Starting in 1960, the
Soviet space program launched a series of probes to Mars including the first intended (but unsuccessful) flybys and hard (
impact) landing. In November 1962,
Mars 2MV-3 No.1 was intended to land on Mars but didn't manage to leave the
low Earth orbit and decayed down the Earth's atmosphere, disintegrating progressively. On November 14, 1971,
Mariner 9 became the first space probe to orbit another planet when it entered into orbit around Mars. The amount of data returned by probes increased substantially as technology improved. The first to contact the surface were two Soviet probes:
Mars 2 lander on November 27 and
Mars 3 lander on December 2, 1971. Mars 2's landing system failed during descent and the probe was lost in the subsequent crash. Mars 3 succeeded in the first Martian
soft landing.
Mars 6 failed during descent but did return some corrupted atmospheric data in 1974. The 1975 NASA launches of the
Viking program consisted of two orbiters, each with a lander that successfully soft landed in 1976.
Viking 1 remained operational for six years,
Viking 2 for three years. The Viking landers relayed the first color panoramas of Mars. The Soviet probes
Phobos 1 and 2 were sent to Mars in 1988 to study Mars and its two moons, with a focus on Phobos. Phobos 1 lost contact on the way to Mars. Phobos 2, while successfully photographing Mars and Phobos, failed before it was set to release two landers to the surface of Phobos. Missions that ended prematurely after Phobos 1 and 2 (1988) include (see
Probe difficulties section for more details): •
Mars Observer (launched in 1992) •
Mars 96 (1996) •
Mars Climate Orbiter (1999) •
Mars Polar Lander with
Deep Space 2 (1999) •
Nozomi (2003) •
Beagle 2 (2003) •
Fobos-Grunt with
Yinghuo-1 (2011) •
Schiaparelli lander (2016) Following the 1993 failure of the
Mars Observer orbiter, the NASA
Mars Global Surveyor achieved Mars orbit in 1997. This mission was a complete success, having finished its primary mapping mission in early 2001. Contact was lost with the probe in November 2006 during its third extended program, spending exactly 10 operational years in space. The NASA
Mars Pathfinder, carrying a robotic exploration vehicle
Sojourner, landed in the
Ares Vallis on Mars in July 1997, returning many images. NASA's
Mars Odyssey orbiter entered Mars orbit in 2001.
Odyssey Gamma Ray Spectrometer detected significant amounts of hydrogen in the upper metre or so of
regolith on Mars. This hydrogen is thought to be contained in large deposits of
water ice. The
Mars Express mission of the
European Space Agency (ESA) reached Mars in 2003. It carried the
Beagle 2 lander, which was not heard from after being released and was declared lost in February 2004.
Beagle 2 was located in January 2015 by the HiRise camera on NASA's
Mars Reconnaissance Orbiter (MRO) having landed safely but failed to fully deploy its solar panels and antenna. In early 2004, the
Mars Express Planetary Fourier Spectrometer team announced the orbiter had detected
methane in the Martian atmosphere, a potential
biosignature. ESA announced in June 2006 the discovery of
aurora on Mars by the
Mars Express. In January 2004, the NASA twin
Mars Exploration Rovers named
Spirit (MER-A) and
Opportunity (MER-B) landed on the surface of Mars. Both have met and exceeded all their science objectives. Among the most significant scientific returns has been conclusive evidence that liquid water existed at some time in the past at both landing sites.
Martian dust devils and windstorms have occasionally cleaned both rovers' solar panels, and thus increased their lifespan.
Spirit rover (MER-A) was active until 2010, when it stopped sending data because it got stuck in a sand dune and was unable to reorient itself to recharge its batteries.
Rosetta came within 250 km of Mars during its 2007 flyby.
Dawn flew by Mars in February 2009 for a gravity assist on its way to investigate
Vesta and
Ceres.
Phoenix landed on the north polar region of Mars on May 25, 2008. Its robotic arm dug into the Martian soil and the presence of water ice was confirmed on June 20, 2008. The mission concluded on November 10, 2008, after contact was lost. In 2008, the price of transporting material from the surface of Earth to the surface of Mars was approximately
US$309,000 per
kilogram. The
Indian Space Research Organisation (ISRO) launched their
Mars Orbiter Mission (MOM) on November 5, 2013, and it was inserted into Mars orbit on September 24, 2014. India's ISRO is the fourth space agency to reach Mars, after the Soviet space program, NASA and ESA. India successfully placed a spacecraft into Mars orbit, and became the first country to do so in its maiden attempt.
Overview of missions The following entails a brief overview of previous missions to Mars, oriented towards orbiters and flybys; see also
Mars landing and
Mars rover.
