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Mars landing

A Mars landing is the controlled descent and touchdown of a spacecraft on the surface of Mars, enabling scientific instruments to analyze the planet's geology, atmosphere, climate, and potential for past habitability. The first soft landing on Mars was achieved by the Soviet Union's Mars 3 lander on December 2, 1971, though it operated for only about 14.5 seconds before losing contact during a severe dust storm.^[1] The first fully successful landing came nearly five years later with NASA's Viking 1 on July 20, 1976, in the Chryse Planitia region, where it transmitted images and data for over six years.^[2] Since these pioneering efforts, Mars landings have become a cornerstone of robotic planetary exploration, with missions deploying stationary landers and mobile rovers to gather evidence of ancient water flows, volcanic activity, and organic compounds. The challenges of Mars landings stem from the planet's thin atmosphere—about 1% as dense as Earth's—which provides insufficient drag for parachutes alone, necessitating advanced entry, descent, and landing (EDL) technologies like heat shields, retro-rockets, and sky cranes to achieve precision touchdown at speeds over 12,000 miles per hour.^[3] NASA's Viking program set the stage with Viking 2 landing successfully on September 3, 1976, in Utopia Planitia, conducting similar surface and meteorological studies.^[2] Subsequent U.S. missions advanced mobility and longevity: the 1997 Mars Pathfinder delivered the Sojourner rover, the first wheeled vehicle on another planet, testing autonomous navigation; the 2004 Mars Exploration Rovers Spirit and Opportunity far exceeded expectations, with Opportunity operating for nearly 15 years and discovering hematite spheres indicative of past liquid water.^[2] Later landings expanded scientific scope, including NASA's Phoenix lander on May 25, 2008, which confirmed water ice in the northern polar plains by excavating soil samples.^[2] The Curiosity rover touched down in Gale Crater on August 6, 2012, using a novel sky crane system, and has since analyzed habitable environments through rock drilling and chemical spectroscopy.^[2] Stationary missions like InSight, landing November 26, 2018, probed Mars's interior with seismometers, detecting marsquakes and revealing a liquid core.^[2] Internationally, China's Tianwen-1 mission achieved a successful landing with the Zhurong rover on May 14, 2021, in Utopia Planitia, marking the second nation to operate a rover on Mars and studying surface composition via ground-penetrating radar.^[4] The most recent U.S. landing, Perseverance on February 18, 2021, in Jezero Crater, focuses on astrobiology by collecting rock samples for future return to Earth and testing oxygen production technologies.^[2] Overall, of the approximately 20 attempted Mars landings as of 2025, ten have been fully successful, primarily by NASA, contributing to ongoing robotic exploration beginning in 1997 and transforming our understanding of Mars from a cold desert to a dynamic world with a watery past.^[2] These missions have informed future goals, such as sample return and human exploration, while highlighting the engineering feats required to navigate Mars's "seven minutes of terror" during EDL.^[3]

Entry, Descent, and Landing Technologies

Aerodynamic Deceleration Methods

Aerodynamic deceleration begins with the spacecraft's hypersonic entry into the Martian atmosphere at an altitude of approximately 125 km, where velocities range from 5 to 7 km/s depending on the mission trajectory and entry angle.^[5]^[6] This phase relies on atmospheric drag to rapidly reduce speed from orbital velocities, converting kinetic energy into heat and aerodynamic forces while protecting the payload from extreme thermal loads. The thin Martian atmosphere, with a scale height of about 11 km, necessitates precise entry conditions to achieve sufficient deceleration without excessive heating or skipping out of the atmosphere.^[5] Central to this process is the ablative heat shield on the forebody of the entry vehicle, which withstands peak temperatures up to approximately 1400°C by charring and eroding in a controlled manner to dissipate heat.^[7]^[8] Materials like Phenolic Impregnated Carbon Ablator (PICA), with a low density of approximately 0.27 g/cm³, form a carbonaceous char layer that insulates the underlying structure and re-radiates thermal energy, enabling survival during peak heating rates of 100-200 W/cm² for Mars entries.^[7] PICA's efficiency stems from its ability to pyrolyze and ablate without significant mass loss, as demonstrated in missions from Stardust to Mars Science Laboratory, where it reduced heat transfer to the vehicle by over 90% compared to non-ablative alternatives.^[7] As velocity drops to Mach 1.5-2.5 at altitudes of 10-12 km, supersonic parachutes deploy to further decelerate the vehicle, increasing drag area to slow descent from hundreds of meters per second to tens.^[9] The disk-gap-band (DGB) parachute design, featuring a central disk, annular gap, and outer band, provides stable inflation and high drag coefficients of 0.6-0.9 in the supersonic regime, depending on deployment conditions and forebody wake effects.^[9] This configuration minimizes canopy collapse and fluttering, achieving dynamic pressures of 200-800 Pa during deployment.^[9] The historical evolution of these methods traces back to early blunt-body designs, such as the 70-degree sphere-cone aeroshell used in the Viking missions of 1976, which optimized shock wave detachment for stable hypersonic flight and heat distribution.^[10] Pre-Viking wind tunnel and high-altitude drop tests in the 1960s validated DGB parachutes over alternatives like ringsail designs for Mach >2 stability, leading to their adoption as the standard.^[10] Modern iterations, seen in missions like Mars Pathfinder (1997) and Perseverance (2021), refined these with larger DGB canopies up to 21.5 m diameter and advanced materials like Kevlar, while retaining the blunt-body forebody for aerodynamic predictability; computational fluid dynamics has since enabled finer tuning of shapes to reduce peak loads by 10-20%.^[10] These advancements have increased parachute deployment reliability to over 95% across U.S. Mars landings.^[10]

