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— CH. 1 · INTRODUCTION —

Mars Exploration Rover

~9 min read · Ch. 1 of 7
7 sections
  • Mars Exploration Rover was a NASA mission that sent two robots, Spirit and Opportunity, to the surface of Mars in January 2004, with a plan for each to last exactly 90 Martian solar days. Spirit survived more than six years. Opportunity lasted nearly fifteen. When engineers finally declared the mission over in February 2019, they had been operating rovers on another planet for over a decade and a half.

    The numbers are hard to absorb. Each rover was designed to drive a total of 600 meters. Opportunity eventually covered more than 45 km. At one point it passed the total distance driven by the Apollo 17 Lunar Roving Vehicle on the Moon. It then broke the record held by the Soviet Lunokhod 2. On the 23rd of March 2015, it crossed the 42.2 km mark, the full distance of a marathon, with a finish time of roughly 11 years and 2 months.

    But raw distance only hints at what the mission accomplished. The original scientific objective was to search for rocks and soils that carry signs of past water activity on Mars. What the rovers found, in crater walls and plains and layered outcrops, rewrote how scientists understand a planet once thought to be bone dry. How two machines, launched in the summer of 2003, managed to survive dust storms, mechanical failures, and Martian winters to return that story is the subject of this documentary.

  • Sofi Collis was nine years old and in third grade in Arizona when she won the essay competition that named the two rovers. She had been born in Russia and spent part of her childhood in an orphanage. Her winning entry read, in part: "I used to live in an orphanage. It was dark and cold and lonely. At night, I looked up at the sparkly sky and felt better. I dreamed I could fly there. In America, I can make all my dreams come true. Thank you for the 'Spirit' and the 'Opportunity.'" The names stuck in a way that the mission designations MER-A and MER-B never could.

    Before the competition, the rovers were identified internally as MER-1 Rover 1 and MER-2 Rover 2. Engineers at the Jet Propulsion Laboratory, which designed, built, and operated the whole mission, used MER-A for Spirit and MER-B for Opportunity based on the order each touched down on Mars. Two asteroids were eventually named in the rovers' honor, 37452 Spirit and 39382 Opportunity, a recognition of the scientific record both had accumulated.

  • Spirit lifted off on the 10th of June 2003 aboard a Boeing Delta II 7925-9.5 rocket from Cape Canaveral Space Launch Complex 17A. Opportunity followed on the 7th of July 2003 from the adjacent pad, SLC-17B, on the heavier version of the same rocket, because it needed more energy for the Trans-Mars injection. The two pads sit right next to each other, which allowed mission planners to work the 15-day and 21-day planetary launch windows close together. The last possible launch day for Spirit was the 19th of June 2003; the first available day for Opportunity was the 25th of June 2003.

    The cruise stage that carried each rover across roughly 500 million kilometers was spin-stabilized at two revolutions per minute. Solar arrays on the outer ring could generate up to 600 watts near Earth and around 300 watts at Mars. Two aluminium-lined tanks held about 31 kg of hydrazine propellant for course corrections, and navigators planned up to six trajectory correction maneuvers along the way. A star scanner and a Sun sensor gave the spacecraft its orientation, with no backup system for the star scanner.

    Entry into the Martian atmosphere was the most violent phase of the journey. The aeroshell, built by Lockheed Martin Space in Denver, Colorado, used an ablator made of cork wood, binder, and silica glass spheres, a formula first developed for the Viking Mars lander missions and closely related to the materials used in the Mercury, Gemini, and Apollo crewed flights. The spacecraft slowed from 19,000 to 1,600 km/h in about a minute, generating roughly 60 meters per second squared of acceleration. A parachute 40% larger than the one flown on Mars Pathfinder, designed and built by Pioneer Aerospace in South Windsor, Connecticut, helped brake the descent. Three RAD rockets, each producing about a ton of force for nearly 4 seconds, brought the lander to a dead stop 10-15 meters above the surface. Then airbags made of Vectran, a material with roughly twice the strength of Kevlar, inflated and let the lander bounce across the Martian surface at approximately 100 km/h before coming to rest.