Early Soviet missions 1960s spacecraft Between 1960 and 1969, the Soviet Union launched nine probes intended to reach Mars. They all failed: three at launch; three failed to reach near-Earth orbit; one during the burn to put the spacecraft into trans-Mars trajectory; and two during the interplanetary orbit. The
Mars 1M programs (sometimes dubbed Mars-nik in Western media) was the first Soviet uncrewed spacecraft interplanetary exploration program, which consisted of two flyby probes launched towards Mars in October 1960,
Mars 1960A and
Mars 1960B (also known as
Korabl 4 and
Korabl 5 respectively). After launch, the third stage pumps on both launchers were unable to develop enough pressure to commence ignition, so Earth parking orbit was not achieved. The spacecraft reached an altitude of 120 km before reentry.
Mars 1962A was a Mars flyby mission, launched on October 24, 1962, and
Mars 1962B an intended first Mars lander mission, launched in late December of the same year (1962). Both failed from either breaking up as they were going into Earth orbit or having the upper stage explode in orbit during the burn to put the spacecraft into trans-Mars trajectory. Sixty-one radio transmissions were held, initially at 2-day intervals and later at 5-day intervals, from which a large amount of interplanetary data was collected. On 21 March 1963, when the spacecraft was at a distance of 106,760,000 km from Earth, on its way to Mars, communications ceased due to failure of its antenna orientation system.
1970s The USSR intended to have the first artificial satellite of Mars beating the planned American
Mariner 8 and
Mariner 9 Mars orbiters. In May 1971, one day after Mariner 8 malfunctioned at launch and failed to reach orbit,
Cosmos 419 (Mars 1971C), a heavy probe of the Soviet Mars program M-71, also failed to launch. This spacecraft was designed as an orbiter only, while the next two probes of project M-71,
Mars 2 and
Mars 3, were multipurpose combinations of an orbiter and a lander with small skis-walking
rovers,
PrOP-M, that would be the first planet rovers outside the Moon. They were successfully launched in mid-May 1971 and reached Mars about seven months later. On November 27, 1971, the lander of Mars 2
crash-landed due to an on-board computer malfunction and became the first man-made object to reach the surface of Mars. On 2 December 1971, the Mars 3 lander became the first spacecraft to achieve a
soft landing, but its transmission was interrupted after 14.5 seconds. The Mars 2 and 3 orbiters sent back a relatively large volume of data covering the period from December 1971 to March 1972, although transmissions continued through to August. By 22 August 1972, after sending back data and a total of 60 pictures, Mars 2 and 3 concluded their missions. The images and data enabled creation of surface relief maps, and gave information on the Martian
gravity and
magnetic fields. In 1973, the Soviet Union sent four more probes to Mars: the
Mars 4 and
Mars 5 orbiters and the
Mars 6 and
Mars 7 flyby/lander combinations. All missions except Mars 7 sent back data, with Mars 5 being most successful. Mars 5 transmitted just 60 images before a loss of pressurization in the transmitter housing ended the mission. Mars 6 lander transmitted data during descent, but failed upon impact. Mars 4 flew by the planet at a range of 2200 km returning one swath of pictures and radio
occultation data, which constituted the first detection of the nightside
ionosphere on Mars. Mars 7 probe separated prematurely from the carrying vehicle due to a problem in the operation of one of the onboard systems (
attitude control or retro-rockets) and missed the planet by .
Mariner program In 1964,
NASA's
Jet Propulsion Laboratory made two attempts at reaching Mars.
Mariner 3 and
Mariner 4 were identical spacecraft designed to carry out the first flybys of Mars. Mariner 3 was launched on November 5, 1964, but the shroud encasing the spacecraft atop its rocket failed to open properly, dooming the mission. Three weeks later, on November 28, 1964, Mariner 4 was launched successfully on a 7-month voyage to Mars. Mariner 4 flew past Mars on July 14, 1965, providing the first close-up photographs of another planet. The pictures, gradually played back to Earth from a small tape recorder on the probe, showed impact craters. It provided radically more accurate data about the planet; a surface
atmospheric pressure of about 1% of Earth's and daytime temperatures of −100 °C (−148 °F) were estimated. No
magnetic field or
Martian radiation belts were detected. The new data meant redesigns for then planned Martian landers, and showed life would have a more difficult time surviving there than previously anticipated. , as seen by Mariner 4. The location is
Phaethontis quadrangle. NASA continued the Mariner program with another pair of Mars flyby probes,
Mariner 6 and 7. They were sent at the next launch window, and reached the planet in 1969. During the following launch window the Mariner program again suffered the loss of one of a pair of probes.