Powered Descent and Precision Landing

Powered descent represents the final phase of Mars entry, descent, and landing, where retropropulsion systems ignite to arrest the vehicle's velocity after initial aerodynamic braking. These systems employ throttleable rocket engines to provide controlled deceleration in Mars' thin atmosphere and low gravity of 3.7 m/s², ensuring a soft touchdown. For instance, NASA's studies on supersonic retropropulsion highlight the need for engines with thrust-to-weight ratios of 80 to 90 and throttling capabilities down to 20% of full thrust to manage descent dynamics for payloads exceeding 10 metric tons.^[11] SpaceX's Starship concept utilizes Raptor engines, which throttle from 40% to 100% thrust, enabling precise retropropulsive maneuvers tailored to Mars' gravitational environment.^[12] Precision during powered descent relies on advanced guidance technologies, such as terrain-relative navigation (TRN), which integrates onboard cameras and LIDAR to map surface features in real time and avoid hazards like rocks or craters. TRN processes data at frame rates up to 20 Hz, generating 3D terrain maps with 7 cm range precision from altitudes as low as 500 meters, thereby reducing positional errors from hundreds of meters to tens of meters.^[13] This autonomous system compares descent imagery against preloaded high-resolution maps, allowing the vehicle to divert to safer sites without ground intervention. A notable implementation of powered descent control is the sky crane maneuver, employed by NASA's Curiosity and Perseverance rovers. In this technique, a rocket-powered descent stage hovers approximately 20 meters above the surface after parachute separation, lowering the rover via nylon tethers to enable a gentle touchdown on its wheels.^[14] Once sensors confirm contact, the tethers are pyrotechnically severed, and the descent stage ascends and crashes safely away to prevent contamination. This method accommodates the rovers' mass of over 900 kg while achieving landing accuracy within kilometers of the target. Over successive missions, precision landing errors have improved dramatically from several kilometers in early Viking landers to tens of meters in recent operations, facilitated by algorithms like convex optimization for trajectory planning. These algorithms formulate powered descent as a second-order cone program, optimizing propellant use while enforcing constraints such as glide slopes and pinpoint targeting, as demonstrated in simulations for Mars sites.^[15] For Perseverance, TRN further refined this to an ellipse of about 40 meters, boosting success probability to over 99%.^[16] Such advancements, building on guided entry techniques since Curiosity, enable landings in scientifically rich but hazardous terrains.^[17]

Innovations for Heavier Payloads

To enable Mars landings of payloads exceeding the approximately 1-tonne limit of legacy entry, descent, and landing (EDL) systems, supersonic retropropulsion (SRP) has emerged as a critical innovation, involving engine firings during the supersonic phase to augment drag and decelerate heavier vehicles. However, SRP introduces significant challenges, particularly the complex interactions between the vehicle's bow shock and the engine plumes, which can generate unsteady flowfields, alter aerodynamic stability, and increase structural loads on the spacecraft.^[18] For payloads over 10 tonnes, these systems require substantial propellant mass fractions, often approaching or exceeding 20-30% of the vehicle's initial mass during descent, with some configurations demanding up to 50% to achieve terminal velocities suitable for touchdown, depending on thrust-to-weight ratios and entry conditions.^[19]^[20] Hypersonic inflatable aerodynamic decelerators (HIADs) address the need for greater drag area by deploying lightweight, packable structures that inflate to form large aeroshells, significantly expanding the effective diameter beyond rigid heat shields. These devices can achieve diameters up to 20 meters, providing ballistic coefficients as low as 17-38 kg/m², which enables deceleration of payloads up to 20 tonnes while reducing peak heating and dynamic pressure during hypersonic entry.^[21] HIADs leverage toroidal or stacked-tube designs with flexible thermal protection systems, allowing for scalable drag without proportional mass penalties, and have been validated through ground and flight tests demonstrating structural integrity at Mach numbers above 3.^[21] For human-scale missions requiring 20-100 tonne landers, integrated EDL architectures combine HIADs with parachutes and SRP in nested sequences to progressively decelerate from orbital velocities. NASA's Low-Density Supersonic Decelerator (LDSD) program tested these concepts, including a 6-8 meter HIAD (SIAD) for initial supersonic drag augmentation from Mach 3.5 to 2, followed by a 30-meter supersonic parachute for subsonic transition, and SRP for final powered descent, enabling 2-3 tonne payloads with landing ellipses reduced to 3 km.^[22] This multi-stage approach mitigates the limitations of single decelerators, supporting access to elevated terrains like the Martian Southern Highlands while accommodating the mass and volume of crewed habitats.^[22] Fuel efficiency in these heavy-payload systems is enhanced by in-situ resource utilization (ISRU), which produces propellants on Mars to offset the high mass fractions needed for SRP and ascent. ISRU processes extract water from regolith and CO₂ from the atmosphere to generate methane (CH₄) and oxygen (O₂) via electrolysis and Sabatier reactions, potentially yielding 7-23 tonnes of propellant per mission and reducing the landed propellant mass by up to 95% compared to Earth-sourced alternatives.^[23] For example, systems requiring 52 kW power can fully fuel a Mars ascent vehicle, minimizing the initial EDL propellant load and enabling sustainable round-trip architectures for larger payloads.^[23]

Challenges and Risks

Atmospheric and Terrain Obstacles

The Martian atmosphere poses significant challenges for spacecraft entry, descent, and landing due to its low density, which is approximately 0.6% that of Earth's at sea level.^[24] This thin envelope, primarily composed of carbon dioxide with surface pressures around 6 mbar, generates insufficient aerodynamic drag to fully decelerate incoming vehicles traveling at hypersonic entry velocities of about 6 km/s.^[25] As a result, the limited drag necessitates hybrid deceleration strategies that combine atmospheric braking with other mechanisms to achieve safe landing speeds.^[26] Dust storms further complicate landings by drastically reducing visibility and altering atmospheric conditions. These events can become global, encircling the planet and lasting for weeks to months, particularly during southern spring and summer near perihelion.^[27] Winds driving these storms typically reach speeds of 14–32 m/s (50–115 km/h), lifting fine dust particles that obscure surface features essential for navigation and deposit additional mass—up to 0.4 g/m³—onto vehicles, potentially affecting stability and sensor performance.^[27] Such storms can make optical imaging unreliable, heightening the risk of imprecise site assessment during descent.^[28] The diverse Martian terrain introduces additional hazards, including widespread craters, scattered boulders up to 1 m in size, and slopes exceeding 15°. These features are prevalent across much of the surface, with rock abundances often reaching 5–20% in potential landing areas and steep inclines common in cratered or hilly regions.^[26] Approximately 50% of candidate sites exhibit sufficient variability in these elements to require active hazard avoidance measures during final approach.^[29] Variations in surface elevation and the planet's lower gravity (about 3.7 m/s²) also influence landing dynamics through their effects on atmospheric density and ballistic coefficients. Mars' atmospheric scale height of approximately 11 km—compared to Earth's 8 km—means density decreases more gradually with altitude, but higher-elevation sites (above -1 km relative to the datum) experience even thinner air, reducing drag and limiting accessible areas to roughly the northern hemisphere lowlands. These factors alter the ballistic coefficient (mass-to-drag area ratio), demanding precise trajectory adjustments to compensate for reduced gravitational pull and ensure controlled descent.

