °C (−40 °F), but since the rover was stuck on flat ground it is estimated that its internal temperature dropped to −55 °C (−67 °F). If Spirit had survived these conditions and there had been a cleaning event, there was a possibility that with the southern summer solstice in March 2011, solar energy would increase to a level that would wake up the rover.[29]

Spirit remains silent at its location, called "Troy," on the west side of Home Plate. There was no communication with the rover after March 22, 2010 (sol 2208).[30]

It is likely that Spirit experienced a low-power fault and had turned off all sub-systems, including communication, and gone into a deep sleep, trying to recharge its batteries. It is also possible that the rover had experienced a mission clock fault. If that had happened, the rover would have lost track of time and tried to remain asleep until enough sunlight struck the solar arrays to wake it. This state is called "Solar Groovy." If the rover woke up from a mission clock fault, it would only listen. Starting on July 26, 2010 (sol 2331), a new procedure to address the possible mission clock fault was implemented.

End of mission[edit]

JPL continued attempts to regain contact with Spirit until May 25, 2011, when NASA announced the end of contact efforts and the completion of the mission.[14][16][31] According to NASA, the rover likely experienced excessively cold "internal temperatures" due to "inadequate energy to run its survival heaters" that, in turn, was a result of "a stressful Martian winter without much sunlight." Many critical components and connections would have been "susceptible to damage from the cold."[16] Assets that had been needed to support Spirit were transitioned to support Spirit's then still-active twin, Opportunity.[14]

The primary surface mission for Spirit was planned to last at least 90 sols. The mission received several extensions and lasted about 2,208 sols. On August 11, 2007, Spirit obtained the second longest operational duration on the surface of Mars for a lander or rover at 1282 Sols, one sol longer than the Viking 2 lander. Viking 2 was powered by a nuclear cell whereas Spirit is powered by solar arrays. Until Opportunity overtook it on May 19, 2010, the Mars probe with longest operational period was Viking 1 that lasted for 2245 Sols on the surface of Mars. On March 22, 2010, Spirit sent its last communication, thus falling just over a month short of surpassing Viking 1's operational record. An archive of weekly updates on the rover's status can be found at the Spirit Update Archive.[32]

Spirit's total odometry is 7,730.50 meters (4.80 mi).[33]

Design and construction[edit]

Annotated rover diagram
Pancam Mast Assembly (PMA)

Spirit (and its twin, Opportunity) are six-wheeled, solar-powered robots standing 1.5 meters (4.9 ft) high, 2.3 meters (7.5 ft) wide and 1.6 meters (5.2 ft) long and weighing 180 kilograms (400 lb). Six wheels on a rocker-bogie system enabled mobility over rough terrain. Each wheel had its own motor. The vehicle was steered at front and rear and was designed to operate safely at tilts of up to 30 degrees. The maximum speed was 5 centimeters per second (2.0 in/s);[34] 0.18 kilometers per hour (0.11 mph), although the average speed was about 1 centimeter per second (0.39 in/s). Both Spirit and Opportunity have pieces of the fallen World Trade Center's metal on them that were "turned into shields to protect cables on the drilling mechanisms".[35][36]

Solar arrays generated about 140 watts for up to fourteen hours per sol, while rechargeable lithium ion batteries stored energy for use at night. Spirit's onboard computer uses a 20 MHz RAD6000 CPU with 128 MB of DRAM and 3 MB of EEPROM.[37] The rover's operating temperature ranges from −40 to +40 °C (−40 to 104 °F) and radioisotope heaters provide a base level of heating, assisted by electrical heaters when necessary.[38]

Communications depended on an omnidirectional low-gain antenna communicating at a low data rate and a steerable high-gain antenna, both in direct contact with Earth. A low-gain antenna was also used to relay data to spacecraft orbiting Mars.[39]

Science payload[edit]

The science instruments included:[40]

The rover arm held the following instruments:[41]

  • Mössbauer spectrometer (MB) MIMOS II – used for close-up investigations of the mineralogy of iron-bearing rocks and soils.
  • Alpha particle X-ray spectrometer (APXS) – close-up analysis of the abundances of elements that make up rocks and soils.
  • Magnets – for collecting magnetic dust particles.
  • Microscopic Imager (MI) – obtained close-up, high-resolution images of rocks and soils.
  • Rock Abrasion Tool (RAT) – exposed fresh material for examination by instruments on board.