Mariner 9 successfully entered orbit about Mars, the first spacecraft ever to do so, after the launch time failure of its sister ship,
Mariner 8. When Mariner 9 reached Mars in 1971, it and two Soviet orbiters (Mars 2 and Mars 3) found that a planet-wide dust storm was in progress. The mission controllers used the time spent waiting for the storm to clear to have the probe rendezvous with, and photograph,
Phobos. When the storm cleared sufficiently for Mars's surface to be photographed by Mariner 9, the pictures returned represented a substantial advance over previous missions. These pictures were the first to offer more detailed evidence that liquid water might at one time have flowed on the planetary surface. They also finally discerned the true nature of many Martian albedo features. For example, Nix Olympica was one of only a few features that could be seen during the planetary duststorm, revealing it to be the
highest mountain (
volcano, to be exact) on any planet in the entire
Solar System, and leading to its reclassification as
Olympus Mons.
Viking program The Viking program launched
Viking 1 and
Viking 2 spacecraft to Mars in 1975; The program consisted of two orbiters and two landers – these were the second and third spacecraft to successfully land on Mars. In 1976,
Viking 1 and
Viking 2 touched down on the Martian surface. These landers were significantly larger than the Soviet Mars 3 lander (Viking 1 was 3,527 kilograms compared to the 358 kg Mars 3 lander). They were able to take the first photographs from the surface of Mars. Viking 1 operated on the surface of Mars for around six years (On Nov 11, 1982 the Lander stopped operating after getting a faulty command) and Viking 2 for over three years (mission ended in early 1980). Both landers were equipped with a robotic sampler arm which successfully scooped up soil samples and tested them with instruments such as a
Gas chromatography–mass spectrometer. The landers measured temperatures ranging from negative 86 degrees Celsius before dawn to negative 33 degrees Celsius in the afternoon. Both landers had issues obtaining accurate results from their
seismometers. Photographs from the landers and orbiters surpassed expectations in quality and quantity. The total exceeded 4,500 from the landers and 52,000 from the orbiters. The Viking landers recorded atmospheric pressures ranging from below 7 millibars (0.0068 bars) to over 10 millibars (0.0108 bars) over the Martian year, leading to the conclusion that atmospheric pressure varies by 30 percent during the Martian year because carbon dioxide condenses and sublimes at the polar caps. Martian winds generally blow more slowly than expected, scientists had expected them to reach speeds of several hundred miles an hour from observing global dust storms, but neither lander recorded gusts over 120 kilometers (74 miles) an hour, and average velocities were considerably lower. Nevertheless, the orbiters observed more than a dozen small dust storms. The Viking landers detected
nitrogen in the atmosphere for the first time, and that it was a significant component of the Martian atmosphere. There was speculation from the atmospheric analysis that the atmosphere of Mars used to be much denser. '' takes Alpha Proton X-ray Spectrometer measurements of the
Yogi Rock.
Mars Pathfinder was a U.S. spacecraft that landed a base station with a
roving probe on Mars on July 4, 1997. It consisted of a lander and a small wheeled robotic rover named
Sojourner, which was the first rover to operate on the surface of Mars. In addition to scientific objectives, the Mars Pathfinder mission was also a "proof-of-concept" for various technologies, such as an
airbag landing system and automated obstacle avoidance, both later exploited by the
Mars Exploration Rovers. The mission studied the entire Martian surface, atmosphere, and interior, and returned more data about the red planet than all previous Mars missions combined. The data has been archived and remains available publicly. ,
Bahram Vallis,
Vedra Vallis,
Maumee Vallis, and
Maja Valles. Map location is in
Lunae Palus quadrangle and includes parts of Lunae Planum and
Chryse Planitia.|A color-coded elevation map produced from data collected by
Mars Global Surveyor indicating the result of floods on Mars Among key scientific findings,
Global Surveyor took pictures of gullies and debris flow features that suggest there may be current sources of liquid water, similar to an
aquifer, at or near the surface of the planet. Similar channels on Earth are formed by flowing water, but on Mars the temperature is normally too cold and the atmosphere too thin to sustain liquid water. Nevertheless, many scientists hypothesize that liquid groundwater can sometimes surface on Mars, erode gullies and channels, and pool at the bottom before freezing and evaporating.
Magnetometer readings showed that the planet's
magnetic field is not globally generated in the planet's core, but is localized in particular areas of the crust. New temperature data and closeup images of the Martian moon Phobos showed that its surface is composed of powdery material at least 1 meter (3 feet) thick, caused by millions of years of meteoroid impacts. Data from the spacecraft's
laser altimeter gave scientists their first 3-D views of Mars's north polar ice cap in January 1999. Faulty software uploaded to the vehicle in June 2006 caused the spacecraft to orient its solar panels incorrectly several months later, resulting in battery overheating and subsequent failure. On November 5, 2006, MGS lost contact with Earth. NASA ended efforts to restore communication on January 28, 2007.
