Mars (pronounced /ˈmɑrz/) is the fourth planet from the Sun in the Solar System. The planet is named after Mars, the Roman god of war. It is also referred to as the "Red Planet" because of its reddish appearance, due to iron oxide prevalent on its surface.
Mars is a terrestrial planet with a thin atmosphere, having surface features reminiscent both of the impact craters of the Moon and the volcanoes, valleys, deserts and polar ice caps of Earth. It is the site of Olympus Mons, the highest known mountain in the Solar System, and of Valles Marineris, the largest canyon. Furthermore, in June 2008 three articles published in Nature presented evidence of an enormous impact crater in Mars' northern hemisphere, 10,600 km long by 8,500 km wide, or roughly four times larger than the largest impact crater yet discovered, the South Pole-Aitken basin. In addition to its geographical features, Mars’ rotational period and seasonal cycles are likewise similar to those of Earth.
Until the first flyby of Mars by Mariner 4 in 1965, many speculated that there might be liquid water on the planet's surface. This was based on observations of periodic variations in light and dark patches, particularly in the polar latitudes, which looked like seas and continents, while long, dark striations were interpreted by some observers as irrigation channels for liquid water. These straight line features were later proven not to exist and were instead explained as optical illusions. Still, of all the planets in the Solar System other than Earth, Mars is the most likely to harbor liquid water, and perhaps life. Radar data from Mars Express and the Mars Reconnaissance Orbiter have revealed the presence of large quantities of water ice both at the poles (July 2005) and at mid-latitudes (November 2008). The Phoenix Mars Lander directly sampled water ice in shallow martian soil on July 31, 2008.
Mars is currently host to three functional orbiting spacecraft: Mars Odyssey, Mars Express, and the Mars Reconnaissance Orbiter. With the exception of Earth, this is more than any planet in the Solar System. The surface is also home to the two Mars Exploration Rovers (Spirit and Opportunity) and several inert landers and rovers, both successful and unsuccessful. The Phoenix lander recently completed its mission on the surface. Geological evidence gathered by these and preceding missions suggests that Mars previously had large-scale water coverage, while observations also indicate that small geyser-like water flows have occurred during the past decade. Observations by NASA's Mars Global Surveyor show evidence that parts of the southern polar ice cap have been receding.
Mars has two moons, Phobos and Deimos, which are small and irregularly shaped. These may be captured asteroids, similar to 5261 Eureka, a Martian Trojan asteroid. Mars can be seen from Earth with the naked eye. Its apparent magnitude reaches −2.9, a brightness surpassed only by Venus, the Moon, and the Sun, although most of the time Jupiter will appear brighter to the naked eye than Mars.
Mars has approximately half the radius of Earth. It is less dense than Earth, having about 15% of Earth's volume and 11% of the mass. Its surface area is only slightly less than the total area of Earth's dry land. While Mars is larger and more massive than Mercury, Mercury has a higher density. This results in a slightly stronger gravitational force at Mercury's surface. Mars is also roughly intermediate in size, mass, and surface gravity between Earth and Earth's Moon (the Moon is about half the diameter of Mars, whereas Earth is twice; the Earth is about ten times more massive than Mars, and the Moon ten times less massive). The red-orange appearance of the Martian surface is caused by iron(III) oxide, more commonly known as hematite, or rust.
- Main article: Geology of Mars
Based on orbital observations and the examination of the Martian meteorite collection, the surface of Mars appears to be composed primarily of basalt. Some evidence suggests that a portion of the Martian surface is more silica-rich than typical basalt, and may be similar to andesitic rocks on Earth; however, these observations may also be explained by silica glass. Much of the surface is deeply covered by finely grained iron(III) oxide dust.
