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Mars - August 30 2021 - Flickr - Kevin M. Gill.png
Mars in true color, [lower-alpha 1] taken by the Emirates Mars Mission on August 30, 2021, when Mars was in northern solstice.
Adjectives Martian
Symbol Mars symbol (bold).svg
Orbital characteristics [1]
Epoch J2000
Aphelion 249261000 km
(154884000 mi; 1.66621 AU) [2]
Perihelion 206650000 km
(128410000 mi; 1.3814 AU) [2]
227939366 km
(141634956 mi; 1.52368055 AU) [3]
Eccentricity 0.0934 [2]
686.980 d
(1.88085  yr; 668.5991  sols) [2]
779.94 d
(2.1354  yr) [3]
Average orbital speed
24.07 km/s
(86700 km/h; 53800 mph) [2]
19.412° [2]
49.57854° [2]
2022-Jun-21 [5]
286.5° [3]
Satellites 2 (Phobos and Deimos)
Physical characteristics
Mean radius
3389.5 ± 0.2 km [lower-alpha 2] [6]
(2106.1 ± 0.1 mi)
Equatorial radius
3396.2 ± 0.1 km [lower-alpha 2] [6]
(2110.3 ± 0.1 mi; 0.533 Earths)
Polar radius
3376.2 ± 0.1 km [lower-alpha 2] [6]
(2097.9 ± 0.1 mi; 0.531 Earths)
Flattening 0.00589±0.00015 [5] [6]
144.37×106 km2 [7]
(5.574×107 sq mi; 0.284 Earths)
Volume 1.63118×1011 km3 [8]
(0.151 Earths)
Mass 6.4171×1023 kg [9]
(0.107 Earths)
Mean density
3.9335 g/cm3 [8]
(0.1421 lb/cu in)
3.72076 m/s2 [10]
(12.2072 ft/s2; 0.3794  g )
0.3644±0.0005 [9]
5.027 km/s
(18100 km/h; 11250 mph) [11]
1.02749125 d [12]
24h 39m 36s
1.025957 d
24h 37m 22.7s [8]
Equatorial rotation velocity
241 m/s
(870 km/h; 540 mph) [2]
25.19° to its orbital plane [2]
North pole right ascension
317.68143° [6]
21h 10m 44s
North pole declination
52.88650° [6]
Temperature 209 K (−64 °C) (blackbody temperature) [14]
Surface temp. minmeanmax
Celsius −110 °C [15] −60 °C [16] 35 °C [15]
Fahrenheit −166 °F [15] −80 °F [16] 95 °F [15]
Surface absorbed dose rate 8.8 μGy/h [17]
Surface equivalent dose rate 27 μSv/h [17]
−2.94 to +1.86 [18]
−1.5 [19]
3.5–25.1″ [2]
Atmosphere [2] [20]
Surface pressure
0.636 (0.4–0.87)  kPa
0.00628  atm
Composition by volume

    Mars is the fourth planet and the furthest terrestrial planet from the Sun. The reddish color of its surface is due to finely grained iron(III) oxide dust in the soil, giving it the nickname "the Red Planet". [21] [22] Mars has a second smallest radius among the planets in the Solar System at 3,389.5 km (2,106 mi) and has a surface gravity of 3.72 m/s2 (12.2 ft/s2), which is 38% of Earth's gravity. The Martian dichotomy can be clearly seen on the surface: on average, the terrain on Mars northern hemisphere is flatter and lower than Mars southern hemisphere. Mars has a very thin atmosphere made primarily of carbon dioxide and two irregularly shaped natural satellites: Phobos and Deimos.


    Geologically, Mars is fairly active, with dust devils sweeping across the landscape and marsquakes (Martian analog to earthquakes) trembling underneath the ground. The surface of Mars hosts a shield volcano (Olympus Mons) and one of the largest canyons in the Solar System (Valles Marineris). Mars's celestial motion is comparable to that of Earth, with a slightly eccentric orbit and an axial tilt only slightly greater than Earth's. This motion causes seasonal changes to the polar ice caps' coverage and temperature swings between −110 °C (−166 °F) to 35 °C (95 °F) on the surface. A Martian solar day (sol) is equal to 24.5 hours and a Martian solar year is equal to 1.88 Earth years.

    Like the other planets in the Solar System, Mars was formed 4.5 billion years ago. During the Noachian period from about 4.1 to 3.7 billion years ago, Mars's surface was marked by meteor impacts, valley formation, erosion, and the possible presence of water oceans. The Hesperian period from 3.7 to 3.2–2 billion years ago was dominated by widespread volcanic activity and flooding that carved immense outflow channels. The Amazonian period, which continues today, was marked by the wind's influence on geological processes. It is not yet known whether life has ever existed on Mars, though search for evidences of life on Mars is still ongoing.

    Mars is among the brightest objects in Earth's sky, and thus has been known from the ancient times. The Romans named it for the god of war, Mārs , as did Greeks (Ares) and Mesopotamians (Nergal), likely because its color suggested blood. Its high-contrast albedo features make it an attractive target for viewing with a telescope.

    Since the late 20th century, Mars has been explored by uncrewed spacecraft and rovers, with the first flyby by the Mariner 4 probe in 1965, the first Mars orbiter by the Mars 2 probe in 1971, and the first landing by the Viking 1 in 1976. As of 2023, there are at least 11 active probes orbiting Mars or at the Martian surface. Currently, Mars is an attractive target for the first future interplanetary human missions.

    Natural history

    Scientists have theorized that during the Solar System's formation, Mars was created as the result of a random process of run-away accretion of material from the protoplanetary disk that orbited the Sun. Mars has many distinctive chemical features caused by its position in the Solar System. Elements with comparatively low boiling points, such as chlorine, phosphorus, and sulfur, are much more common on Mars than Earth; these elements were probably pushed outward by the young Sun's energetic solar wind. [23]

    After the formation of the planets, all were subjected to the so-called "Late Heavy Bombardment". About 60% of the surface of Mars shows a record of impacts from that era, [24] [25] [26] whereas much of the remaining surface is probably underlain by immense impact basins caused by those events. There is evidence of an enormous impact basin in the Northern Hemisphere of Mars, spanning 10,600 by 8,500 kilometres (6,600 by 5,300 mi), or roughly four times the size of the Moon's South Pole – Aitken basin, the largest impact basin yet discovered. [27] This theory suggests that Mars was struck by a Pluto-sized body about four billion years ago. The event, thought to be the cause of the Martian hemispheric dichotomy, created the smooth Borealis basin that covers 40% of the planet. [28] [29]

    The geological history of Mars can be split into many periods, but the following are the three primary periods: [30] [31]

    Geological activity is still taking place on Mars. The Athabasca Valles is home to sheet-like lava flows created about 200  mya. Water flows in the grabens called the Cerberus Fossae occurred less than 20 Mya, indicating equally recent volcanic intrusions. [33] The Mars Reconnaissance Orbiter has captured images of avalanches. [34] [35]

    Physical characteristics

    Mars, Earth size comparison.jpg
    Comparison: Earth and Mars
    Animation (00:40) showing major features of Mars
    Video (01:28) showing how three NASA orbiters mapped the gravity field of Mars

    Mars is approximately half the diameter of Earth, with a surface area only slightly less than the total area of Earth's dry land. [2] Mars is less dense than Earth, having about 15% of Earth's volume and 11% of Earth's mass, resulting in about 38% of Earth's surface gravity. The red-orange appearance of the Martian surface is caused by ferric oxide, or rust. [36] It can look like butterscotch; [37] other common surface colors include golden, brown, tan, and greenish, depending on the minerals present. [37]

    Internal structure

    Like Earth, Mars has differentiated into a dense metallic core overlaid by less dense materials. [38] [39] Current models of its interior imply a core consisting primarily of iron and nickel with about 16–17% sulfur. [40] This iron(II) sulfide core is thought to be twice as rich in lighter elements as Earth's. [41] The core is surrounded by a silicate mantle that formed many of the tectonic and volcanic features on the planet, but it appears to be dormant. Besides silicon and oxygen, the most abundant elements in the Martian crust are iron, magnesium, aluminium, calcium, and potassium. The average thickness of the planet's crust is about 50 kilometres (31 mi), with a maximum thickness of 125 kilometres (78 mi). [41] By comparison, Earth's crust averages 40 kilometres (25 mi) in thickness. [42] [43]