Spirit was 'driven' by several operators throughout its mission.[42]

Power[edit]

The rover uses a combination of solar cells and a rechargeable chemical battery.[43] This class of rover has two rechargeable lithium batteries, each composed of 8 cells with 8 amp-hour capacity.[44] At the start of the mission the solar panels could provide up to around 900 watt-hours (Wh) per day to recharge the battery and power system in one Sol, but this could vary due to a variety of factors.[43] In Eagle crater the cells were producing about 840 Wh per day, but by Sol 319 in December 2004, it had dropped to 730 Wh per day.[45]

Like Earth, Mars has seasonal variations that reduce sunlight during winter. However, since the Martian year is longer than that of the Earth, the seasons fully rotate roughly once every 2 Earth years.[46] By 2016, MER-B had endured seven Martian winters, during which times power levels drop which can mean the rover avoids doing activities that use a lot of power.[46] During its first winter power levels dropped to under 300 Wh per day for two months, but some later winters were not as bad.[46]

Another factor that can reduce received power is dust in the atmosphere, especially dust storms.[47] Dust storms have occurred quite frequently when Mars is closest to the Sun.[47] Global dust storms in 2007 reduced power levels for Opportunity and Spirit so much they could only run for a few minutes each day.[47] Due to the 2018 dust storms on Mars, Opportunity entered hibernation mode on June 12,[48][49] but it remained silent after the storm subsided in early October.[50]

Discoveries[edit]

The 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 (geologists would say they have vesicles and vugs).[51][52]

Annotated panorama of rocks near Spirit (April, 2006)

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.[53]

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).[54]

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.[55] 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.[56][57]

Astronomy[edit]

Earth from Mars
Night sky of Mars showing Deimos (left) and Phobos (right) in front of Sagittarius, as seen by Mars Exploration Rover Spirit on August 26, 2005. For full animation, see Image:Phobos & Deimos full.gif.

Spirit pointed its cameras towards the sky and observed a transit of the Sun by Mars' moon Deimos (see Transit of Deimos from Mars). It also took the first photo of Earth from the surface of another planet in early March 2004.

In late 2005, Spirit took advantage of a favorable energy situation to make multiple nighttime observations of both of Mars' moons Phobos and Deimos.[58] These observations included a "lunar" (or rather phobian) eclipse as Spirit watched Phobos disappear into Mars' shadow. Some of Spirit's star gazing was designed to look for a predicted meteor shower caused by Halley's Comet, and although at least four imaged streaks were suspect meteors, they could not be unambiguously differentiated from those caused by cosmic rays.[58]

A transit of Mercury from Mars took place on January 12, 2005, from about 14:45 UTC to 23:05 UTC. Theoretically, this could have been observed by both Spirit and Opportunity; however, camera resolution did not permit seeing Mercury's 6.1" angular diameter. They were able to observe transits of Deimos across the Sun, but at 2' angular diameter, Deimos is about 20 times larger than Mercury's 6.1" angular diameter. Ephemeris data generated by JPL Horizons indicates that Opportunity would have been able to observe the transit from the start until local sunset at about 19:23 UTC Earth time, while Spirit would have been able to observe it from local sunrise at about 19:38 UTC until the end of the transit.[clarification needed][59]

Equipment wear and failures[edit]

Both rovers passed their original mission time of 90 sols many times over. The extended time on the surface, and therefore additional stress on components, resulted in some issues developing.[30]

On March 13, 2006 (sol 778), the right front wheel ceased working[60] after having covered 4.2 mi (7 km) on Mars. Engineers began driving the rover backwards, dragging the dead wheel. Although this resulted in changes to driving techniques, the dragging effect became a useful tool, partially clearing away soil on the surface as the rover traveled, thus allowing areas to be imaged that would normally be inaccessible. However, in mid-December 2009, to the surprise of the engineers, the right front wheel showed slight movement in a wheel-test on sol 2113 and clearly rotated with normal resistance on three of four wheel-tests on sol 2117, but stalled on the fourth. On November 29, 2009 (sol 2098), the right rear wheel also stalled and remained inoperable for the remainder of the mission.

Scientific instruments also experienced degradation as a result of exposure to the harsh Martian environment and use over a far longer period than had been anticipated by the mission planners. Over time, the diamond in the resin grinding surface of the Rock Abrasion Tool wore down, after that the device could only be used to brush targets.[61] All of the other science instruments and engineering cameras continued to function until contact was lost; however, towards the end of Spirit's life, the MIMOS II Mössbauer spectrometer took much longer to produce results than it did earlier in the mission because of the decay of its cobalt-57 gamma ray source that has a half life of 271 days.