Although Mars has no intrinsic magnetic field, observations show that parts of the planet's crust have been magnetized and that alternating polarity reversals of its dipole field have occurred. This paleomagnetism of magnetically susceptible minerals has properties that are very similar to the alternating bands found on the ocean floors of Earth. One theory, published in 1999 and re-examined in October 2005 (with the help of the Mars Global Surveyor), is that these bands demonstrate plate tectonics on Mars 4 billion years ago, before the planetary dynamo ceased to function and caused the planet's magnetic field to fade away.
Current models of the planet's interior imply a core region about 1,480 kilometres in radius, consisting primarily of iron with about 14–17% sulfur. This iron sulfide core is partially fluid, and has twice the concentration of the lighter elements than exist at Earth's core. The core is surrounded by a silicate mantle that formed many of the tectonic and volcanic features on the planet, but now appears to be inactive. The average thickness of the planet's crust is about 50 km, with a maximum thickness of 125 km. Earth's crust, averaging 40 km, is only a third as thick as Mars’ crust relative to the sizes of the two planets.
The geological history of Mars can be split into many epochs, but the following are the three main ones:
- Noachian epoch (named after Noachis Terra): Formation of the oldest extant surfaces of Mars, 3.8 billion years ago to 3.5 billion years ago. Noachian age surfaces are scarred by many large impact craters. The Tharsis bulge volcanic upland is thought to have formed during this period, with extensive flooding by liquid water late in the epoch.
- Hesperian epoch (named after Hesperia Planum): 3.5 billion years ago to 1.8 billion years ago. The Hesperian epoch is marked by the formation of extensive lava plains.
- Amazonian epoch (named after Amazonis Planitia): 1.8 billion years ago to present. Amazonian regions have few meteorite impact craters but are otherwise quite varied. Olympus Mons formed during this period along with lava flows elsewhere on Mars.
A major geological event occurred on Mars on February 19, 2008, and was caught on camera by the Mars Reconnaissance Orbiter. Images capturing a spectacular avalanche of materials thought to be fine grained ice, dust, and large blocks are shown to have detached from a 700-metre high cliff. Evidence of the avalanche is present in the dust clouds left above the cliff afterwards.
Recent studies support a theory, first proposed in the 1980s, that Mars was struck by a Pluto-sized meteor 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.
- Main article: Martian soil
In June, 2008, the Phoenix Lander returned data showing Martian soil to be slightly alkaline and containing vital nutrients such as magnesium, sodium, potassium and chloride, all of which are necessary for living organisms to grow. Scientists compared the soil near Mars' north pole to that of backyard gardens on Earth, and concluded that it could be suitable for growth of plants such as asparagus. However, in August, 2008, the Phoenix Lander conducted simple chemistry experiments, mixing water from Earth with Martian soil in an attempt to test its pH, and discovered traces of the salt perchlorate, while also confirming many scientists theories that the Martian surface was considerably basic, measuring at 8.3. The presence of the perchlorate, if confirmed, would make Martian soil more exotic than previously believed. Further testing is necessary to eliminate the possibility of the perchlorate readings being caused by terrestrial sources, which may have migrated from the spacecraft either into samples or the instrumentation.
- Main article: Water on Mars
Liquid water cannot exist on the surface of Mars with its present low atmospheric pressure, except at the lowest elevations for short periods but water ice is in no short supply, with two polar ice caps made largely of ice. In March 2007, NASA announced that the volume of water ice in the south polar ice cap, if melted, would be sufficient to cover the entire planetary surface to a depth of 11 metres. Additionally, an ice permafrost mantle stretches down from the pole to latitudes of about 60°.