    Mars is seismically active. In 2019, it was reported that InSight (now offline) had detected and recorded over 450 marsquakes and related events. [44] [45] In 2021 it was reported that based on eleven low-frequency marsquakes detected by the InSight lander the core of Mars was indeed liquid and had a radius of about 1830±40 km and a temperature around 1900–2000 K. The Martian core radius is abnormally large, accounting for more than half the radius of Mars and about half the size of the Earth's core. To this, it has been suggested that the core contains some amount of lighter elements like oxygen and hydrogen in addition to the iron–nickel alloy and about 15% of sulfur. [46] [47]

    The core of Mars is overlaid by the rocky mantle, which does not seem to have a thermally insulating layer analogous to the Earth's lower mantle. [47] The Martian mantle appears to be solid down to the depth of about 500 km, where the low-velocity zone (partially melted asthenosphere) begins. [48] Below the asthenosphere the velocity of seismic waves starts to grow again; and at the depth of about 1050 km lies the boundary of the transition zone extending down to the core. [47]

    Surface geology

    Curiosity's view of Martian soil and boulders after crossing the "Dingo Gap" sand dune PIA17944-MarsCuriosityRover-AfterCrossingDingoGapSanddune-20140209.jpg
    Curiosity 's view of Martian soil and boulders after crossing the "Dingo Gap" sand dune

    Mars is a terrestrial planet with a surface that consists of minerals containing silicon and oxygen, metals, and other elements that typically make up rock. The Martian surface is primarily composed of tholeiitic basalt, [49] although parts are more silica-rich than typical basalt and may be similar to andesitic rocks on Earth, or silica glass. Regions of low albedo suggest concentrations of plagioclase feldspar, with northern low albedo regions displaying higher than normal concentrations of sheet silicates and high-silicon glass. Parts of the southern highlands include detectable amounts of high-calcium pyroxenes. Localized concentrations of hematite and olivine have been found. [50] Much of the surface is deeply covered by finely grained iron(III) oxide dust. [51]

    Although Mars has no evidence of a structured global magnetic field, [52] observations show that parts of the planet's crust have been magnetized, suggesting that alternating polarity reversals of its dipole field have occurred in the past. This paleomagnetism of magnetically susceptible minerals is similar to the alternating bands found on Earth's ocean floors. One theory, published in 1999 and re-examined in October 2005 (with the help of the Mars Global Surveyor ), is that these bands suggest plate tectonic activity on Mars four billion years ago, before the planetary dynamo ceased to function and the planet's magnetic field faded. [53]

    The Phoenix lander returned data showing Martian soil to be slightly alkaline and containing elements such as magnesium, sodium, potassium and chlorine. These nutrients are found in soils on Earth. They are necessary for growth of plants. [54] Experiments performed by the lander showed that the Martian soil has a basic pH of 7.7, and contains 0.6% of the salt perchlorate, [55] [56] concentrations that are toxic to humans. [57] [58]

    Streaks are common across Mars and new ones appear frequently on steep slopes of craters, troughs, and valleys. The streaks are dark at first and get lighter with age. The streaks can start in a tiny area, then spread out for hundreds of metres. They have been seen to follow the edges of boulders and other obstacles in their path. The commonly accepted theories include that they are dark underlying layers of soil revealed after avalanches of bright dust or dust devils. [59] Several other explanations have been put forward, including those that involve water or even the growth of organisms. [60] [61]

    Radiation levels on the surface are on average 0.64 millisieverts of radiation per day, and significantly less than the radiation of 1.84 millisieverts per day or 22 millirads per day during the flight to and from Mars. [62] [63] For comparison the radiation levels in low Earth orbit, where Earth's space stations orbit, are around 0.5 millisieverts of radiation per day. [64] Hellas Planitia has the lowest surface radiation at about 0.342 millisieverts per day, featuring lava tubes southwest of Hadriacus Mons with potentially levels as low as 0.064 millisieverts per day. [65]

    Geography and features

    A MOLA-based topographic map showing highlands (red and orange) dominating the Southern Hemisphere of Mars, lowlands (blue) the northern. Volcanic plateaus delimit regions of the northern plains, whereas the highlands are punctuated by several large impact basins. Mars topography (MOLA dataset) with poles HiRes.jpg
    A MOLA-based topographic map showing highlands (red and orange) dominating the Southern Hemisphere of Mars, lowlands (blue) the northern. Volcanic plateaus delimit regions of the northern plains, whereas the highlands are punctuated by several large impact basins.

    Although better remembered for mapping the Moon, Johann Heinrich Mädler and Wilhelm Beer were the first areographers. They began by establishing that most of Mars's surface features were permanent and by more precisely determining the planet's rotation period. In 1840, Mädler combined ten years of observations and drew the first map of Mars. [66]

    Features on Mars are named from a variety of sources. Albedo features are named for classical mythology. Craters larger than roughly 50 km are named for deceased scientists and writers and others who have contributed to the study of Mars. Smaller craters are named for towns and villages of the world with populations of less than 100,000. Large valleys are named for the word "Mars" or "star" in various languages; smaller valleys are named for rivers. [67]

    Large albedo features retain many of the older names but are often updated to reflect new knowledge of the nature of the features. For example, Nix Olympica (the snows of Olympus) has become Olympus Mons (Mount Olympus). [68] The surface of Mars as seen from Earth is divided into two kinds of areas, with differing albedo. The paler plains covered with dust and sand rich in reddish iron oxides were once thought of as Martian "continents" and given names like Arabia Terra (land of Arabia) or Amazonis Planitia (Amazonian plain). The dark features were thought to be seas, hence their names Mare Erythraeum, Mare Sirenum and Aurorae Sinus. The largest dark feature seen from Earth is Syrtis Major Planum. [69] The permanent northern polar ice cap is named Planum Boreum. The southern cap is called Planum Australe. [70]

    Mars's equator is defined by its rotation, but the location of its Prime Meridian was specified, as was Earth's (at Greenwich), by choice of an arbitrary point; Mädler and Beer selected a line for their first maps of Mars in 1830. After the spacecraft Mariner 9 provided extensive imagery of Mars in 1972, a small crater (later called Airy-0), located in the Sinus Meridiani ("Middle Bay" or "Meridian Bay"), was chosen by Merton Davies, Harold Masursky, and Gérard de Vaucouleurs for the definition of 0.0° longitude to coincide with the original selection. [71] [72] [73]

    Because Mars has no oceans and hence no "sea level", a zero-elevation surface had to be selected as a reference level; this is called the areoid [74] of Mars, analogous to the terrestrial geoid. [75] Zero altitude was defined by the height at which there is 610.5  Pa (6.105  mbar ) of atmospheric pressure. [76] This pressure corresponds to the triple point of water, and it is about 0.6% of the sea level surface pressure on Earth (0.006 atm). [77]

    For mapping purposes, the United States Geological Survey divides the surface of Mars into thirty cartographic quadrangles, each named for a classical albedo feature it contains. [78] In April 2023, The New York Times reported an updated global map of Mars based on images from the Hope spacecraft. [79] A related, but much more detailed, global Mars map was released by NASA on 16 April 2023. [80]


    Picture of the largest volcano on Mars, Olympus Mons. It is approximately 550 km (340 mi) across. Olympus Mons - ESA Mars Express - Flickr - Andrea Luck.png
    Picture of the largest volcano on Mars, Olympus Mons. It is approximately 550 km (340 mi) across.