  • Each rover stands 1.5 meters high, 2.3 meters wide, and 1.6 meters long, and weighs 180 kg, with 35 kg of that in the wheel and suspension system alone. Six aluminium wheels mount on a rocker-bogie suspension, the same basic design used on the smaller Sojourner rover, which keeps all wheels on the ground over rough terrain and allows the vehicle to cross obstacles larger than a wheel diameter of 250 mm. The wheels have cleats for grip in soft sand and rock faces. Each wheel has its own drive motor, and the front and rear wheels each carry individual steering motors, so the rover can turn on the spot through a full revolution. Maxon Motor, a Swiss company, made the drive motors.

    Power came from triple-junction solar arrays that generate about 140 watts when fully illuminated, enough to run the rover for up to four hours per Martian day. The rover needs around 100 watts just to drive. Two lithium-ion batteries weighing 7.15 kg each stored energy for the night. Engineers expected dust to cut solar output to roughly 50 watts by the end of the 90-sol mission. What actually happened was that wind-driven cleaning events removed dust from the panels far more often than anticipated, and power output remained between 300 and 900 watt-hours per day across much of the extended mission.

    At the heart of each rover is a radiation-hardened RAD6000 processor running at 20 MHz, paired with 128 MB of DRAM and 256 MB of flash memory. The operating system is VxWorks. Onboard instruments include nine cameras, a Miniature Thermal Emission Spectrometer built by Arizona State University, a Mössbauer spectrometer developed by Göstar Klingelhöfer at Johannes Gutenberg University in Mainz, an alpha particle X-ray spectrometer from the Max Planck Institute for Chemistry, also in Mainz, and a Rock Abrasion Tool built by Honeybee Robotics that can grind a hole 45 mm across and 5 mm deep in hard volcanic rock in about two hours.

  • Gusev crater looked, from orbit, like a dry lakebed. When Spirit arrived on the plains inside it, the reality was more complicated. The surface rocks were basalt, volcanic in origin, containing olivine, pyroxene, plagioclase, and magnetite. Signs of water were subtle: thin coatings on the rocks, and some mineral deposits suggesting water had once moved through cracks.

    Spirit's most significant geology came when it climbed up from the plains into the Columbia Hills. On the 21st of August 2005, after 581 sols of driving and a journey of 4.81 km, it reached the summit of Husband Hill. Scientists categorized the rocks there into six groups, named Clovis, Wishbone, Peace, Watchtower, Backstay, and Independence, each after a prominent rock within the group. All six showed signs of alteration by water. The Clovis group contained goethite, detected by the Mössbauer spectrometer. Goethite forms only in the presence of water, making it the first direct mineralogical evidence of past water in those hills. Later in the mission, data from the Mini-TES confirmed carbonate-rich rocks in an outcrop called Comanche, another marker of ancient water.

    Spirit's front right wheel stopped working on the 13th of March 2006 while the rover was heading toward McCool Hill. Drivers tried dragging the dead wheel behind the rover, but soft sand on the lower slopes stopped that approach. Spirit spent the subsequent Martian winter parked on a feature called Low Ridge Haven, angled to collect enough sunlight to survive. Years later, in January 2010, NASA announced that Spirit had become permanently stuck in soft Martian sand and would serve as a stationary research platform. The last successful communication with the rover was on the 22nd of March 2010.

  • Opportunity landed in a small crater the science team nicknamed Eagle, on the flat plains of Meridiani Planum. Within the crater walls, the rover found something that had not been seen before on Mars: layered bedrock with sedimentary texture and, embedded in the soil, small spherical concretions the team called blueberries. Chemical analysis showed the blueberries were rich in hematite and had formed in an aqueous environment. The rock itself was primarily Jarosite, a ferrous sulfate mineral that forms as an evaporite when a salty body of water dries up.