Large quantities of water are thought to be trapped underneath Mars's thick cryosphere. Radar data from Mars Express and the Mars Reconnaissance Orbiter have revealed the presence of large quantities of water ice both at the poles (July 2005) and at mid-latitudes (November 2008). The Phoenix Mars Lander directly sampled water ice in shallow martian soil on July 31, 2008. A large release of liquid water is thought to have occurred when the Valles Marineris formed early in Mars's history, forming massive outflow channels. A smaller but more recent outflow may have occurred when the Cerberus Fossae chasm opened about 5 million years ago, leaving a supposed sea of frozen ice still visible today on the Elysium Planitia centered at Cerberus Palus. However, the morphology of this region may correspond to the ponding of lava flows, causing a superficial morphology similar to ice flows, which probably draped the terrain established by earlier massive floods of Athabasca Valles. Rough surface texture at decimetre (dm) scales, thermal inertia comparable to that of the Gusev plains, and hydrovolcanic cones are consistent with the lava flow hypothesis. Furthermore, the stoichiometric mass fraction of water in this area to tens of centimetre depths is only ~4%, easily attributable to hydrated minerals and inconsistent with the presence of near-surface ice.
More recently the high resolution Mars Orbiter Camera on the Mars Global Surveyor has taken pictures which give much more detail about the history of liquid water on the surface of Mars. Despite the many giant flood channels and associated tree-like network of tributaries found on Mars there are no smaller scale structures that would indicate the origin of the flood waters. It has been suggested that weathering processes have denuded these, indicating the river valleys are old features. Higher resolution observations from spacecraft like Mars Global Surveyor also revealed at least a few hundred features along crater and canyon walls that appear similar to terrestrial seepage gullies. The gullies tend to be in the highlands of the southern hemisphere and to face the Equator; all are poleward of 30° latitude. The researchers found no partially degraded (i.e. weathered) gullies and no superimposed impact craters, indicating that these are very young features.
In a particularly striking example (see image) two photographs, taken six years apart, show a gully on Mars with what appears to be new deposits of sediment. Michael Meyer, the lead scientist for NASA's Mars Exploration Program, argues that only the flow of material with a high liquid water content could produce such a debris pattern and colouring. Whether the water results from precipitation, underground or another source remains an open question. However, alternative scenarios have been suggested, including the possibility of the deposits being caused by carbon dioxide frost or by the movement of dust on the Martian surface.
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.
Nevertheless, some of the evidence believed to indicate ancient water basins and flows has been negated by higher resolution studies taken at resolution about 30 cm by the Mars Reconnaissance Orbiter.
- Main article: Geography of Mars
Although better remembered for mapping the Moon, Johann Heinrich Mädler and Wilhelm Beer were the first "areographers". They began by establishing once and for all that most of Mars’ surface features were permanent, and determining the planet's rotation period. In 1840, Mädler combined ten years of observations and drew the first map of Mars. Rather than giving names to the various markings, Beer and Mädler simply designated them with letters; Meridian Bay (Sinus Meridiani) was thus feature "a."
Today, features on Mars are named from a number of sources. 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).
Mars’ 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 in 1830 for their first maps of Mars. 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 for the definition of 0.0° longitude to coincide with the original selection.
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Since Mars has no oceans and hence no 'sea level', a zero-elevation surface or mean gravity surface also had to be selected. Zero altitude is defined by the height at which there is 610.5 Pa (6.105 mbar) of atmospheric pressure. This pressure corresponds to the triple point of water, and is about 0.6% of the sea level surface pressure on Earth (.006 atm).
The dichotomy of Martian topography is striking: northern plains flattened by lava flows contrast with the southern highlands, pitted and cratered by ancient impacts. Research in 2008 has presented evidence regarding a theory proposed in 1980 postulating that, four billion years ago, the northern hemisphere of Mars was struck by an object one-tenth to two-thirds the size of the Moon. If validated, this would make Mars' northern hemisphere the site of an impact crater 10 600 km long by 8 500 km wide, or roughly the area of Europe, Asia, and Australia combined, surpassing the South Pole-Aitken basin as the largest impact crater in the Solar System. 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.
- See also: Error: Template must be given at least one article name It is an extinct volcano in the vast upland region Tharsis, which contains several other large volcanoes. It is over three times the height of Mount Everest which in comparison stands at just over 8.8 km.