Engineering and Reliability Issues

Mars landers must withstand intense vibration and shock loads during entry, descent, and landing (EDL), with peak decelerations reaching 11.9–14.3 g's in missions like the Mars Science Laboratory (MSL).^[32] These forces arise from hypersonic atmospheric entry at velocities around 5.94 km/s, generating aeroacoustic noise, structural vibrations, and impulsive shocks from parachute deployment and engine ignition.^[32] To mitigate risks, engineers incorporate redundant structural designs, such as the MSL's aeroshell with a 70-degree sphere-cone shape and multiple descent engines, ensuring no single failure compromises the payload.^[32] Pyrotechnic separation mechanisms, critical for jettisoning the heatshield and backshell, demand reliabilities exceeding 99.9%, achieved through redundant firing circuits and heritage components tested to handle shock propagation without inducing avionics faults.^[33] Power and thermal management pose ongoing reliability challenges for surface operations, as Mars' diurnal temperature swings reach lows of -140°C at night, stressing electronics and batteries. Radioisotope thermoelectric generators (RTGs) provide stable power for missions like Curiosity and Perseverance, delivering hundreds of watts without reliance on sunlight, but require robust thermal insulation to maintain efficiency across extreme conditions. Solar arrays, used in landers like InSight, offer an alternative but suffer from dust accumulation, which typically reduces output by 0.2% per sol under nominal conditions, accumulating to 25–30% attenuation over a Mars year or up to 80% during global dust storms.^[34]^[35]^[36] Mitigation strategies include oversized panels and occasional wind-induced cleaning events, yet these systems demand fault-tolerant batteries to prevent power brownouts during low-output periods.^[37] Software autonomy is essential for EDL due to the one-way light-time delay of approximately 7 minutes between Earth and Mars, precluding real-time ground intervention and necessitating onboard fault detection, isolation, and recovery (FDIR) mechanisms. Fault-tolerant code architectures, such as those in MSL and Perseverance, use radiation-hardened processors to execute guidance algorithms that process large volumes of sensor data, including imagery for terrain-relative navigation (TRN), enabling hazard avoidance without human input.^[38] TRN systems match real-time images against pre-loaded maps derived from orbital surveys, handling data flows that support precise landing within 100 meters despite uncertainties in entry conditions.^[39] Cost-risk tradeoffs in lander design are highlighted by historical failures, such as the 1999 Mars Polar Lander (MPL), where vibrations from leg deployment generated spurious signals that mimicked touchdown, triggering premature engine shutdown and crash at about 22 m/s.^[40] This incident, costing $165 million, revealed vulnerabilities in sensor integration and emphasized the need for vibration-isolated avionics, rigorous environmental testing, and diversified risk postures to balance affordability with reliability in future missions.^[40] Subsequent designs, like those for MSL, incorporated extensive shock and vibration qualification, reducing single-point failure probabilities through modularity and parallel testing campaigns.^[32]

Communication Constraints

Communication with Mars landers is fundamentally limited by the vast interplanetary distance, resulting in a one-way light-time delay of 4 to 20 minutes depending on the orbital alignment of Earth and Mars. This delay, caused by the finite speed of light, renders real-time teleoperation impossible during critical phases like entry, descent, and landing (EDL), requiring spacecraft to operate with complete autonomy to execute pre-programmed maneuvers without ground intervention.^[41] To mitigate the challenges of direct communication, Mars landers primarily use orbiting relay spacecraft, such as the Mars Reconnaissance Orbiter (MRO), to forward data to Earth. These relays employ ultra-high frequency (UHF) links operating around 400 MHz, enabling data rates from 8 to 256 kbps between the lander and orbiter during overflights. However, during EDL, plasma-induced signal degradation and geometric constraints lead to blackouts or brownouts lasting up to about 70 seconds, during which no telemetry can be received, heightening reliance on onboard systems.^[42]^[43] Direct-to-Earth (DTE) communication serves as a backup, utilizing X-band frequencies (around 8.4 GHz) for low-rate transmissions directly to ground stations like those in NASA's Deep Space Network. Initial beacon signals confirming landing success are typically limited to rates up to 500 bits per second due to the extreme distance—often exceeding 200 million kilometers—and resulting free-space path losses on the order of 250 to 300 dB, which severely attenuate signals and restrict bandwidth.^[44]^[45] Over time, the infrastructure has evolved into the Mars Relay Network, an international collaboration involving multiple orbiters including MRO, Mars Odyssey, and MAVEN, which collectively provide more frequent and higher-capacity relay opportunities. Post-landing, this network supports burst data rates up to 2 Mbps for transmitting imagery and science data, dramatically improving throughput compared to early missions and enabling efficient return of large volumes of information from the Martian surface.^[46]^[47]

History of Mars Landings

Early Attempts (1960s-1970s)