    The vast upland region Tharsis contain several extinct volcanoes, which include the shield volcano Olympus Mons (Mount Olympus). The edifice is over 600 km (370 mi) wide. [81] [82] Because the mountain is so large, with complex structure at its edges, giving a defnite height to it is difficult. Its local relief, from the foot of the cliffs which form its northwest margin to its peak, is over 21 km (13 mi), [82] a little over twice the height of Mauna Kea as measured from its base on the ocean floor. The total elevation change from the plains of Amazonis Planitia, over 1,000 km (620 mi) to the northwest, to the summit approaches 26 km (16 mi), [83] roughly three times the height of Mount Everest, which in comparison stands at just over 8.8 kilometres (5.5 mi). Consequently, Olympus Mons is either the tallest or second-tallest mountain in the Solar System; the only known mountain which might be taller is the Rheasilvia peak on the asteroid Vesta, at 20–25 km (12–16 mi). [84]

    Impact topography

    The dichotomy of Martian topography is striking: northern plains flattened by lava flows contrast with the southern highlands, pitted and cratered by ancient impacts. It is possible that, four billion years ago, the Northern Hemisphere of Mars was struck by an object one-tenth to two-thirds the size of Earth's Moon. If this is the case, the Northern Hemisphere of Mars would be the site of an impact crater 10,600 by 8,500 kilometres (6,600 by 5,300 mi) in size, or roughly the area of Europe, Asia, and Australia combined, surpassing Utopia Planitia and the Moon's South Pole–Aitken basin as the largest impact crater in the Solar System. [85] [86] [87]

    Mars is scarred by a number of impact craters: a total of 43,000 craters with a diameter of 5 kilometres (3.1 mi) or greater have been found. [88] The largest exposed crater is Hellas, which is 2,300 kilometres (1,400 mi) wide and 7,000 metres (23,000 ft) deep, and is a light albedo feature clearly visible from Earth. [89] [90] There are other notable impact features, such as Argyre, which is around 1,800 kilometres (1,100 mi) in diameter, [91] and Isidis, which is around 1,500 kilometres (930 mi) in diameter. [92] Due to the smaller mass and size of Mars, the probability of an object colliding with the planet is about half that of Earth. Mars is located closer to the asteroid belt, so it has an increased chance of being struck by materials from that source. Mars is more likely to be struck by short-period comets, i.e., those that lie within the orbit of Jupiter. [93]

    Martian craters can have a morphology that suggests the ground became wet after the meteor impacted. [94]

    Tectonic sites

    Valles Marineris, taken by the Viking 1 probe Mars Valles Marineris.jpeg
    Valles Marineris, taken by the Viking 1 probe

    The large canyon, Valles Marineris (Latin for "Mariner Valleys", also known as Agathodaemon in the old canal maps [95] ), has a length of 4,000 kilometres (2,500 mi) and a depth of up to 7 kilometres (4.3 mi). The length of Valles Marineris is equivalent to the length of Europe and extends across one-fifth the circumference of Mars. By comparison, the Grand Canyon on Earth is only 446 kilometres (277 mi) long and nearly 2 kilometres (1.2 mi) deep. Valles Marineris was formed due to the swelling of the Tharsis area, which caused the crust in the area of Valles Marineris to collapse. In 2012, it was proposed that Valles Marineris is not just a graben, but a plate boundary where 150 kilometres (93 mi) of transverse motion has occurred, making Mars a planet with possibly a two-tectonic plate arrangement. [96] [97]

    Holes and caves

    Images from the Thermal Emission Imaging System (THEMIS) aboard NASA's Mars Odyssey orbiter have revealed seven possible cave entrances on the flanks of the volcano Arsia Mons. [98] The caves, named after loved ones of their discoverers, are collectively known as the "seven sisters". [99] Cave entrances measure from 100 to 252 metres (328 to 827 ft) wide and they are estimated to be at least 73 to 96 metres (240 to 315 ft) deep. Because light does not reach the floor of most of the caves, they may extend much deeper than these lower estimates and widen below the surface. "Dena" is the only exception; its floor is visible and was measured to be 130 metres (430 ft) deep. The interiors of these caverns may be protected from micrometeoroids, UV radiation, solar flares and high energy particles that bombard the planet's surface. [100] [101]


    Edge-on view of Mars atmosphere by Viking 1 probe Mars atmosphere.jpg
    Edge-on view of Mars atmosphere by Viking 1 probe

    Mars lost its magnetosphere 4 billion years ago, [102] possibly because of numerous asteroid strikes, [103] so the solar wind interacts directly with the Martian ionosphere, lowering the atmospheric density by stripping away atoms from the outer layer. [104] Both Mars Global Surveyor and Mars Express have detected ionised atmospheric particles trailing off into space behind Mars, [102] [105] and this atmospheric loss is being studied by the MAVEN orbiter. Compared to Earth, the atmosphere of Mars is quite rarefied. Atmospheric pressure on the surface today ranges from a low of 30  Pa (0.0044  psi ) on Olympus Mons to over 1,155 Pa (0.1675 psi) in Hellas Planitia, with a mean pressure at the surface level of 600 Pa (0.087 psi). [106] The highest atmospheric density on Mars is equal to that found 35 kilometres (22 mi) [107] above Earth's surface. The resulting mean surface pressure is only 0.6% of Earth's 101.3 kPa (14.69 psi). The scale height of the atmosphere is about 10.8 kilometres (6.7 mi), [108] which is higher than Earth's 6 kilometres (3.7 mi), because the surface gravity of Mars is only about 38% of Earth's. [109]

    The atmosphere of Mars consists of about 96% carbon dioxide, 1.93% argon and 1.89% nitrogen along with traces of oxygen and water. [2] [110] [104] The atmosphere is quite dusty, containing particulates about 1.5 µm in diameter which give the Martian sky a tawny color when seen from the surface. [111] It may take on a pink hue due to iron oxide particles suspended in it. [21] The concentration of methane in the Martian atmosphere fluctuates from about 0.24 ppb during the northern winter to about 0.65 ppb during the summer. [112] Estimates of its lifetime range from 0.6 to 4 years, [113] [114] so its presence indicates that an active source of the gas must be present. Methane could be produced by non-biological process such as serpentinization involving water, carbon dioxide, and the mineral olivine, which is known to be common on Mars, [115] or by Martian life. [116]

    Escaping atmosphere on Mars (carbon, oxygen, and hydrogen) by MAVEN in UV PIA18613-MarsMAVEN-Atmosphere-3UV-Views-20141014.jpg
    Escaping atmosphere on Mars (carbon, oxygen, and hydrogen) by MAVEN in UV

    Compared to Earth, its higher concentration of atmospheric CO2 and lower surface pressure may be why sound is attenuated more on Mars, where natural sources are rare apart from the wind. Using acoustic recordings collected by the Perseverance rover, researchers concluded that the speed of sound there is approximately 240 m/s for frequencies below 240 Hz, and 250 m/s for those above. [118] [119]

    Auroras have been detected on Mars. [120] [121] [122] Because Mars lacks a global magnetic field, the types and distribution of auroras there differ from those on Earth; [123] rather than being mostly restricted to polar regions as is the case on Earth, a Martian aurora can encompass the planet. [124] In September 2017, NASA reported radiation levels on the surface of the planet Mars were temporarily doubled, and were associated with an aurora 25 times brighter than any observed earlier, due to a massive, and unexpected, solar storm in the middle of the month. [124] [125]


    Mars without (on left) and with a global dust storm in July 2001 (on right), as seen by the Hubble Space Telescope Mars Before and During Global Dust Storm.jpg
    Mars without (on left) and with a global dust storm in July 2001 (on right), as seen by the Hubble Space Telescope

    Of all the planets in the Solar System, the seasons of Mars are the most Earth-like, due to the similar tilts of the two planets' rotational axes. The lengths of the Martian seasons are about twice those of Earth's because Mars's greater distance from the Sun leads to the Martian year being about two Earth years long. Martian surface temperatures vary from lows of about −110 °C (−166 °F) to highs of up to 35 °C (95 °F) in equatorial summer. [15] The wide range in temperatures is due to the thin atmosphere which cannot store much solar heat, the low atmospheric pressure (about 1% that of the atmosphere of Earth), and the low thermal inertia of Martian soil. [126] The planet is 1.52 times as far from the Sun as Earth, resulting in just 43% of the amount of sunlight. [127] [128]

    If Mars had an Earth-like orbit, its seasons would be similar to Earth's because its axial tilt is similar to Earth's. The comparatively large eccentricity of the Martian orbit has a significant effect. Mars is near perihelion when it is summer in the Southern Hemisphere and winter in the north, and near aphelion when it is winter in the Southern Hemisphere and summer in the north. As a result, the seasons in the Southern Hemisphere are more extreme and the seasons in the northern are milder than would otherwise be the case. The summer temperatures in the south can be warmer than the equivalent summer temperatures in the north by up to 30 °C (54 °F). [129]

    Mars has the largest dust storms in the Solar System, reaching speeds of over 160 km/h (100 mph). These can vary from a storm over a small area, to gigantic storms that cover the entire planet. They tend to occur when Mars is closest to the Sun, and have been shown to increase the global temperature. [130]


    The ice-filled Korolev crater near Mars's north pole is estimated to hold about 2,200 km (530 cu mi), comparable in volume to the Great Bear Lake. Plan view of Korolev crater.jpg
    The ice-filled Korolev crater near Mars's north pole is estimated to hold about 2,200 km (530 cu mi), comparable in volume to the Great Bear Lake.