Mars Odyssey and Mars Express '' trajectory around
Mars from 24 October 2001 to 24 October 2002 '' trajectory around
Mars from 25 December 2003 to 1 January 2010 In 2001, NASA's
Mars Odyssey orbiter arrived at Mars. Its mission is to use
spectrometers and imagers to hunt for evidence of past or present
water and volcanic activity on Mars. In 2002, it was announced that the probe's
gamma-ray spectrometer and
neutron spectrometer had detected large amounts of
hydrogen, indicating that there are vast deposits of water ice in the upper three meters of Mars's soil within 60° latitude of the south pole. On June 2, 2003, the
European Space Agency's
Mars Express set off from
Baikonur Cosmodrome to Mars. The Mars Express craft consists of the
Mars Express Orbiter and the stationary lander
Beagle 2. The lander carried a digging device and the smallest mass
spectrometer created to date, as well as a range of other devices, on a robotic arm in order to accurately analyze soil beneath the dusty surface to look for
biosignatures and
biomolecules. The orbiter entered Mars orbit on December 25, 2003, and Beagle 2 entered Mars's atmosphere the same day. However, attempts to contact the lander failed. Communications attempts continued throughout January, but Beagle 2 was declared lost in mid-February, and a joint inquiry was launched by the UK and ESA. The Mars Express Orbiter confirmed the presence of water ice and carbon dioxide ice at the planet's south pole, while NASA had previously confirmed their presence at the north pole of Mars. The lander's fate remained a mystery until it was located intact on the surface of Mars in a series of images from the
Mars Reconnaissance Orbiter. The images suggest that two of the spacecraft's four
solar panels failed to deploy, blocking the spacecraft's communications antenna.
Beagle 2 is the first British and first European probe to achieve a soft landing on Mars.
MER, Opportunity rover, Spirit rover, Phoenix lander NASA's Mars Exploration Rover Mission (MER), started in 2003, was a robotic space mission involving two rovers,
Spirit (MER-A) and
Opportunity, (MER-B) that explored the Martian surface geology. The mission's scientific objective was to search for and characterize a wide range of rocks and soils that hold clues to past water activity on Mars. The mission was part of NASA's Mars Exploration Program, which includes three previous successful landers: the two Viking program landers in 1976; and Mars Pathfinder probe in 1997.
Rosetta and Dawn swingbys The
ESA Rosetta space probe mission to the comet
67P/Churyumov-Gerasimenko flew within 250 km of Mars on February 25, 2007, in a
gravitational slingshot designed to slow and redirect the spacecraft. The NASA
Dawn spacecraft used the gravity of Mars in 2009 to change direction and velocity on its way to
Vesta, and tested out
Dawn cameras and other instruments on Mars.
Fobos-Grunt On November 8, 2011, Russia's
Roscosmos launched
Fobos-Grunt, which consisted of a lander aimed to
retrieve a sample back to Earth from Mars's moon
Phobos, and place the Chinese
Yinghuo-1 probe in Mars's orbit. The mission suffered a complete control and communications failure shortly after launch and was left stranded in
low Earth orbit, later falling back to Earth. The Yinghuo-1 satellite and Fobos-Grunt underwent destructive re-entry on January 15, 2012, finally disintegrating over the Pacific Ocean.
Mars Orbiter Mission The
Mars Orbiter Mission, also called
Mangalyaan, was launched on 5 November 2013 by the
Indian Space Research Organisation (ISRO). It was successfully inserted into Martian orbit on 24 September 2014. The mission is a technology demonstrator, and as secondary objective, it will also study the Martian atmosphere. This is India's first mission to Mars, and with it, ISRO became the fourth space agency to successfully reach Mars after the Soviet Union,
NASA (USA) and
ESA (Europe). It was completed in a record low budget of $71 million, making it the least-expensive Mars mission to date. The mission concluded on September 27, 2022, after contact was lost.
InSight and MarCO In August 2012, NASA selected
InSight, a $425 million lander mission with a heat flow probe and seismometer, to determine the deep interior structure of Mars.
InSight landed successfully on Mars on 26 November 2018. Valuable data on the atmosphere, surface and the planet's interior were gathered by Insight. Insight's mission was declared as ended on 21 December 2022. Two flyby
CubeSats called
MarCO were launched with
InSight on 5 May 2018 to provide real-time telemetry during the entry and landing of
InSight. The CubeSats separated from the Atlas V booster 1.5 hours after launch and traveled their own trajectories to Mars.
MAVEN NASA's
MAVEN orbiter was launched on 18 November 2013, and on 22 September 2014 it was injected into an areocentric elliptic orbit 6,200 km (3,900 mi) by 150 km (93 mi) above the planet's surface to study its atmosphere. Mission goals included determining how the planet's atmosphere and water, presumed to have once been substantial, were lost over time. It also serves as a communications relay satellite for landers and rovers on the surface. On 6 December 2025, MAVEN lost contact with Earth. == Current missions ==