The early efforts to land on Mars in the 1960s and 1970s were marked by a series of ambitious but challenging missions from both the Soviet Union and the United States, building on initial flyby successes that provided crucial reconnaissance data. In the 1960s, no spacecraft achieved a landing, but NASA's Mariner 4 mission in 1965 became the first to successfully fly by Mars, transmitting 21 close-up images that revealed a cratered, barren surface and informed future landing strategies.^[48] Prior Soviet attempts, such as the Mars 1960A and 1960B probes, failed shortly after launch, highlighting the technical hurdles of interplanetary travel during that era.^[49] These flybys laid the groundwork for surface missions but underscored the high risks, with an overall success rate for Mars attempts in this period approaching 50% when including partial achievements.^[50] The Soviet Union's Mars 2 and Mars 3 missions in 1971 represented the first dedicated attempts at landing. Launched on May 19 and May 28, 1971, respectively, Mars 2 arrived at Mars on November 27 and deployed its lander, which became the first human-made object to impact the Martian surface; however, the lander crashed due to high winds and insufficient deceleration, while the orbiter successfully entered orbit and relayed data for eight months.^[51] Mars 3, arriving on December 2, achieved the first soft landing on Mars in the Ptolemaeus region, but the lander transmitted only 20 seconds of data—likely a test pattern—before falling silent, possibly due to a dust storm or communication failure; its orbiter also operated successfully for months.^[52] These missions used basic entry, descent, and landing (EDL) systems featuring small parachutes for aerodynamic braking followed by solid rocket engines for terminal descent, resulting in large landing ellipses of 100-500 km due to limited guidance capabilities.^[1] The United States achieved the era's first fully successful Mars landings with the Viking program in 1976. Viking 1, launched August 20, 1975, entered Mars orbit on June 19, 1976, and conducted an 11-day orbital survey to certify a safe landing site before touching down in Chryse Planitia on July 20, marking the first intact spacecraft to operate on the surface and transmit detailed images and data.^[53] Viking 2, launched September 9, 1975, followed suit, orbiting on August 7, 1976, and landing in Utopia Planitia on September 3, providing complementary data from a northern site.^[54] Both landers employed similar EDL technology to the Soviet efforts—parachutes and solid rockets—achieving landing accuracies within broad ellipses of approximately 300 km by 100 km, and they far exceeded expectations by operating for over six years, conducting soil analyses, and imaging the surface extensively.^[55] These missions demonstrated the viability of long-term surface operations despite the era's primitive propulsion and navigation constraints.

Viking and Pathfinder Eras (1970s-1990s)

The Viking program marked the first successful soft landings on Mars, with Viking 1 touching down on July 20, 1976, in Chryse Planitia and Viking 2 on September 3, 1976, in Utopia Planitia.^[55] These missions relied on parachute and retrorocket systems for deceleration, followed by three legs for touchdown, enabling over six years of surface operations combined. The accompanying Viking orbiters played a crucial role in landing site vetting by imaging approximately 97% of the Martian surface at resolutions of 150 to 300 meters, allowing scientists to identify safe locations.^[56] Site selection prioritized flat terrains at low elevations, such as the -3 km datum in Chryse, to maximize aerodynamic braking from the thin atmosphere and minimize risks from slopes or boulders exceeding 3.5 degrees.^[57] These choices balanced engineering safety with scientific potential, including prospects for biological activity in regions with possible past water.^[57] Soviet efforts in this era faced setbacks, exemplified by the Mars 6 lander, which entered the Martian atmosphere on March 12, 1973, but lost contact shortly before its retrorockets fired, preventing a successful touchdown.^[58] Similarly, Mars 7, launched in July 1973, malfunctioned during a trajectory correction and missed Mars entirely, entering a heliocentric orbit.^[59] Across the 1970s and 1990s, Mars landing attempts achieved an overall success rate of about 40%, reflecting challenges in entry, descent, and landing technologies amid limited prior data.^[60] The Viking landers advanced surface science through in-situ soil analysis, using gas chromatograph-mass spectrometers to search for organic compounds indicative of life; initial results detected no organics above detection limits, though essential elements like carbon and nitrogen were present in the soil.^[55] Later reexaminations of the data suggested trace chlorinated hydrocarbons, possibly from terrestrial contaminants or Martian perchlorates, sparking ongoing debate about organic preservation on Mars.^[61] The orbiters also served as communication relays, forwarding lander data to Earth during direct-to-Earth windows.^[55] Building on Viking's static landers, the Mars Pathfinder mission in 1997 introduced mobility with the Sojourner rover, landing successfully on July 4 in Ares Vallis, an ancient outflow channel selected for its diverse flood-deposited rocks.^[62] Pathfinder employed an innovative airbag system—inflated to 17 feet in diameter—for cushioning impact, allowing the probe to bounce up to 15 times and skid about 1 km across the surface before settling.^[62] Sojourner, a 23-pound microrover equipped with an alpha proton X-ray spectrometer, demonstrated autonomous navigation and rock analysis, traversing approximately 100 meters over 83 sols to characterize soil composition and test rover technologies for future missions.^[63] Pathfinder's Atmospheric Structure Instrument and Meteorology Package measured surface winds averaging 0.4 to 30 meters per second, including diurnal variations and dust devil activity, which validated general circulation models of the Martian atmosphere and refined predictions for entry dynamics.^[64] These observations confirmed lower-than-expected wind shears during descent, aiding subsequent landing designs.^[62]

Modern Missions (2000s-2020s)