Mars is also scarred by a number of impact craters: a total of 43 000 craters with a diameter of 5 km or greater have been found. The largest confirmed of these is the Hellas impact basin, a light albedo feature clearly visible from Earth. Due to the smaller mass of Mars, the probability of an object colliding with the planet is about half that of the Earth. However, Mars is located closer to the asteroid belt, so it has an increased chance of being struck by materials from that source. Mars is also more likely to be struck by short-period comets, i.e., those that lie within the orbit of Jupiter. In spite of this, there are far fewer craters on Mars compared with the Moon because Mars's atmosphere provides protection against small meteors. Some craters have a morphology that suggests the ground was wet when the meteor impacted.
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The large canyon, Valles Marineris (Latin for Mariner Valleys, also known as Agathadaemon in the old canal maps), has a length of 4000 km and a depth of up to 7 km. 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 km long and nearly 2 km 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. Another large canyon is Ma'adim Vallis (Ma'adim is Hebrew for Mars). It is 700 km long and again much bigger than the Grand Canyon with a width of 20 km and a depth of 2 km in some places. It is possible that Ma'adim Vallis was flooded with liquid water in the past.
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 Arsia Mons volcano. The caves, named after loved ones of their discoverers, are collectively known as the "seven sisters." Cave entrances measure from 100 m to 252 m wide and they are believed to be at least 73 m to 96 m deep. Because light does not reach the floor of most of the caves, it is likely that they 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 m 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. Some researchers have suggested that this protection makes the caves good candidates for future efforts to find liquid water and signs of life.
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- Main article: Atmosphere of Mars
Mars lost its magnetosphere 4 billion years ago, so the solar wind interacts directly with the Martian ionosphere, keeping the atmosphere thinner than it would otherwise be by stripping away atoms from the outer layer. Both Mars Global Surveyor and Mars Express have detected these ionised atmospheric particles trailing off into space behind Mars. The atmosphere of Mars is now relatively thin. Atmospheric pressure on the surface varies from around 30 Pa (0.03 kPa) on Olympus Mons to over 1,155 Pa (1.155 kPa) in the depths of Hellas Planitia, with a mean surface level pressure of 600 Pa (0.6 kPa). Mars's mean surface pressure equals the pressure found 35 km above the Earth's surface. This is less than 1% of the surface pressure on Earth (101.3 kPa). The scale height of the atmosphere, about 11 km, is higher than Earth's (6 km) due to the lower gravity. Mars' gravity is only about 38% of the surface gravity on Earth.
The atmosphere on Mars consists of 95% carbon dioxide, 3% nitrogen, 1.6% argon, and contains traces of oxygen and water. 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.
Several researchers claim to have detected methane in the Martian atmosphere with a concentration of about 30 ppb by volume. Since methane is an unstable gas that is broken down by ultraviolet radiation, typically lasting about 340 years in the Martian atmosphere, its presence would indicate a current or recent source of the gas on the planet. Volcanic activity, cometary impacts, and the presence of methanogenic microbial life forms are among possible sources. It was recently pointed out that methane could also be produced by a non-biological process called serpentinization[b] involving water, carbon dioxide, and the mineral olivine, which is known to be common on Mars.
During a pole's winter, it lies in continuous darkness, chilling the surface and causing 25–30% of the atmosphere to condense out into thick slabs of CO2 ice (dry ice). When the poles are again exposed to sunlight, the frozen CO2 sublimes, creating enormous winds that sweep off the poles as fast as 400 km/h. 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.
- Main article: Climate of Mars
Of all the planets, Mars's seasons are the most Earth-like, due to the similar tilts of the two planets' rotational axes. However, the lengths of the Martian seasons are about twice those of Earth's, as Mars’ greater distance from the Sun leads to the Martian year being about two Earth years in length. Martian surface temperatures vary from lows of about −140 °C (−220 °F) during the polar winters to highs of up to 20 °C (68 °F) in summers. The wide range in temperatures is due to the thin atmosphere which cannot store much solar heat, the low atmospheric pressure, and the low thermal inertia of Martian soil.