Legacy and honors[edit]

To commemorate Spirit's great contribution to the exploration of Mars, the asteroid 37452 Spirit has been named after it.[62] The name was proposed by Ingrid van Houten-Groeneveld who along with Cornelis Johannes van Houten and Tom Gehrels discovered the asteroid on September 24, 1960.

To honor the rover, the JPL team named an area near Endeavour Crater explored by the Opportunity rover, 'Spirit Point'.[63]

Documentary film, Good Night Oppy, about the Opportunity, Spirit, and their long missions, was directed by Ryan White, and included support from JPL and Industrial Light & Magic. It was released in 2022.[64]

Gallery[edit]

The rover could take pictures with its different cameras, but only the PanCam camera had the ability to photograph a scene with different color filters. The panorama views were usually built up from PanCam images. Spirit transferred 128,224 pictures in its lifetime.[65]

Missoula Crater (Sol 105, April 19, 2004)
Color panorama taken from "Larry's Lookout". On the far left is "Tennessee Valley" and on the right, rover tracks.
Annotated Apollo Hills panorama from the Spirit landing site

See also[edit]

References[edit]

  1. ^ "Mars Exploration Rovers". NASA. Retrieved December 6, 2018.
  2. ^ "Spirit". NASA's Solar System Exploration website. Retrieved December 2, 2022.
  3. ^ a b c Nelson, Jon. "Mars Exploration Rover – Spirit". NASA. Archived from the original on January 28, 2018. Retrieved February 2, 2014.
  4. ^ a b "Launch Event Details – When did the Rovers Launch?". Retrieved April 25, 2009.
  5. ^ "Mars Exploration Rover project, NASA/JPL document NSS ISDC 2001 27/05/2001" (PDF). p. 5. Archived from the original (PDF) on May 27, 2010. Retrieved April 28, 2009.
  6. ^ Staff. "Mapping the Mars Rovers' Landing Sites". Esri. Retrieved May 4, 2014.
  7. ^ "NASA Spirit Rover Completes Mission on Mars" (Press release). Jet Propulsion Laboratory. May 25, 2011. Archived from the original on June 11, 2011. Retrieved May 26, 2011.
  8. ^ "Special Issue: Spirit at Gusev Crater". Science. 305 (5685): 737–900. August 6, 2004.
  9. ^ Henry Fountain (May 26, 2009). "Crater was Shaped by Wind and Water, Mars Rover Data Shows". The New York Times.
  10. ^ Amos, Jonathan (January 26, 2010). "Nasa accepts Spirit Mars rover 'stuck for good'". BBC News. The US space agency (Nasa) has conceded defeat in its battle to free the Spirit rover from its Martian sand trap. The vehicle became stuck in soft soil back in May last year and all the efforts to extricate it have failed.
  11. ^ Brown, Dwayne; Webster, Guy (January 26, 2010). "Now a Stationary Research Platform, NASA's Mars Rover Spirit Starts a New Chapter in Red Planet Scientific Studies". NASA (Press release). Retrieved January 26, 2010. Washington – After six years of unprecedented exploration of the Red Planet, NASA's Mars Exploration Rover Spirit no longer will be a fully mobile robot. NASA has designated the once-roving scientific explorer a stationary science platform after efforts during the past several months to free it from a sand trap have been unsuccessful.
  12. ^ September 30 – October 5, 2010 Spirit Remains Silent at Troy NASA. October 5, 2010.
  13. ^ A.J.S. Rayl Mars Exploration Rovers Update Archived March 18, 2012, at the Wayback Machine Planetary Society November 30, 2010
  14. ^ a b c Webster, Guy (May 25, 2011). "NASA's Spirit Rover Completes Mission on Mars". NASA. Archived from the original on February 7, 2023. Retrieved October 12, 2011.
  15. ^ "NASA's Spirit Rover Completes Mission on Mars". NASA/JPL.