The modern era of Mars landings, beginning in the early 2000s, marked a resurgence in successful surface missions after setbacks in the late 1990s, with NASA's Mars Exploration Rovers (MER) Spirit and Opportunity pioneering extended rover operations. Launched in 2003 and landing in January 2004, both rovers employed an airbag-assisted bounce-and-roll system to touch down safely. Spirit arrived in Gusev Crater on January 4, potentially an ancient lakebed, and traversed 7.7 kilometers over six years before becoming immobile in 2010 due to wheel damage. Opportunity landed in Meridiani Planum on January 25, a site rich in iron oxide deposits hinting at a watery past, and remarkably operated for over 15 years until a planet-encircling dust storm ended communications in June 2018, during which it drove 45.16 kilometers and provided definitive evidence of liquid water's role in Mars' geological history.^[65]^[66] Building on these achievements, subsequent missions introduced innovative landing techniques and stationary landers to probe Mars' diverse environments. NASA's Phoenix lander, touching down on May 25, 2008, in the Vastitas Borealis northern plains using a parachute and retro-rocket system, confirmed the presence of subsurface water ice by excavating and analyzing soil samples with its robotic arm, revealing perchlorates that could serve as an energy source for potential microbial life.^[67] In 2012, the larger Curiosity rover demonstrated the sky crane maneuver—a rocket-powered descent stage lowering the vehicle on tethers—for a precise landing in Gale Crater on August 6, powered by a radioisotope thermoelectric generator (RTG) for long-term mobility exceeding solar-dependent predecessors. Over its mission, Curiosity has traversed more than 20 kilometers up Mount Sharp, analyzing rock layers to find chemical and mineral evidence of ancient habitable environments suitable for microbes.^[68]^[14] The 2010s and 2020s saw further advancements in stationary and mobile exploration, emphasizing interior science and sample return preparation. NASA's InSight lander arrived in Elysium Planitia on November 26, 2018, via a Phoenix-derived touchdown system, deploying a seismometer and heat probe to detect over 1,300 marsquakes and map the planet's rocky mantle structure, offering unprecedented insights into Mars' seismic activity and formation.^[69] Perseverance, landing in Jezero Crater on February 18, 2021, using an evolved sky crane for enhanced precision—including brief terrain-relative navigation—focuses on collecting rock cores for future Earth return, while investigating an ancient river delta for signs of past life; it has cached dozens of samples to date.^[70] Complementing these, China's Tianwen-1 mission achieved the nation's first Mars landing on May 14, 2021, in Utopia Planitia, deploying the Zhurong rover eight days later on May 22, 2021, to traverse 1.9 kilometers, identifying hydrated minerals and evidence of ancient liquid water flows through multispectral imaging and ground-penetrating radar.^[71] Despite these triumphs, failures persisted, underscoring the challenges of Mars entry, descent, and landing. In 1999, NASA's Mars Polar Lander crashed near the south pole on December 3 due to a premature engine shutdown triggered by a false signal from leg deployment, while its piggyback Deep Space 2 penetrators failed to transmit after impact, likely from inadequate drilling or communication issues.^[72] The European Space Agency's Beagle 2 lander, arriving December 25, 2003, in Isidis Planitia, lost contact post-separation, with investigations pointing to a likely failure in the airbag or solar panel deployment during descent.^[73] More recently, ESA's Schiaparelli demonstrator crashed in Meridiani Planum on October 19, 2016, after erroneous inertial measurements caused excessive spin-up, leading to an early parachute release and high-speed impact at over 300 km/h.^[74] These incidents, while setbacks, informed safer designs for later successes, highlighting the era's progress in rover endurance and scientific yield.

Planned Future Missions

The European Space Agency's (ESA) Rosalind Franklin rover, part of the ExoMars programme's second phase, is scheduled for launch in 2028, with a landing on Mars targeted for 2030.^[75]^[76] This six-wheeled rover will explore Oxia Planum, a site selected for its ancient clay-rich sediments that preserve potential signs of past microbial life.^[77] Equipped with a subsurface drill capable of reaching depths up to 2 meters, Rosalind Franklin aims to analyze organic molecules and minerals in unweathered rock layers, providing insights into Mars' habitability history.^[75] The mission includes a newly developed European landing platform built by Airbus to replace the previously canceled Russian contribution, ensuring independent descent and touchdown capabilities.^[78] As of November 2025, NASA and ESA's collaborative Mars Sample Return (MSR) mission faces significant challenges, including potential cancellation by the U.S. due to cost overruns, with NASA evaluating alternative architectures or scaled-back options to retrieve the approximately 30 samples collected by the Perseverance rover from Jezero Crater, marking the first such effort from another planet.^[79] The retrieval phase would involve a Mars ascent vehicle to launch the samples into orbit for capture by the Earth Return Orbiter, enabling detailed laboratory analysis on Earth for biosignatures and geological context.^[80] This multi-launch campaign builds on Perseverance's ongoing caching efforts, prioritizing scientific return while navigating engineering complexities like autonomous sample handling.^[81] SpaceX plans initial uncrewed Starship demonstrations to Mars starting in 2026, with additional flights potentially extending to 2028, to test entry, descent, and landing technologies for large-scale payloads.^[82] These missions aim to deliver over 100 metric tonnes of cargo per flight using supersonic retropropulsion for powered descent, paving the way for sustainable human exploration infrastructure.^[83] Elon Musk has indicated that while 2026 remains the target, a 2028 timeline is more realistic for the first uncrewed landings, followed by crewed missions in the early 2030s to establish a self-sustaining presence.^[83] The Starship system, powered by Raptor engines, emphasizes reusability and in-situ resource utilization to support long-duration stays. India's Indian Space Research Organisation (ISRO) has confirmed the Mangalyaan-2 mission for launch in 2030, shifting from earlier 2024-2025 windows due to technical and approval delays.^[84] This follow-on to the 2013 Mars Orbiter Mission will include an orbiter, lander, and rover to attempt India's first Mars surface touchdown, focusing on mineralogical and atmospheric studies.^[85] The lander-rover combination draws on experience from the Chandrayaan-3 lunar success, targeting sites with potential water ice evidence. Japan's Aerospace Exploration Agency (JAXA) Martian Moons eXploration (MMX) mission is set for launch in fiscal year 2026 aboard an H3 rocket, arriving at Mars in 2027 for Phobos sample return.^[86] While primarily focused on the moon's composition to understand solar system formation, MMX involves Mars orbital operations and a brief Phobos landing to collect up to 10 grams of regolith using a coring device.^[87] The spacecraft will deploy a small rover for surface analysis before departing in 2029 and returning samples to Earth in 2031, with international contributions from ESA, NASA, and France's CNES.^[88] China National Space Administration's (CNSA) Tianwen-3 mission plans dual launches around 2028 to achieve Mars sample return by 2031, emphasizing the search for ancient life signatures.^[89] The campaign includes orbiters, a lander, and ascent vehicle to collect and launch up to 500 grams of surface and subsurface material from multiple sites, potentially including volcanic regions.^[90] Open to international payloads, Tianwen-3 incorporates advanced rovers and drills for biosignature detection, operating for about 90 Martian days before return.^[91]