    On the 23rd of March 2004, a news conference announced major discoveries of evidence for past liquid water on the Martian surface. Data from Meridiani showed a stratified pattern and cross-bedding in the rocks inside the crater. The irregular distribution of chlorine and bromine further suggested the site was once the shoreline of a salty sea.

    Opportunity kept moving. In February 2007, it became the first spacecraft to travel 10 km on the surface of Mars. It entered Victoria Crater in September 2007 and spent months exploring its interior before climbing out in August 2008. Project scientist Bruce Banerdt was quoted as saying the rover had done everything expected inside Victoria and more. On the 7th of March 2009, after driving about 3.2 km since leaving Victoria, Opportunity first caught sight of the rim of the much larger Endeavour crater, a 25-km-diameter feature whose orbital spectroscopy showed phyllosilicate rocks, indicative of older sedimentary deposits. It finally reached Endeavour's rim eight years after landing. By January 2009, the two rovers together had sent back 250,000 images.

  • In July 2007, during the fourth mission extension, a global Martian dust storm reduced sunlight so severely that engineers feared one or both rovers might be permanently disabled. Both hunkered down. Opportunity's power dipped to 128 watt-hours during that storm. The storm lifted, and both rovers resumed driving roughly two months after suspending operations.

    In June 2018, Opportunity was caught in a second global dust storm. Solar power fell below the threshold for normal operation, and the last contact with the rover came on the 10th of June 2018. NASA kept sending signals after the storm subsided, but the rover did not respond, possibly because a catastrophic system failure had occurred or because dust had settled thickly over the solar panels. On the 13th of February 2019, at a press conference, NASA officially declared the Opportunity mission over, closing a mission that had run for sixteen years.

    The fifth and final mission extension had been granted in October 2007, running through the end of 2009. The total cost of building, launching, landing, and operating the rovers for the initial 90-sol primary mission was 820 million US dollars. The first four extensions together added 104 million dollars, and the fifth cost at least 20 million. At their death, both rovers had long since paid back that investment in ways that went beyond the original mission brief: by January 2014, NASA had formally expanded its Mars objectives to include searching for evidence of ancient life, a goal that grew directly from what Spirit and Opportunity had found in the rocks of Gusev and Meridiani.

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Common questions

How long did the Mars Exploration Rover mission last?

The Mars Exploration Rover mission lasted sixteen years. Spirit was active until the 22nd of March 2010, and Opportunity until the 10th of June 2018. NASA officially declared the mission over on the 13th of February 2019.

How far did Opportunity rover travel on Mars?

Opportunity traveled more than 45 km on the Martian surface, far exceeding its designed goal of 600 meters. On the 23rd of March 2015 it crossed the marathon distance of 42.2 km, and it previously surpassed both the Apollo 17 Lunar Roving Vehicle and the Soviet Lunokhod 2 rover for total distance driven on another world.

Who named the Spirit and Opportunity rovers?

The rovers were named by Sofi Collis, a nine-year-old third-grade Russian-American student from Arizona, through a NASA student essay competition. Her winning essay drew on her experience growing up in an orphanage and her hope that America would let her dreams come true.

What did the Mars Exploration Rovers discover about water on Mars?

Both rovers found strong evidence that liquid water once existed on Mars. Opportunity found Jarosite, an evaporite mineral that forms when salty water dries up, along with layered sedimentary bedrock and hematite-rich spherical concretions formed in an aqueous environment. Spirit found goethite in the Columbia Hills, a mineral that forms only in the presence of water, and later confirmed carbonate-rich rocks at an outcrop called Comanche.

What caused Spirit rover to stop working?

Spirit became permanently stuck in soft Martian sand in a region near Gusev crater. NASA announced in January 2010 that it would be used as a stationary research platform. The last successful communication with Spirit was on the 22nd of March 2010, and NASA ceased attempts to contact the rover on the 22nd of May 2011.