  16. ^ a b c "NASA Concludes Attempts to Contact Mars Rover Spirit". NASA. Archived from the original on October 11, 2011. Retrieved May 25, 2011.
  17. ^ Chang, Kenneth (May 24, 2011). "NASA to Abandon Mars Spirit Rover". The New York Times.
  18. ^ "Objectives - NASA". mars.nasa.gov. Retrieved April 23, 2023.
  19. ^ "Mars Exploration Rover Mission Science Objectives". mars.nasa.gov. Retrieved February 19, 2021.
  20. ^ "Opportunity Update Archive". NASA/JPL. Archived from the original on May 7, 2009. Retrieved May 4, 2009.
  21. ^ "Gusev Crater: LandingSites". marsoweb.nas.nasa.gov.
  22. ^ Spaceflightnow.com, Destination Mars, Rover headed toward hilly vista for martian exploration
  23. ^ "APOD: 2004 January 14 – A Mars Panorama from the Spirit Rover". antwrp.gsfc.nasa.gov.
  24. ^ Maggie McKee (May 12, 2009). "Mars rover may not escape sand trap for weeks". New Scientist.
  25. ^ Chang, Kenneth (May 19, 2009). "Mars rover's 5 working wheels are stuck in hidden soft spot". The New York Times. ISSN 0362-4331. Retrieved May 19, 2009.
  26. ^ "Now A Stationary Research Platform, NASA's Mars Rover Spirit Starts a New Chapter in Red Planet Scientific Studies". NASA. January 26, 2010. Archived from the original on November 29, 2014. Retrieved June 26, 2009.
  27. ^ "Spirit May Have Begun Months-Long Hibernation". NASA. March 31, 2010.
  28. ^ "Spirit status". NASA. Retrieved February 28, 2011.
  29. ^ A.J.S. Rayl Spirit Sleeps Soundlessly, Opportunity Turns a Corner Archived April 1, 2012, at the Wayback Machine Planetary Society July 31, 2010
  30. ^ a b Reisert, Sarah (2017). "Life on Mars". Distillations. 3 (1): 42–45. Archived from the original on March 25, 2019. Retrieved April 13, 2018.
  31. ^ Atkinson, Nancy (May 25, 2011). "End of the Road for Spirit Rover". Universe Today. Retrieved May 25, 2011.
  32. ^ "Spirit Update Archive". NASA/JPL. Retrieved May 4, 2009.
  33. ^ "Spirit Updates". Archived from the original on February 28, 2014. Retrieved May 14, 2012.
  34. ^ "Mars Exploration Rover Mission: The Mission". marsrovers.jpl.nasa.gov.
  35. ^ Chang, Kenneth (November 7, 2004). "Martian Robots, Taking Orders From a Manhattan Walk-Up". The New York Times. Retrieved April 9, 2009.
  36. ^ Squyres, Steve (2005). Roving Mars: Spirit, Opportunity, and the Exploration of the Red Planet. Hyperion Press. pp. 113–117. ISBN 978-1-4013-0149-1.
  37. ^ "The Rover's "Brains" - NASA". mars.nasa.gov. Retrieved April 23, 2023.
  38. ^ "The Rover's Temperature Controls - NASA". mars.nasa.gov. Retrieved April 23, 2023.
  39. ^ "The Rover's Antennas - NASA". mars.nasa.gov. Retrieved April 23, 2023.
  40. ^ "The Rover's "Eyes" and Other "Senses" - NASA". mars.nasa.gov. Retrieved April 23, 2023.
  41. ^ "The Rover's "Arm" - NASA". mars.nasa.gov. Retrieved April 23, 2023.
  42. ^ Venkatraman, Vijaysree (July 13, 2015). "The space roboticist". Science magazine. Retrieved February 14, 2019.
  43. ^ a b "Mars Exploration Rover Mission: Technology". nasa.gov. Archived from the original on December 28, 2016. Retrieved January 5, 2017.
  44. ^ "Power". Archived from the original on January 18, 2017. Retrieved September 20, 2018.
  45. ^ "Mars Exploration Rover Mission: All Opportunity Updates". nasa.gov. Archived from the original on February 1, 2017. Retrieved January 5, 2017.
  46. ^ a b c mars.nasa.gov. "Mars Rover Opportunity Busy Through Depth of Winter – Mars News". nasa.gov. Archived from the original on July 26, 2016. Retrieved January 5, 2017.
  47. ^ a b c "Europe's ExoMars mission arrives in the middle of dust season". phys.org. Archived from the original on November 30, 2016. Retrieved January 5, 2017.