Landing Site Selection

Criteria and Processes

The selection of landing sites on Mars involves a rigorous evaluation of both scientific objectives and engineering constraints to ensure mission success and maximize knowledge gain. Primary criteria emphasize scientific value, such as the potential to investigate evidence of past habitability, including ancient river deltas or lake beds that may preserve biosignatures, while safety requirements prioritize low-elevation terrains, typically below 0 km but up to +1 km for some missions, to benefit from denser atmospheric braking during entry, descent, and landing (EDL).^[92] Additionally, sites must feature low average slopes (less than 3 degrees over 2-5 km scales) and minimal rock abundance (typically less than 10%) to avoid hazards during touchdown, with additional mobility criteria like slopes under 15 degrees for rover operations.^[92] These standards are outlined in NASA's planetary protection and mission planning guidelines, balancing the pursuit of high-priority geology with the need for reliable operations. International missions, such as ESA's ExoMars, adapt similar criteria with adjustments for their EDL systems, like allowing steeper local slopes up to 20 degrees for rover navigation.^[93] Risk assessment is integral to the process, focusing on defining a landing ellipse—varying by mission from tens of km in early efforts to under 10 km in recent ones like Perseverance's 7.7 km x 6.6 km—that achieves a hazard probability of less than 1% for safe touchdown.^[94] This involves probabilistic modeling of terrain features, wind patterns, and EDL dynamics to quantify uncertainties, ensuring that the selected footprint minimizes the likelihood of impacts with boulders, craters, or steep inclines. For instance, terrains with obstacles like those in rugged highlands are deprioritized to maintain low risk profiles. The assessment draws from frameworks developed by the Mars Exploration Program, which integrate statistical analyses to refine site viability. The site selection process is iterative, beginning with initial geophysical modeling based on orbital gravity and topography data, followed by integration of high-resolution imagery, such as the High Resolution Imaging Science Experiment (HiRISE) at 25 cm per pixel, to map potential hazards and scientific targets. Engineering simulations then evaluate EDL performance, including parachute deployment and powered descent, across candidate sites to confirm feasibility. This multi-stage approach, coordinated through workshops involving international scientists and engineers, refines the final choice from dozens of candidates to a single location. Over time, the process has evolved from the broad, reconnaissance-based searches of the Viking era in the 1970s, which relied on limited Mariner orbiter data for large, flat basins, to the precise pinpointing enabled by Perseverance in 2021, supported by decades of orbital assets like Mars Reconnaissance Orbiter. This progression reflects advancements in data volume and computational tools, allowing for more targeted selections that enhance both safety and scientific return.

Characterization Techniques

Characterization techniques for Mars landing sites rely on a suite of orbital instruments to assess surface composition, topography, and subsurface features, ensuring safe and scientifically valuable locations. Orbital remote sensing plays a central role, employing spectroscopy, altimetry, and radar to map potential hazards and resources. The Compact Reconnaissance Imaging Spectrometer for Mars (CRISM) aboard the Mars Reconnaissance Orbiter (MRO) uses visible and near-infrared spectroscopy to identify minerals indicative of past water activity, such as phyllosilicates and sulfates, which inform site habitability and geological context. For instance, CRISM data from the Mars Pathfinder landing site revealed olivine exposures in nearby craters, highlighting regional compositional variations atypical of the northern plains. Complementing this, the Mars Orbiter Laser Altimeter (MOLA) on Mars Global Surveyor provided global topography with a vertical resolution of approximately 1 meter and along-track spacing of 330 meters, enabling precise elevation models to evaluate slopes and elevation constraints for entry, descent, and landing (EDL) systems. Additionally, the Shallow Radar (SHARAD) instrument on MRO penetrates up to 1-2 kilometers into the subsurface to detect water ice deposits, as demonstrated in Utopia Planitia where radargrams identified extensive ice-rich layers that could serve as in-situ resources for future missions. High-resolution imaging further refines site characterization by providing detailed overviews and three-dimensional (3D) reconstructions of terrain hazards. The Context Camera (CTX) on MRO captures grayscale images at 6 meters per pixel across a 30-kilometer swath, offering broad contextual views of candidate sites to identify large-scale features like craters and dunes. CTX has achieved near-global coverage of Mars, imaging over 99% of the surface at least once, which supports initial hazard screening and correlation with higher-resolution data. For finer-scale analysis, the High Resolution Imaging Science Experiment (HiRISE) on MRO acquires images at 25-32 centimeters per pixel and generates stereo pairs to produce digital elevation models (DEMs) with 1-meter horizontal and sub-meter vertical accuracy. These stereo-derived 3D hazard maps quantify rock distributions, slopes exceeding 15-20 degrees, and other obstacles, as used in the Mars 2020 Perseverance landing site selection to ensure traversability within the 7.7-kilometer ellipse at Jezero Crater. Modeling and simulation integrate remote sensing data to predict EDL performance and support mission planning. The Mars Climate Database (MCD), developed by the Laboratoire de Météorologie Dynamique, provides atmospheric profiles including wind speeds and directions, which are essential for simulating entry trajectories and assessing gust-induced risks. MCD version 6.1, for example, enables high-fidelity trajectory modeling by incorporating small-scale gravity wave perturbations, aiding in the design of heat shields and parachutes for missions like ExoMars. Virtual reality (VR) tools enhance team training by allowing scientists and engineers to interactively explore reconstructed landing sites. NASA's OnSight software, for instance, uses mixed-reality headsets to overlay rover paths and instrument placements on photorealistic Mars terrains derived from HiRISE and CTX data, facilitating collaborative site evaluation and operational rehearsals without physical prototypes. Ground truthing from prior landers validates orbital datasets and refines risk models for future sites. The Opportunity rover's in-situ measurements in Meridiani Planum quantified rock abundance at approximately 10-15% in pebble-rich areas, informing probabilistic models for rover mobility hazards. These observations, combined with thermal inertia estimates from orbital surveys, helped calibrate landing site criteria for subsequent missions like Mars Science Laboratory, reducing uncertainties in rock-induced tip-over risks from earlier Viking-era estimates of 20-30% abundance. Such empirical data from Opportunity's decade-long traverse directly enhanced predictive algorithms for safe touchdown ellipses, emphasizing the iterative nature of characterization techniques.