    Water in its liquid form cannot exist on the surface of Mars due to low atmospheric pressure, which is less than 1% that of Earth, [131] except at the lowest of elevations for short periods. [39] [132] The two polar ice caps appear to be made largely of water. [133] [134] The volume of water ice in the south polar ice cap, if melted, would be enough to cover the entire surface of the planet with a depth of 11 metres (36 ft). [135] Large quantities of ice are thought to be trapped within the thick cryosphere of Mars. Radar data from Mars Express and the Mars Reconnaissance Orbiter (MRO) show large quantities of ice at both poles, [136] [137] and at middle latitudes. [138] The Phoenix lander directly sampled water ice in shallow Martian soil on 31 July 2008. [139]

    Landforms visible on Mars strongly suggest that liquid water has existed on the planet's surface. Huge linear swathes of scoured ground, known as outflow channels, cut across the surface in about 25 places. These are thought to be a record of erosion caused by the catastrophic release of water from subsurface aquifers, though some of these structures have been hypothesized to result from the action of glaciers or lava. [140] [141] One of the larger examples, Ma'adim Vallis, is 700 kilometres (430 mi) long, much greater than the Grand Canyon, with a width of 20 kilometres (12 mi) and a depth of 2 kilometres (1.2 mi) in places. It is thought to have been carved by flowing water early in Mars's history. [142] The youngest of these channels are thought to have formed only a few million years ago. [143]

    Elsewhere, particularly on the oldest areas of the Martian surface, finer-scale, dendritic networks of valleys are spread across significant proportions of the landscape. Features of these valleys and their distribution strongly imply that they were carved by runoff resulting from precipitation in early Mars history. Subsurface water flow and groundwater sapping may play important subsidiary roles in some networks, but precipitation was probably the root cause of the incision in almost all cases. [144]

    Along crater and canyon walls, there are thousands of features that appear similar to terrestrial gullies. The gullies tend to be in the highlands of the Southern Hemisphere and to face the Equator; all are poleward of 30° latitude. A number of authors have suggested that their formation process involves liquid water, probably from melting ice, [145] [146] although others have argued for formation mechanisms involving carbon dioxide frost or the movement of dry dust. [147] [148] No partially degraded gullies have formed by weathering and no superimposed impact craters have been observed, indicating that these are young features, possibly still active. [146] Other geological features, such as deltas and alluvial fans preserved in craters, are further evidence for warmer, wetter conditions at an interval or intervals in earlier Mars history. [149] Such conditions necessarily require the widespread presence of crater lakes across a large proportion of the surface, for which there is independent mineralogical, sedimentological and geomorphological evidence. [150] Further evidence that liquid water once existed on the surface of Mars comes from the detection of specific minerals such as hematite and goethite, both of which sometimes form in the presence of water. [151]

    Polar caps

    Martian north polar cap.jpg
    North polar early summer water ice cap (1999); a seasonal layer of carbon dioxide ice forms in winter and disappears in summer.
    South Polar Cap of Mars during Martian South summer 2000.jpg
    South polar midsummer ice cap (2000); the south cap has a permanent carbon dioxide ice cap covered with water ice. [152]

    Mars has two permanent polar ice caps. During a pole's winter, it lies in continuous darkness, chilling the surface and causing the deposition of 25–30% of the atmosphere into slabs of CO2 ice (dry ice). [153] When the poles are again exposed to sunlight, the frozen CO2 sublimes. These seasonal actions transport large amounts of dust and water vapor, giving rise to Earth-like frost and large cirrus clouds. Clouds of water-ice were photographed by the Opportunity rover in 2004. [154]

    The caps at both poles consist primarily of water ice. Frozen carbon dioxide accumulates as a comparatively thin layer about one metre thick on the north cap in the northern winter only, whereas the south cap has a permanent dry ice cover about eight metres thick. This permanent dry ice cover at the south pole is peppered by flat floored, shallow, roughly circular pits, which repeat imaging shows are expanding in some places and retreating in others. [155] The northern polar cap has a diameter of about 1,000 kilometres (620 mi), [156] and contains about 1.6 million cubic kilometres (5.7×1016 cu ft) of ice, which, if spread evenly on the cap, would be 2 kilometres (1.2 mi) thick. [157] (This compares to a volume of 2.85 million cubic kilometres (1.01×1017 cu ft) for the Greenland ice sheet.) The southern polar cap has a diameter of 350 kilometres (220 mi) and a thickness of 3 kilometres (1.9 mi). [158] The total volume of ice in the south polar cap plus the adjacent layered deposits has been estimated at 1.6 million cubic km. [159] Both polar caps show spiral troughs, which recent analysis of SHARAD ice penetrating radar has shown are a result of katabatic winds that spiral due to the Coriolis effect. [160] [161]

    The seasonal frosting of areas near the southern ice cap results in the formation of transparent 1-metre-thick slabs of dry ice above the ground. With the arrival of spring, sunlight warms the subsurface and pressure from subliming CO2 builds up under a slab, elevating and ultimately rupturing it. This leads to geyser-like eruptions of CO2 gas mixed with dark basaltic sand or dust. This process is rapid, observed happening in the space of a few days, weeks or months, a rate of change rather unusual in geology – especially for Mars. The gas rushing underneath a slab to the site of a geyser carves a spiderweb-like pattern of radial channels under the ice, the process being the inverted equivalent of an erosion network formed by water draining through a single plughole. [162] [163]

    Observations and findings of water evidence

    Water equivalent hydrogen abundance in the lower latitudes of Mars 01.jpg
    Water equivalent hydrogen abundance in the high latitudes of Mars.jpg
    Proportion of water ice present in the upper meter of the Martian surface for lower (top) and higher (bottom) latitudes

    In 2004, Opportunity detected the mineral jarosite. This forms only in the presence of acidic water, showing that water once existed on Mars. [164] [165] The Spirit rover found concentrated deposits of silica in 2007 that indicated wet conditions in the past, and in December 2011, the mineral gypsum, which also forms in the presence of water, was found on the surface by NASA's Mars rover Opportunity. [166] [167] [168] It is estimated that the amount of water in the upper mantle of Mars, represented by hydroxyl ions contained within Martian minerals, is equal to or greater than that of Earth at 50–300 parts per million of water, which is enough to cover the entire planet to a depth of 200–1,000 metres (660–3,280 ft). [169] [170]

    On 18 March 2013, NASA reported evidence from instruments on the Curiosity rover of mineral hydration, likely hydrated calcium sulfate, in several rock samples including the broken fragments of "Tintina" rock and "Sutton Inlier" rock as well as in veins and nodules in other rocks like "Knorr" rock and "Wernicke" rock. [171] [172] Analysis using the rover's DAN instrument provided evidence of subsurface water, amounting to as much as 4% water content, down to a depth of 60 centimetres (24 in), during the rover's traverse from the Bradbury Landing site to the Yellowknife Bay area in the Glenelg terrain. [171] In September 2015, NASA announced that they had found strong evidence of hydrated brine flows in recurring slope lineae, based on spectrometer readings of the darkened areas of slopes. [173] [174] [175] These streaks flow downhill in Martian summer, when the temperature is above −23° Celsius, and freeze at lower temperatures. [176] These observations supported earlier hypotheses, based on timing of formation and their rate of growth, that these dark streaks resulted from water flowing just below the surface. [177] However, later work suggested that the lineae may be dry, granular flows instead, with at most a limited role for water in initiating the process. [178] A definitive conclusion about the presence, extent, and role of liquid water on the Martian surface remains elusive. [179] [180]

    Researchers suspect much of the low northern plains of the planet were covered with an ocean hundreds of meters deep, though this theory remains controversial. [181] In March 2015, scientists stated that such an ocean might have been the size of Earth's Arctic Ocean. This finding was derived from the ratio of protium to deuterium in the modern Martian atmosphere compared to that ratio on Earth. The amount of Martian deuterium is eight times the amount that exists on Earth, suggesting that ancient Mars had significantly higher levels of water. Results from the Curiosity rover had previously found a high ratio of deuterium in Gale Crater, though not significantly high enough to suggest the former presence of an ocean. Other scientists caution that these results have not been confirmed, and point out that Martian climate models have not yet shown that the planet was warm enough in the past to support bodies of liquid water. [182] Near the northern polar cap is the 81.4 kilometres (50.6 mi) wide Korolev Crater, which the Mars Express orbiter found to be filled with approximately 2,200 cubic kilometres (530 cu mi) of water ice. [183]