How much did the Mars Exploration Rover mission cost?

The initial 90-sol primary mission cost 820 million US dollars to build, launch, land, and operate. The first four mission extensions added 104 million dollars, and the fifth extension, granted in October 2007, cost at least 20 million dollars.

All sources

82 references cited across the entry

  1. 1webRover Update: 2010: Allmars.nasa.gov
  2. 2webAfter 15 years, the Mars Opportunity rover's mission has endedAshley Strickland — February 13, 2019
  3. 5webNASA extends Mars rovers' missionNBC News — October 16, 2007
  4. 15webNASA Extends Mars Rover Mission a Fifth TimeNASA — October 15, 2007
  5. 18newsNASA's rovers mark five years on Red PlanetCNN — January 3, 2009
  6. 20webOpportunity Rover Passes 10-Mile Mark on MarsSpace.com — May 26, 2009
  7. 30journalIntroduction to Special Issue - Habitability, Taphonomy, and the Search for Organic Carbon on MarsJohn P. Grotzinger — January 24, 2014
  8. 33journalA Habitable Fluvio-Lacustrine Environment at Yellowknife Bay, Gale Crater, MarsGrotzinger, J.P. — January 24, 2014
  9. 37webNASA's Mars Rover Opportunity Concludes a 15-Year MissionKenneth Chang — February 13, 2019
  10. 38bookPlanet MarsSpringerLink — 2008
  11. 39webWhat are the RAD Rockets?mars.nasa.gov
  12. 46journalThe performance of gallium arsenide/germanium solar cells at the Martian surfaceD. Crisp et al. — 2004
  13. 50journalAn overview of the 1985–2006 Mars Orbiter Camera science investigationMichael C. Malin et al. — January 6, 2010
  14. 52webThe IECR Progressive Wavelet Image CompressorA Kiely et al. — 2003-11-15
  15. 56journalThe miniaturized Mössbauer spectrometer MIMOS II for extraterrestrial and outdoor terrestrial applications: A status reportKlingelhöfer G. et al. — 2002
  16. 60journalThe new Athena alpha particle X-ray spectrometer for the Mars Exploration RoversR. Rieder et al. — 2003
  17. 61webOverviewMarch 22, 2024
  18. 67webTest-Bed Rover is Now Stuck — Which is a Good Thing!Nancy Atkinson — July 2, 2009
  19. 69journalLocalization and Physical Properties Experiments Conducted by Spirit at Gusev CraterArvidson R. E. — 2004
  20. 70journalThe Alpha Particle X-ray Spectrometer (APXS): results from Gusev crater and calibration reportGelbert R. — 2006
  21. 71journalInitial Results from the Mini-TES Experiment in Gusev Crater from the Spirit RoverChristensen P — August 2004
  22. 72journalMagnetic Properties on the Mars Exploration Rover Spirit at Gusev CraterBertelsen P. — 2004
  23. 73journalChemistry of Rocks and Soils in Gusev Crater from the Alpha Particle X-ray SpectrometerGelbert R. — 2004
  24. 75journalMars Exploration Rover Geologic Traverse by the Spirit Rover in the Plains of Gusev Crater, MarsCrumpler L. — 2005
  25. 76journalRocks of the Columbia HillsSquyres S. — 2006
  26. 77journalGeochemical and mineralogical indicators for aqueous processes in the Columbia Hills of Gusev crater, MarsMing D. — 2006
  27. 80journalOutcrop of long-sought rare rock on Mars foundR. V. Morris et al. — June 4, 2010
  28. 81journalIdentification of Carbonate-Rich Outcrops on Mars by the Spirit RoverMorris Richard V. et al. — 2010
  29. 82journalThe Opportunity Rover's Athena Science Investigation At Meridiani Planum, MarsSquyres S. — 2004
  30. 83journalOverview of the Opportunity Mars Exploration Rover Mission to Meridiani Planum: Eagle Crater to Purgatory DuneSquyres S. — 2006