Earth Analogs

Twinned Locations

Twinned locations refer to specific Earth sites selected as terrestrial analogs to replicate the environmental, geological, and atmospheric conditions encountered at Mars landing sites, enabling ground-based studies of landing dynamics, soil interactions, and surface processes. These analogs are chosen based on similarities in terrain, climate, and mineralogy to the Martian surface, facilitating the testing of rover mobility, instrument calibration, and hazard avoidance without direct access to Mars.^[95] Devon Island in Canada, particularly the Haughton Crater, serves as a primary analog for polar cold desert environments akin to those at high-latitude Mars landing sites. The 23-km-diameter impact crater, formed about 23 million years ago in a polar desert setting, features hyper-arid conditions, permafrost, and impact-related geology that mirror Martian polar terrains, with temperatures dropping to -30°C and minimal precipitation supporting studies of cold-weather landing challenges.^[96]^[97] The site's rugged, boulder-strewn landscapes and cryospheric features have been used to simulate dust and ice interactions during descent and touchdown.^[98] The Atacama Desert in Chile provides an analog for the dry, dusty soils prevalent at many equatorial and mid-latitude Mars landing zones. As the driest non-polar desert on Earth, with annual precipitation below 1 mm in its core regions, it replicates Mars' hyper-arid conditions, high UV radiation, and sulfate-rich soils, allowing tests of wheel-soil traction and abrasion in low-moisture regolith.^[99]^[100] Sites like the Yungay region exhibit salt and gypsum deposits similar to those detected by Mars rovers, aiding in the evaluation of landing gear performance on fine, cohesive dust layers.^[101] The Mars Desert Research Station (MDRS) in Utah, USA, analogs basalt-dominated terrains comparable to much of the Martian surface, particularly ancient volcanic plains. Located in a semi-arid badland with red-hued soils and eroded volcanic features, the site supports simulations of rover traversal over basaltic regolith, where iron-rich rocks and dust mimic the mechanical properties of Mars' Hesperian-aged crust.^[102]^[103] In Australia, the Pilbara region analogs the hematite-rich signatures observed at Meridiani Planum, the landing site of the Opportunity rover. The ancient craton's iron oxide concretions and layered sediments, formed in Archean wet-dry cycles, replicate the spherical hematite "blueberries" and evaporitic deposits on Mars, providing a venue for studying landing stability on hematite-cemented soils.^[104] Physical similarities between these sites and Mars extend to simulated atmospheric and regolith conditions. Low-pressure chambers, such as those at research facilities, replicate Mars' surface pressure of approximately 6 mbar using CO2-dominated atmospheres to test parachute deployment, airbag inflation, and dust dispersion during landing.^[105]^[106] Regolith simulants like JSC Mars-1A, derived from Hawaiian volcanic ash, match the grain size, density, and angularity of Martian soil for mechanical testing of lander footpads and rover wheels, ensuring accurate prediction of sinkage and traction.^[107]^[108] Specific pairings link historical Mars sites to Earth analogs for targeted validation. The Viking landing sites, characterized by basaltic plains and wind-sculpted features, are twinned with Icelandic basalts, where altered volcanic glasses and ventifacts in regions like Hvalfjordur provide analogs for soil composition and eolian processes observed in Viking imagery.^[95]^[109] Similarly, the Phoenix site's icy, polygonal terrains in the Martian Arctic are paired with the Antarctic Dry Valleys, such as Beacon Valley, where subsurface ice tables, periglacial polygons, and desiccated soils replicate the cold, low-humidity conditions for studying landing on ice-cemented ground.^[110]^[111]

Simulation and Research Applications

Earth analogs play a crucial role in field campaigns that simulate Mars landing and surface operations, enabling the testing of rover technologies and procedures under realistic constraints. NASA's Desert Research and Technology Studies (Desert RATS), conducted annually in the arid terrains of Arizona, focus on rover operations by deploying high-fidelity prototypes like the Field Integrated Design and Operations (FIDO) rover, which supported missions such as the Mars Exploration Rovers and Mars Science Laboratory. These campaigns incorporate simulated communication delays of up to 20 minutes one-way to mimic the Earth-Mars light-time lag, forcing crews to operate autonomously during traverses and geological sampling activities, such as drilling for subsurface samples and analyzing rock formations.^[112]^[113]^[114] Laboratory-based simulations complement field efforts by replicating Mars' environmental extremes for entry, descent, and landing (EDL) testing. Vacuum chambers at facilities like NASA's Jet Propulsion Laboratory allow engineers to evaluate parachute deployment, heat shield performance, and propulsion systems under low-pressure conditions approximating the Martian atmosphere at 6 millibars. Drop towers, such as those at NASA's Glenn Research Center, provide short-duration low-gravity simulations (around 0.38g for Mars) to study descent dynamics and landing gear impacts, validating models for powered descent phases in missions like Perseverance. Wind tunnels, including the Martian Surface Wind Tunnel (MARSWIT) at Ames Research Center, test dust storm effects on hardware; experiments expose solar panels to simulated Martian dust (basalt particles 5–100 µm) at velocities up to 124 m/s, revealing that storms can reduce transmittance by occluding surfaces, though self-cleaning occurs above 35 m/s wind speeds.^[115]^[116]^[117] Analog missions also offer training benefits for human crews, fostering psychological resilience and procedural proficiency through habitat mockups and suited operations. The Hawaii Space Exploration Analog and Simulation (HI-SEAS), located on Mauna Loa volcano, immerses crews in a 1,200-square-foot dome habitat simulating a Mars base, complete with resource-limited systems and isolation protocols. Participants don mockup spacesuits for extravehicular activities (EVAs), rehearsing geological surveys and equipment handling while enduring 20-minute communication delays, which enhance decision-making under autonomy. These simulations assess behavioral health via surveys and monitoring, revealing insights into team cohesion and stress management essential for long-duration Mars landings and stays.^[118]^[119] Research outputs from these analogs have directly informed Mars mission hardware validation. For instance, regolith simulants derived from Atacama Desert soils have been used to test in-situ resource utilization (ISRU) technologies for oxygen production from regolith, evaluating electrolysis efficiency and material compatibility in arid environments.^[120] Meanwhile, the Mars Oxygen In-Situ Resource Utilization Experiment (MOXIE) on Perseverance, which produces oxygen from atmospheric CO2, demonstrated the ability to generate 5–12 grams per hour during its operations on Mars, which concluded in 2023, paving the way for scalable propellant systems in future human landings.^[121]^[122]