    In November 2016, NASA reported finding a large amount of underground ice in the Utopia Planitia region. The volume of water detected has been estimated to be equivalent to the volume of water in Lake Superior (which is 12,100 cubic kilometres [184] ). [185] [186] During observations from 2018 through 2021, the ExoMars Trace Gas Orbiter spotted indications of water, probably subsurface ice, in the Valles Marineris canyon system. [187]

    Orbit and rotation

    Orbit of Mars and other Inner Solar System planets Solar system orrery inner planets.gif
    Orbit of Mars and other Inner Solar System planets

    Mars's average distance from the Sun is roughly 230 million km (143 million mi), and its orbital period is 687 (Earth) days. The solar day (or sol) on Mars is only slightly longer than an Earth day: 24 hours, 39 minutes, and 35.244 seconds. [188] A Martian year is equal to 1.8809 Earth years, or 1 year, 320 days, and 18.2 hours. [2]

    The axial tilt of Mars is 25.19° relative to its orbital plane, which is similar to the axial tilt of Earth. [2] As a result, Mars has seasons like Earth, though on Mars they are nearly twice as long because its orbital period is that much longer. In the present day epoch, the orientation of the north pole of Mars is close to the star Deneb. [20]

    Mars has a relatively pronounced orbital eccentricity of about 0.09; of the seven other planets in the Solar System, only Mercury has a larger orbital eccentricity. It is known that in the past, Mars has had a much more circular orbit. At one point, 1.35 million Earth years ago, Mars had an eccentricity of roughly 0.002, much less than that of Earth today. [189] Mars's cycle of eccentricity is 96,000 Earth years compared to Earth's cycle of 100,000 years. [190]

    Mars approaches Earth in a synodic period of 779.94 days. Earth orbits the Sun the closest to Mars's orbit around the Sun, and Mars orbit is the second closest to Earth after the orbit of Venus. Therefore, their closest approaches, the inferior conjunctions, are the second closest for Earth after those with Venus, and the closest for Mars to any other planet. The gravitational potential difference, and thus the delta-v needed to transfer between Mars and Earth is the second lowest for Earth and the lowest for Mars to any other planet, while transfers can possibly be optimized with Venus flybys. [191] [192]


    Phobos colour 2008.jpg
    Enhanced-color HiRISE image of Phobos, showing a series of mostly parallel grooves and crater chains, with Stickney crater at right
    Enhanced-color HiRISE image of Deimos (not to scale), showing its smooth blanket of regolith

    Mars has two relatively small (compared to Earth's) natural moons, Phobos (about 22 kilometres (14 mi) in diameter) and Deimos (about 12 kilometres (7.5 mi) in diameter), which orbit close to the planet. The origin of both moons is unclear, although a popular theory states that they were asteroids captured into Martian orbit. [193]

    Both satellites were discovered in 1877 by Asaph Hall and were named after the characters Phobos (the deity of panic and fear) and Deimos (the deity of terror and dread), twins from Greek mythology who accompanied their father Ares, god of war, into battle. [194] Mars was the Roman equivalent to Ares. In modern Greek, the planet retains its ancient name Ares (Aris: Άρης). [86]

    From the surface of Mars, the motions of Phobos and Deimos appear different from that of the Earth's satellite, the Moon. Phobos rises in the west, sets in the east, and rises again in just 11 hours. Deimos, being only just outside synchronous orbit  where the orbital period would match the planet's period of rotation rises as expected in the east, but slowly. Because the orbit of Phobos is below synchronous altitude, tidal forces from Mars are gradually lowering its orbit. In about 50 million years, it could either crash into Mars's surface or break up into a ring structure around the planet. [195]

    The origin of the two satellites is not well understood. Their low albedo and carbonaceous chondrite composition have been regarded as similar to asteroids, supporting a capture theory. The unstable orbit of Phobos would seem to point toward a relatively recent capture. But both have circular orbits, near the equator that is unusual for captured objects and the required capture dynamics are complex. Accretion early in the history of Mars is plausible, but would not account for a composition resembling asteroids rather than Mars itself, if that is confirmed. [196] Mars may have yet-undiscovered moons, smaller than 50 to 100 metres (160 to 330 ft) in diameter, and a dust ring is predicted to exist between Phobos and Deimos. [197]

    A third possibility for their origin as satellites of Mars is the involvement of a third body or a type of impact disruption. More-recent lines of evidence for Phobos having a highly porous interior, [198] and suggesting a composition containing mainly phyllosilicates and other minerals known from Mars, [199] point toward an origin of Phobos from material ejected by an impact on Mars that reaccreted in Martian orbit, similar to the prevailing theory for the origin of Earth's satellite. Although the visible and near-infrared (VNIR) spectra of the moons of Mars resemble those of outer-belt asteroids, the thermal infrared spectra of Phobos are reported to be inconsistent with chondrites of any class. [199] It is also possible that Phobos and Deimos are fragments of an older moon, formed by debris from a large impact on Mars, and then destroyed by a more recent impact upon the satellite. [200]

    Human observations and exploration

    The history of observations of Mars is marked by the oppositions of Mars when the planet is closest to Earth and hence is most easily visible, which occur every couple of years. Even more notable are the perihelic oppositions of Mars, which are distinguished because Mars is close to perihelion, making it even closer to Earth. [201]

    Ancient and medieval observations

    The ancient Sumerians named Mars Nergal, the god of war and plague. During Sumerian times, Nergal was a minor deity of little significance, but, during later times, his main cult center was the city of Nineveh. [202] In Mesopotamian texts, Mars is referred to as the "star of judgement of the fate of the dead." [203] The existence of Mars as a wandering object in the night sky was also recorded by the ancient Egyptian astronomers and, by 1534 BCE, they were familiar with the retrograde motion of the planet. [204] By the period of the Neo-Babylonian Empire, the Babylonian astronomers were making regular records of the positions of the planets and systematic observations of their behavior. For Mars, they knew that the planet made 37 synodic periods, or 42 circuits of the zodiac, every 79 years. They invented arithmetic methods for making minor corrections to the predicted positions of the planets. [205] [206] In Ancient Greece, the planet was known as Πυρόεις . [207] Commonly, the Greek name for the planet now referred to as Mars, was Ares. It was the Romans who named the planet Mars, for their god of war, often represented by the sword and shield of the planet's namesake. [208]

    In the fourth century BCE, Aristotle noted that Mars disappeared behind the Moon during an occultation, indicating that the planet was farther away. [209] Ptolemy, a Greek living in Alexandria, [210] attempted to address the problem of the orbital motion of Mars. Ptolemy's model and his collective work on astronomy was presented in the multi-volume collection later called the Almagest (from the Arabic for "greatest"), which became the authoritative treatise on Western astronomy for the next fourteen centuries. [211] Literature from ancient China confirms that Mars was known by Chinese astronomers by no later than the fourth century BCE. [212] In the East Asian cultures, Mars is traditionally referred to as the "fire star" based on the Wuxing system. [213] [214] [215]

    During the seventeenth century A.D., Tycho Brahe measured the diurnal parallax of Mars that Johannes Kepler used to make a preliminary calculation of the relative distance to the planet. [216] From Brahe's observations of Mars, Kepler deduced that the planet orbited the Sun not in a circle, but in an ellipse. Moreover, Kepler showed that Mars sped up as it approached the Sun and slowed down as it moved farther away, in a manner that later physicists would explain as a consequence of the conservation of angular momentum. [217] :433–437 When the telescope became available, the diurnal parallax of Mars was again measured in an effort to determine the Sun-Earth distance. This was first performed by Giovanni Domenico Cassini in 1672. The early parallax measurements were hampered by the quality of the instruments. [218] The only occultation of Mars by Venus observed was that of 13 October 1590, seen by Michael Maestlin at Heidelberg. [219] In 1610, Mars was viewed by Italian astronomer Galileo Galilei, who was first to see it via telescope. [220] The first person to draw a map of Mars that displayed any terrain features was the Dutch astronomer Christiaan Huygens. [221]

    Martian "canals"

    A 1962 map of Mars published by the U.S. Aeronautical Chart and Information Center, showing canals snaking through the Martian landscape. At the time, the existence canals was still highly controversial as no close-up pictures of Mars had been taken (until Mariner 4's flyby in 1965). Mars - MEC-1 Prototype. LOC 2013593160.jpg
    A 1962 map of Mars published by the U.S. Aeronautical Chart and Information Center, showing canals snaking through the Martian landscape. At the time, the existence canals was still highly controversial as no close-up pictures of Mars had been taken (until Mariner 4's flyby in 1965).