  48. ^ NASA's Opportunity rover is in a deep sleep on Mars – but there's hope it will wake up again Archived June 14, 2018, at the Wayback Machine. Loren Grush, The Verge. June 13, 2018.
  49. ^ Malik, Tariq. "As Massive Storm Rages on Mars, Opportunity Rover Falls Silent". Scientific American (Space.com). Archived from the original on June 13, 2018. Retrieved June 13, 2018.
  50. ^ "Mars Exploration Rover Mission: All Opportunity Updates". mars.nasa.gov. Archived from the original on March 25, 2018. Retrieved February 10, 2018.
  51. ^ McSween, HY; Arvidson, RE; Bell Jf, 3rd; Blaney, D; Cabrol, NA; Christensen, PR; Clark, BC; Crisp, JA; et al. (2004). "Basaltic Rocks Analyzed by the Spirit Rover in Gusev Crater". Science. 305 (5685): 842–845. Bibcode:2004Sci...305..842M. doi:10.1126/science.3050842. PMID 15297668.{{cite journal}}: CS1 maint: numeric names: authors list (link)
  52. ^ Arvidson, R. E.; Anderson, RC; Bartlett, P; Bell Jf, 3rd; Blaney, D; Christensen, PR; Chu, P; Crumpler, L; et al. (2004). "Localization and physical properties experiments conducted by Spirit at Gusev Crater". Science. 305 (5685): 821–824. Bibcode:2004Sci...305..821A. doi:10.1126/science.1099922. PMID 15297662. S2CID 31102951.{{cite journal}}: CS1 maint: numeric names: authors list (link)
  53. ^ Gellert, R.; Rieder, R.; Brückner, J.; Clark, B. C.; Dreibus, G.; Klingelhöfer, G.; Lugmair, G.; Ming, D. W.; et al. (2006). "Alpha Particle X-Ray Spectrometer (APXS): Results from Gusev crater and calibration report". Journal of Geophysical Research. 111 (E2): n/a. Bibcode:2006JGRE..111.2S05G. doi:10.1029/2005JE002555. hdl:2060/20080026124. S2CID 129432577.
  54. ^ Christensen, P.; Ruff, SW; Fergason, RL; Knudson, AT; Anwar, S; Arvidson, RE; Bandfield, JL; Blaney, DL; et al. (2004). "Initial Results from the Mini-TES Experiment in Gusev Crater from the Spirit Rover". Science. 305 (5685): 837–842. Bibcode:2004Sci...305..837C. doi:10.1126/science.1100564. PMID 15297667. S2CID 34983664.
  55. ^ Bertelsen, P.; Goetz, W; Madsen, MB; Kinch, KM; Hviid, SF; Knudsen, JM; Gunnlaugsson, HP; Merrison, J; et al. (2004). "Magnetic Properties on the Mars Exploration Rover Spirit at Gusev Crater". Science. 305 (5685): 827–829. Bibcode:2004Sci...305..827B. doi:10.1126/science.1100112. PMID 15297664. S2CID 41811443.
  56. ^ Bell, J (ed.) The Martian Surface. 2008. Cambridge University Press. ISBN 978-0-521-86698-9
  57. ^ Gelbert, R. (2004). "Chemistry of Rocks and Soils in Gusev Crater from the Alpha Particle X-ray Spectrometer". Science. 305 (5685): 829–832. Bibcode:2004Sci...305..829G. doi:10.1126/science.1099913. PMID 15297665. S2CID 30195269.
  58. ^ a b Jim Bell (Cornell University) et al. Pancam Projects: Spirit Night-time Imaging. Retrieved October 21, 2008
  59. ^ Chamberlin, Alan. "HORIZONS System". ssd.jpl.nasa.gov.
  60. ^ "JPL.NASA.GOV: Mars Exploration Rovers". www-b.jpl.nasa.gov. Archived from the original on July 21, 2011.
  61. ^ "NASAʼs Mars rovers and Steve Squyres keep going and going – Cornell Chronicle". www.news.cornell.edu.
  62. ^ "Mars Exploration Rover Mission: Spotlight". marsrovers.nasa.gov. Archived from the original on May 11, 2008. Retrieved June 30, 2006.
  63. ^ Greicius, Tony; Dunbar, Brian (August 10, 2011). "Arrival at 'Spirit Point' by Mars Rover Opportunity". NASA. Retrieved February 2, 2014.
  64. ^ Ross, Rollo (November 22, 2022). "'Good Night Oppy' about NASA's rover mission may make you cry". Reuters. Retrieved April 23, 2023.
  65. ^ mars.nasa.gov. "Mars Exploration Rover". marsrovers.jpl.nasa.gov.

External links[edit]

JPL, MSSS, and NASA links[edit]

Other links[edit]