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Mar 12, 2025 · Tianwen-3 aims to collect samples from Mars and, for the first time ever, deliver them to Earth. The primary scientific goal is the detection of ...
[90]
[PDF] Announcement of Opportunities for International Collaboration of ...
Tianwen-3, launching around 2028, aims to return Mars samples around 2030. International collaboration is open at system or payload level, with projects on ERO ...
[91]
Terrestrial analogs to wind‐related features at the Viking and ...
Jan 31, 2002 · [14] In many respects, parts of Iceland, including the region around the Askja volcanic center, provide an excellent analog for Mars. This area ...
[92]
Haughton Impact Crater | The Planetary Society
Jan 1, 2002 · From that standpoint, it promises to serve as a parallel to Mars. Although conditions on Devon Island remain significantly milder than those ...
[93]
Haughton-Mars Project (HMP)
Devon Island is home to Haughton Crater, a 20 km diameter meteorite impact crater that formed about 23 million years ago, during the Miocene. Research at HMP.
[94]
Crater serves as terrestrial analog for Martian impact structures
The Haughton impact crater site on Devon Island in Canada's. Nunavut Territory has been the focus of Mars analog studies because of the similarity of its.
[95]
Inhabited subsurface wet smectites in the hyperarid core of ... - Nature
Nov 5, 2020 · The Atacama Desert, particularly the Yungay region, is a well-known Martian analog because of its hyper-aridity and similar salt and ...
[96]
Prospecting the first Chilean Martian simulants from the Atacama ...
Mar 15, 2025 · Considering that Chile contains the Atacama Desert, a natural Mars analog terrain with organic soil analogs resembling the Martian arid ...
[97]
Subsurface Microbial Habitats in an Extreme Desert Mars-Analog ...
Feb 28, 2019 · Among those, the hyper-arid core of the Atacama Desert in Chile is widely regarded as a tractable Mars analog in the field of astrobiology.
[98]
Phyllosilicate and sulfate analogues to Mars mission landing sites
The Mars Desert Research Station (MDRS) is an analogue planetary surface habitat located in a remote area in south-central Utah. The MDRS offers a cost- ...
[99]
[PDF] Utah Desert Analogue Sites for Mars Research and Missions
Introduction: The geological site near Hanksville, Utah, contains a range of Mars analogue features relevant for geology and astrobiology studies.Missing: basalt | Show results with:basalt
[100]
The geology of Australian Mars analogue sites - ScienceDirect.com
The Mars analogue value of Australia's acid lakes, hypersaline embayments and mound spring complexes is highlighted along with the Pilbara region, where the ...
[101]
Simulation of the Martian dust aerosol at low wind speeds
Dec 19, 2002 · [31] A low-pressure wind tunnel has been constructed in order to simulate the Martian aerosol. It has been demonstrated to produce a well- ...Missing: analogs | Show results with:analogs
[102]
An environmental simulation wind tunnel for studying Aeolian ...
The mass density of the Martian atmosphere is significantly lower than that of earth, with measured surface pressure in the range 6–10 mbar. Significant ...Missing: analogs | Show results with:analogs
[103]
Exploration Science Projects | Lunar Regolith Simulants | JSC-1/1A
JSC-1/1A is recommended for geotechnical testing that involves loose simulant. JSC-1/1A is also recommended for ISRU testing that does not depend on iron redox ...
[104]
Characterizing The Mechanical Properties of JSC Mars-1A Martian ...
Mar 25, 2017 · Direct shear tests were run to test the shear strength and obtain the friction angle of the simulant, which provides more information regarding ...
[105]
Altered basaltic glass: A terrestrial analog to the soil of Mars
Our model for the formation of fine-grained Martian surface soil begins with eruptions of basaltic magma through ground ice, forming deposits of glassy tuff.
[106]
The high elevation Dry Valleys in Antarctica as analog sites for ...
Sep 1, 2013 · The Mars Phoenix spacecraft landed in the martian Arctic at 68.22°N latitude, 234.25°E longitude on 25 May 2008 (Smith et al., 2009). A main ...
[107]
Cold and dry processes in the Martian Arctic: Geomorphic ...
Nov 6, 2009 · We compare landforms observed at the Phoenix landing site to terrestrial analogs across microclimate zones in the Antarctic Dry Valleys.
[108]
NASA Desert RATS (Research and Technology Studies)
Feb 23, 2018 · Desert-RATS is a field campaign which conducts mission rover and extravehicular activity testing in the challenging and remote terrain of Arizona.
[109]
[PDF] NASA's Analog Missions - BryceTech
Sep 13, 2010 · For the 2010 Desert RATS mission, communication scenario ... The crew performed exploration tasks with a 20-minute-delayed signal to mission ...
[110]
[PDF] Human-in-the-Loop Operations over Time Delay: NASA Analog ...
The time delay studies focused on a mars delay of 20 minutes (OWLT) where communications was limited to twice a day. Half of the mission was executed with no ...
[111]
[PDF] Mars Entry, Descent, and Landing Challenges for Human Missions
This white paper introduces atmospheric entry, descent, and landing (EDL), discusses some of the unique challenges of Mars exploration, and provides insight ...
[112]
How (and why) do NASA researchers simulate microgravity on Earth?
Feb 12, 2024 · Important tools for simulating microgravity close to Earth include drop towers, parabolic flights, and suborbital flights.
[113]
[PDF] The Viability of Photovoltaics on the
The PV cells were run neutral, and also biased up to ±200 V dc. The winds on Mars were simulated using the Martian Surface Wind Tunnel (MARS WIT) at the. NASA ...
[114]
Mānoa: Second HI-SEAS Mars space analog study begins
Mar 28, 2014 · Likewise, crew members will suit up in mockup spacesuits whenever they step outside of the habitat. These “excursions” will be modeled after ...
[115]
Biobehavioral and psychosocial stress changes during three 8–12 ...
Dec 7, 2022 · In brief, HI-SEAS immerses 6-person crews of astronaut-like individuals in a Mars-like habitat on Mauna Loa volcano, isolated from the rest of ...Missing: suits mockups training
[116]
Review of space resources processing for Mars missions: Martian ...
This review provides the first comprehensive literature review of ISRU materials research employing Martian simulants.
[117]
MIT's MOXIE experiment reliably produces oxygen on Mars
Aug 31, 2022 · The MIT-led Mars Oxygen In-Situ Resource Utilization Experiment, or MOXIE, has been successfully making oxygen from the Red Planet's carbon-dioxide-rich ...Missing: Atacama analogs