    By the 19th century, the resolution of telescopes reached a level sufficient for surface features to be identified. On 5 September 1877, a perihelic opposition of Mars occurred. The Italian astronomer Giovanni Schiaparelli used a 22-centimetre (8.7 in) telescope in Milan to help produce the first detailed map of Mars. These maps notably contained features he called canali, which were later shown to be an optical illusion. These canali were supposedly long, straight lines on the surface of Mars, to which he gave names of famous rivers on Earth. His term, which means "channels" or "grooves", was popularly mistranslated in English as "canals". [222] [223]

    Influenced by the observations, the orientalist Percival Lowell founded an observatory which had 30- and 45-centimetre (12- and 18-in) telescopes. The observatory was used for the exploration of Mars during the last good opportunity in 1894 and the following less favorable oppositions. He published several books on Mars and life on the planet, which had a great influence on the public. [224] [225] The canali were independently observed by other astronomers, like Henri Joseph Perrotin and Louis Thollon in Nice, using one of the largest telescopes of that time. [226] [227]

    The seasonal changes (consisting of the diminishing of the polar caps and the dark areas formed during Martian summer) in combination with the canals led to speculation about life on Mars, and it was a long-held belief that Mars contained vast seas and vegetation. As bigger telescopes were used, fewer long, straight canali were observed. During observations in 1909 by Antoniadi with an 84-centimetre (33 in) telescope, irregular patterns were observed, but no canali were seen. [228]

    Robotic exploration

    Self-portrait of Perseverance rover and Ingenuity helicopter (left) at Wright Brothers Field, 2021 Mars 2020 selfie containing both perseverance rover and ingenuity.gif
    Self-portrait of Perseverance rover and Ingenuity helicopter (left) at Wright Brothers Field, 2021

    Dozens of crewless spacecraft, including orbiters, landers, and rovers, have been sent to Mars by the Soviet Union, the United States, Europe, India, the United Arab Emirates, and China to study the planet's surface, climate, and geology. [229] NASA's Mariner 4 was the first spacecraft to visit Mars; launched on 28 November 1964, it made its closest approach to the planet on 15 July 1965. Mariner 4 detected the weak Martian radiation belt, measured at about 0.1% that of Earth, and captured the first images of another planet from deep space. [230]

    Once spacecraft visited the planet during NASA's Mariner missions in the 1960s and 1970s, many previous concepts of Mars were radically broken. After the results of the Viking life-detection experiments, the hypothesis of a dead planet was generally accepted. [231] The data from Mariner 9 and Viking allowed better maps of Mars to be made, and the Mars Global Surveyor mission, which launched in 1996 and operated until late 2006, produced complete, extremely detailed maps of the Martian topography, magnetic field and surface minerals. [232] These maps are available online at websites including Google Mars. Both the Mars Reconnaissance Orbiter and Mars Express continued exploring with new instruments and supporting lander missions. NASA provides two online tools: Mars Trek, which provides visualizations of the planet using data from 50 years of exploration, and Experience Curiosity, which simulates traveling on Mars in 3-D with Curiosity. [233] [234]

    As of 2023, Mars is host to thirteen functioning spacecraft. Eight are in orbit: 2001 Mars Odyssey , Mars Express , Mars Reconnaissance Orbiter , MAVEN , ExoMars Trace Gas Orbiter , the Hope orbiter, and the Tianwen-1 orbiter. [235] [236] Another five are on the surface: the Mars Science Laboratory Curiosity rover, the Perseverance rover, the Ingenuity helicopter, the Tianwen-1 lander, and the Zhurong rover. [237]

    Planned missions to Mars include the Rosalind Franklin rover mission, designed to search for evidence of past life, which was intended to be launched in 2018 but has been repeatedly delayed, with a launch date pushed to 2024 at the earliest, with a more likely one sometime in 2028. [238] [239] [240] A current concept for a joint NASA-ESA mission to return samples from Mars would launch in 2026. [241] [242]

    (view * discuss)
Interactive image map of the global topography of Mars, overlain with locations of Mars Lander and Rover sites. Hover your mouse over the image to see the names of over 60 prominent geographic features, and click to link to them. Coloring of the base map indicates relative elevations, based on data from the Mars Orbiter Laser Altimeter on NASA's Mars Global Surveyor. Whites and browns indicate the highest elevations (+12 to +8 km); followed by pinks and reds (+8 to +3 km); yellow is 0 km; greens and blues are lower elevations (down to -8 km). Axes are latitude and longitude; Polar regions are noted.
(See also: Mars map; Mars Memorials map / list)
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Active ROVER *
Inactive *
Active LANDER *
Inactive *
Future ) Mars Map.JPGCydonia MensaeGale craterHolden craterJezero craterLomonosov craterLyot craterMalea PlanumMaraldi craterMareotis TempeMie craterMilankovič craterSisyphi Planum
    Interactive icon.svg Interactive image map of the global topography of Mars, overlain with locations of Mars Lander and Rover sites. Hover your mouse over the image to see the names of over 60 prominent geographic features, and click to link to them. Coloring of the base map indicates relative elevations, based on data from the Mars Orbiter Laser Altimeter on NASA's Mars Global Surveyor . Whites and browns indicate the highest elevations (+12 to +8 km); followed by pinks and reds (+8 to +3 km); yellow is 0 km; greens and blues are lower elevations (down to −8 km). Axes are latitude and longitude; Polar regions are noted.
    (    Active ROVER   Inactive   Active LANDER   Inactive   Future )
    Beagle 2 (2003)
    Curiosity (2012)
    Deep Space 2 (1999)

    InSight (2018)
    Mars 2 (1971)
    Mars 3 (1971)
    Mars 6 (1973)
    Polar Lander (1999)
    Opportunity (2004)
    Perseverance (2021)
    Phoenix (2008)
    Schiaparelli EDM (2016)
    Sojourner (1997)
    Spirit (2004)
    Zhurong (2021)
    Viking 1 (1976)
    Viking 2 (1976)

    Habitability and the search for life

    Curiosity rover's robotic arm showing drill in place, February 2013 MarsCuriosityRover-Drilling-Sol170++-2.jpg
    Curiosity rover’s robotic arm showing drill in place, February 2013

    During the late nineteenth century, it was widely accepted in the astronomical community that Mars had life-supporting qualities, including the presence of oxygen and water. [243] However, in 1894 W. W. Campbell at Lick Observatory observed the planet and found that "if water vapor or oxygen occur in the atmosphere of Mars it is in quantities too small to be detected by spectroscopes then available". [243] That observation contradicted many of the measurements of the time and was not widely accepted. [243] Campbell and V. M. Slipher repeated the study in 1909 using better instruments, but with the same results. It wasn't until the findings were confirmed by W. S. Adams in 1925 that the myth of the Earth-like habitability of Mars was finally broken. [243] However, even in the 1960s, articles were published on Martian biology, putting aside explanations other than life for the seasonal changes on Mars. Detailed scenarios for the metabolism and chemical cycles for a functional ecosystem were being published as late as 1962. [244]

    The current understanding of planetary habitability  the ability of a world to develop environmental conditions favorable to the emergence of life favors planets that have liquid water on their surface. Most often this requires the orbit of a planet to lie within the habitable zone, which for the Sun is estimated to extend from within the orbit of Earth to about that of Mars. [245] During perihelion, Mars dips inside this region, but Mars's thin (low-pressure) atmosphere prevents liquid water from existing over large regions for extended periods. The past flow of liquid water demonstrates the planet's potential for habitability. Recent evidence has suggested that any water on the Martian surface may have been too salty and acidic to support regular terrestrial life. [246]

    The environmental conditions on Mars are a challenge to sustaining organic life: the planet has little heat transfer across its surface, it has poor insulation against bombardment by the solar wind due to the absence of a magnetosphere and has insufficient atmospheric pressure to retain water in a liquid form (water instead sublimes to a gaseous state). Mars is nearly, or perhaps totally, geologically dead; the end of volcanic activity has apparently stopped the recycling of chemicals and minerals between the surface and interior of the planet. [247]

    Scoop of Mars soil by Curiosity, October 2012 PIA16226-MarsCuriosityRover-FirstScoopOfSoil-20121007.jpg
    Scoop of Mars soil by Curiosity, October 2012

    In situ investigations have been performed on Mars by the Viking landers, Spirit and Opportunity rovers, Phoenix lander, and Curiosity rover. Evidence suggests that the planet was once significantly more habitable than it is today, but whether living organisms ever existed there remains unknown. The Viking probes of the mid-1970s carried experiments designed to detect microorganisms in Martian soil at their respective landing sites and had positive results, including a temporary increase of CO2 production on exposure to water and nutrients. This sign of life was later disputed by scientists, resulting in a continuing debate, with NASA scientist Gilbert Levin asserting that Viking may have found life. [248] Tests conducted by the Phoenix Mars lander have shown that the soil has an alkaline pH and it contains magnesium, sodium, potassium and chloride. [249] The soil nutrients may be able to support life, but life would still have to be shielded from the intense ultraviolet light. [250]

    A 2014 analysis of Martian meteorite EETA79001 found chlorate, perchlorate, and nitrate ions in sufficiently high concentration to suggest that they are widespread on Mars. UV and X-ray radiation would turn chlorate and perchlorate ions into other, highly reactive oxychlorines, indicating that any organic molecules would have to be buried under the surface to survive. [251]

    Scientists have proposed that carbonate globules found in meteorite ALH84001, which is thought to have originated from Mars, could be fossilized microbes extant on Mars when the meteorite was blasted from the Martian surface by a meteor strike some 15 million years ago. This proposal has been met with skepticism, and an exclusively inorganic origin for the shapes has been proposed. [252] Small quantities of methane and formaldehyde detected by Mars orbiters are both claimed to be possible evidence for life, as these chemical compounds would quickly break down in the Martian atmosphere. [253] [254] Alternatively, these compounds may instead be replenished by volcanic or other geological means, such as serpentinite. [115] Impact glass, formed by the impact of meteors, which on Earth can preserve signs of life, has also been found on the surface of the impact craters on Mars. [255] [256] Likewise, the glass in impact craters on Mars could have preserved signs of life, if life existed at the site. [257] [258] [259]

    Human mission proposals

    Several plans for a human mission to Mars have been proposed throughout the 20th and 21st centuries, but none have come to fruition. The NASA Authorization Act of 2017 directed NASA to study the feasibility of a crewed Mars mission in the early 2030s; the resulting report eventually concluded that this would be unfeasible. [260] [261] In addition, in 2021, China was planning to send a crewed Mars mission in 2033. [262] Privately held companies such as SpaceX have also proposed plans to send humans to Mars, with the eventual goal to settle on the planet. [263] The moon Phobos has been proposed as an anchor point for a space elevator. [264]

    Viewing from Earth

    Mars seen through an 16-inch amateur telescope, at 2020 opposition Mars - 2020 Opposition (crop).jpg
    Mars seen through an 16-inch amateur telescope, at 2020 opposition

    The mean apparent magnitude of Mars is +0.71 with a standard deviation of 1.05. [18] Because the orbit of Mars is eccentric, the magnitude at opposition from the Sun can range from about −3.0 to −1.4. [265] The minimum brightness is magnitude +1.86 when the planet is near aphelion and in conjunction with the Sun. [18] At its brightest, Mars (along with Jupiter) is second only to Venus in apparent brightness. [18] Mars usually appears distinctly yellow, orange, or red. When farthest away from Earth, it is more than seven times farther away than when it is closest. Mars is usually close enough for particularly good viewing once or twice at 15-year or 17-year intervals. [266] As Mars approaches opposition, it begins a period of retrograde motion, which means it will appear to move backwards in a looping curve with respect to the background stars. This retrograde motion lasts for about 72 days, and Mars reaches its peak apparent brightness in the middle of this interval. [267]

    The point at which Mars's geocentric longitude is 180° different from the Sun's is known as opposition, which is near the time of closest approach to Earth. The time of opposition can occur as much as 8.5 days away from the closest approach. The distance at close approach varies between about 54 and 103 million km (34 and 64 million mi) due to the planets' elliptical orbits, which causes comparable variation in angular size. [268] [269] The most recent Mars opposition occurred on 13 October 2020, at a distance of about 63 million km (39 million mi). [270] The average time between the successive oppositions of Mars, its synodic period, is 780 days; but the number of days between successive oppositions can range from 764 to 812. [190]

    Mars comes into opposition from Earth every 2.1 years. The planets come into opposition near Mars's perihelion in 2003, 2018 and 2035, with the 2020 and 2033 events being particularly close to perihelic opposition. [201] [271] Mars made its closest approach to Earth and maximum apparent brightness in nearly 60,000 years, 55,758,006 km (0.37271925 AU; 34,646,419 mi), magnitude −2.88, on 27 August 2003, at 09:51:13 UTC. This occurred when Mars was one day from opposition and about three days from its perihelion, making it particularly easy to see from Earth. The last time it came so close is estimated to have been on 12 September 57,617 BC, the next time being in 2287. [272] This record approach was only slightly closer than other recent close approaches. [190]

    Optical ground-based telescopes are typically limited to resolving features about 300 kilometres (190 mi) across when Earth and Mars are closest because of Earth's atmosphere. [273]

    In culture

    The War of the Worlds by H. G. Wells, 1897, depicts an invasion of Earth by fictional Martians. War-of-the-worlds-tripod.jpg
    The War of the Worlds by H. G. Wells, 1897, depicts an invasion of Earth by fictional Martians.

    Mars is named after the Roman god of war. This association between Mars and war dates back at least to Babylonian astronomy, in which the planet was named for the god Nergal, deity of war and destruction. [274] [275] It persisted into modern times, as exemplified by Gustav Holst's orchestral suite The Planets , whose famous first movement labels Mars "the bringer of war". [276] The planet's symbol, a circle with a spear pointing out to the upper right, is also used as a symbol for the male gender. [277] The symbol dates from at latest the 11th century, though a possible predecessor has been found in the Greek Oxyrhynchus Papyri. [278]

    The idea that Mars was populated by intelligent Martians became widespread in the late 19th century. Schiaparelli's "canali" observations combined with Percival Lowell's books on the subject put forward the standard notion of a planet that was a drying, cooling, dying world with ancient civilizations constructing irrigation works. [279] Many other observations and proclamations by notable personalities added to what has been termed "Mars Fever". [280] High-resolution mapping of the surface of Mars revealed no artifacts of habitation, but pseudoscientific speculation about intelligent life on Mars still continues. Reminiscent of the canali observations, these speculations are based on small scale features perceived in the spacecraft images, such as "pyramids" and the "Face on Mars". [281] In his book Cosmos, planetary astronomer Carl Sagan wrote: "Mars has become a kind of mythic arena onto which we have projected our Earthly hopes and fears." [223]

    The depiction of Mars in fiction has been stimulated by its dramatic red color and by nineteenth-century scientific speculations that its surface conditions might support not just life but intelligent life. [282] This gave way to many science fiction stories involving these concepts, such as H. G. Wells' The War of the Worlds , in which Martians seek to escape their dying planet by invading Earth, Ray Bradbury's The Martian Chronicles , in which human explorers accidentally destroy a Martian civilization, as well as Edgar Rice Burroughs' Barsoom series, C. S. Lewis' novel Out of the Silent Planet (1938), [283] and a number of Robert A. Heinlein stories before the mid-sixties. [284] Since then, depictions of Martians have also extended to animation. A comic figure of an intelligent Martian, Marvin the Martian, appeared in Haredevil Hare (1948) as a character in the Looney Tunes animated cartoons of Warner Brothers, and has continued as part of popular culture to the present. [285] After the Mariner and Viking spacecraft had returned pictures of Mars as it really is, a lifeless and canal-less world, these ideas about Mars were abandoned; for many science-fiction authors, the new discoveries initially seemed like a constraint, but eventually the post-Viking knowledge of Mars became itself a source of inspiration for works like Kim Stanley Robinson's Mars trilogy. [286]

    See also


      1. The light filters are 635 nm, 546 nm, and 437 nm, which corresponds to red, green and blue
      2. 1 2 3 Best-fit ellipsoid

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      <span class="mw-page-title-main">Phobos (moon)</span> Largest and innermost moon of Mars

      Phobos is the innermost and larger of the two natural satellites of Mars, the other being Deimos. The two moons were discovered in 1877 by American astronomer Asaph Hall. It is named after Phobos, the Greek god of fear and panic, who is the son of Ares (Mars) and twin brother of Deimos.

      <span class="mw-page-title-main">Deimos (moon)</span> Smallest and outermost moon of Mars

      Deimos is the smaller and outermost of the two natural satellites of Mars, the other being Phobos. Deimos has a mean radius of 6.2 km (3.9 mi) and takes 30.3 hours to orbit Mars. Deimos is 23,460 km (14,580 mi) from Mars, much farther than Mars' other moon, Phobos. It is named after Deimos, the Ancient Greek god and personification of dread and terror.

      <i>Mars Global Surveyor</i> NASA Mars orbiter launched in 1996

      Mars Global Surveyor (MGS) was an American robotic space probe developed by NASA's Jet Propulsion Laboratory and launched November 1996. MGS was a global mapping mission that examined the entire planet, from the ionosphere down through the atmosphere to the surface. As part of the larger Mars Exploration Program, Mars Global Surveyor performed atmospheric monitoring for sister orbiters during aerobraking, and helped Mars rovers and lander missions by identifying potential landing sites and relaying surface telemetry.

      <span class="mw-page-title-main">Mars Exploration Rover</span> NASA mission to explore Mars via two rovers (Spirit and Opportunity); launched in 2003

      NASA's Mars Exploration Rover (MER) mission was a robotic space mission involving two Mars rovers, Spirit and Opportunity, exploring the planet Mars. It began in 2003 with the launch of the two rovers to explore the Martian surface and geology; both landed on Mars at separate locations in January 2004. Both rovers far outlived their planned missions of 90 Martian solar days: MER-A Spirit was active until March 22, 2010, while MER-B Opportunity was active until June 10, 2018.

      <i>Spirit</i> (rover) NASA Mars rover, active from 2004 to 2010

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

      <span class="mw-page-title-main">Exploration of Mars</span> Overview of the exploration of Mars

      The planet Mars has been explored remotely by spacecraft. Probes sent from Earth, beginning in the late 20th century, have yielded a large increase in knowledge about the Martian system, focused primarily on understanding its geology and habitability potential. Engineering interplanetary journeys is complicated and the exploration of Mars has experienced a high failure rate, especially the early attempts. Roughly sixty percent of all spacecraft destined for Mars failed before completing their missions and some failed before their observations could begin. Some missions have met with unexpected success, such as the twin Mars Exploration Rovers, Spirit and Opportunity which operated for years beyond their specification.

      <span class="mw-page-title-main">Life on Mars</span> Scientific assessments on the microbial habitability of Mars

      The possibility of life on Mars is a subject of interest in astrobiology due to the planet's proximity and similarities to Earth. To date, no proof of past or present life has been found on Mars. Cumulative evidence suggests that during the ancient Noachian time period, the surface environment of Mars had liquid water and may have been habitable for microorganisms, but habitable conditions do not necessarily indicate life.

      <span class="mw-page-title-main">Moons of Mars</span> Natural satellites orbiting Mars

      The two moons of Mars are Phobos and Deimos. They are irregular in shape. Both were discovered by American astronomer Asaph Hall in August 1877 and are named after the Greek mythological twin characters Phobos and Deimos who accompanied their father Ares into battle. Ares, god of war, was known to the Romans as Mars.

      <span class="mw-page-title-main">Terraforming of Mars</span> Hypothetical modification of Mars into a habitable planet

      The terraforming of Mars or the terraformation of Mars is a hypothetical procedure that would consist of a planetary engineering project or concurrent projects, with the goal to transform Mars from a planet hostile to terrestrial life to one that can sustainably host humans and other lifeforms free of protection or mediation. The process would involve the modification of the planet's extant climate, atmosphere, and surface through a variety of resource-intensive initiatives, and the installation of a novel ecological system or systems.

      <span class="mw-page-title-main">North Polar Basin (Mars)</span> Large basin in the northern hemisphere of Mars

      The North Polar Basin, more commonly known as the Borealis Basin, is a large basin in the northern hemisphere of Mars that covers 40% of the planet. Some scientists have postulated that the basin formed during the impact of a single, large body roughly 2% of the mass of Mars, having a diameter of about 1,900 km early in the history of Mars, around 4.5 billion years ago. However, the basin is not currently recognized as an impact basin by the IAU. The basin is one of the flattest areas in the Solar System, and has an elliptical shape.

      <span class="mw-page-title-main">Geology of Mars</span> Scientific study of the surface, crust, and interior of the planet Mars

      The geology of Mars is the scientific study of the surface, crust, and interior of the planet Mars. It emphasizes the composition, structure, history, and physical processes that shape the planet. It is analogous to the field of terrestrial geology. In planetary science, the term geology is used in its broadest sense to mean the study of the solid parts of planets and moons. The term incorporates aspects of geophysics, geochemistry, mineralogy, geodesy, and cartography. A neologism, areology, from the Greek word Arēs (Mars), sometimes appears as a synonym for Mars's geology in the popular media and works of science fiction. The term areology is also used by the Areological Society.

      <span class="mw-page-title-main">Climate of Mars</span> Climate patterns of the terrestrial planet

      The climate of Mars has been a topic of scientific curiosity for centuries, in part because it is the only terrestrial planet whose surface can be directly observed in detail from the Earth with help from a telescope.

      <span class="mw-page-title-main">Jezero (crater)</span> Crater on Mars

      Jezero is a crater on Mars in the Syrtis Major quadrangle, about 45.0 km (28.0 mi) in diameter. Thought to have once been flooded with water, the crater contains a fan-delta deposit rich in clays. The lake in the crater was present when valley networks were forming on Mars. Besides having a delta, the crater shows point bars and inverted channels. From a study of the delta and channels, it was concluded that the lake inside the crater probably formed during a period in which there was continual surface runoff.

      <span class="mw-page-title-main">Martian soil</span> Fine regolith found on the surface of Mars

      Martian soil is the fine regolith found on the surface of Mars. Its properties can differ significantly from those of terrestrial soil, including its toxicity due to the presence of perchlorates. The term Martian soil typically refers to the finer fraction of regolith. So far, no samples have been returned to Earth, the goal of a Mars sample-return mission, but the soil has been studied remotely with the use of Mars rovers and Mars orbiters.

      <span class="mw-page-title-main">Arcadia quadrangle</span> Map of Mars

      The Arcadia quadrangle is one of a series of 30 quadrangle maps of Mars used by the United States Geological Survey (USGS) Astrogeology Research Program. The quadrangle is located in the north-central portion of Mars’ western hemisphere and covers 240° to 300° east longitude and 30° to 65° north latitude. The quadrangle uses a Lambert conformal conic projection at a nominal scale of 1:5,000,000 (1:5M). The Arcadia quadrangle is also referred to as MC-3.

      <span class="mw-page-title-main">Water on Mars</span> Study of past and present water on Mars

      Almost all water on Mars today exists as ice, though it also exists in small quantities as vapor in the atmosphere. What was thought to be low-volume liquid brines in shallow Martian soil, also called recurrent slope lineae, may be grains of flowing sand and dust slipping downhill to make dark streaks. The only place where water ice is visible at the surface is at the north polar ice cap. Abundant water ice is also present beneath the permanent carbon dioxide ice cap at the Martian south pole and in the shallow subsurface at more temperate conditions. More than 5 million km3 of ice have been detected at or near the surface of Mars, enough to cover the whole planet to a depth of 35 meters (115 ft). Even more ice is likely to be locked away in the deep subsurface.

      <span class="mw-page-title-main">Composition of Mars</span> Branch of the geology of Mars

      The composition of Mars covers the branch of the geology of Mars that describes the make-up of the planet Mars.

      <span class="mw-page-title-main">Timeline of Mars Science Laboratory</span> Event timeline of the NASA Mars Science Laboratory mission

      The Mars Science Laboratory and its rover, Curiosity, were launched from Earth on November 26, 2011. As of June 5, 2023, Curiosity has been on the planet Mars for 3850 sols since landing on August 6, 2012. (See Current status.)

      <span class="mw-page-title-main">Lakes on Mars</span> Overview of the presence of lakes on Mars

      In summer 1965, the first close-up images from Mars showed a cratered desert with no signs of water. However, over the decades, as more parts of the planet were imaged with better cameras on more sophisticated satellites, Mars showed evidence of past river valleys, lakes and present ice in glaciers and in the ground. It was discovered that the climate of Mars displays huge changes over geologic time because its axis is not stabilized by a large moon, as Earth's is. Also, some researchers maintain that surface liquid water could have existed for periods of time due to geothermal effects, chemical composition or asteroid impacts. This article describes some of the places that could have held large lakes.

      The following outline is provided as an overview of and topical guide to Mars:


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