If Mars had an Earth-like orbit, its seasons would be similar to Earth's because its axial tilt is similar to Earth's. However, 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 reach up to 30 °C (54 °F) warmer than the equivalent summer temperatures in the north.
Mars also has the largest dust storms in our Solar System. 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.
The polar caps at both poles consist primarily of water ice. However, there is dry ice present on their surfaces. Frozen carbon dioxide (dry ice) accumulates as a thin layer about one metre thick on the north cap in the northern winter only, while the south cap has a permanent dry ice cover about eight metres thick. The northern polar cap has a diameter of about 1000 kilometres during the northern Mars summer, and contains about 1.6 million cubic kilometres of ice, which if spread evenly on the cap would be 2 kilometres thick. (This compares to a volume of 2.85 million cubic kilometres for the Greenland ice sheet.) The southern polar cap has a diameter of 350 km and a thickness of 3 km. The total volume of ice in the south polar cap plus the adjacent layered deposits has also been estimated at 1.6 million cubic kilometres. Both polar caps show spiral troughs, which are believed to form as a result of differential solar heating, coupled with the sublimation of ice and condensation of water vapor. Both polar caps shrink and regrow following the temperature fluctuation of the Martian seasons.
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Recent exploration of Mars has revealed evidence of several defining moments in its history. For example, the remnants of a magnetic field suggest that something more than the mass of Mars once kept its interior molten; the ancient presence of water would have required an atmosphere thicker than that of today; and the Northern Basin records a massive and disruptive impact. Possible explanations include:
- A massive satellite, perhaps a captured asteroid, caused enough tidal heating to melt the interior enough to generate a substantial magnetic field. The field protected the Martian atmosphere from the Solar wind, allowing liquid water to remain on the surface.
- A massive impact removes the crust of one hemisphere and strips Mars of its atmosphere. This may have been the satellite, whose orbit could have decayed from tidal forces. The entire crust shifts to a more stable configuration with the impact basin centered at the north pole and Mars' massive volcanoes near the equator. Without tidal heating from the satellite, the magnetic field fades, and Solar wind striking the surface prevents the atmosphere from reforming.
- The lack of stabilizing satellite allows significant wobble on the order of five million years. This periodically warms the polar regions enough for at least some liquid water to form, and leaves striations in the polar ice cap.
Orbit and rotationEdit
Mars’ average distance from the Sun is roughly 230 million km (1.5 AU) 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. A Martian year is equal to 1.8809 Earth years, or 1 year, 320 days, and 18.2 hours.
Mars's axial tilt is 25.19 degrees, which is similar to the axial tilt of the Earth. As a result, Mars has seasons like the Earth, though on Mars they are nearly twice as long given its longer year. Mars passed its perihelion in April 2009 and its aphelion in May 2008. It next reaches perihelion in May 2011 and aphelion in March 2010.
Mars has a relatively pronounced orbital eccentricity of about 0.09; of the seven other planets in the Solar System, only Mercury shows greater eccentricity. However, it is known that in the past Mars has had a much more circular orbit than it does currently. At one point 1.35 million Earth years ago, Mars had an eccentricity of roughly 0.002, much less than that of Earth today. The Mars cycle of eccentricity is 96,000 Earth years compared to the Earth's cycle of 100,000 years. However, Mars also has a much longer cycle of eccentricity with a period of 2.2 million Earth years, and this overshadows the 96,000-year cycle in the eccentricity graphs. For the last 35,000 years Mars' orbit has been getting slightly more eccentric because of the gravitational effects of the other planets. The closest distance between the Earth and Mars will continue to mildly decrease for the next 25,000 years.
The image to the left shows a comparison between Mars and Ceres, a dwarf planet in the Asteroid Belt, as seen from the north ecliptic pole, while the image to the right is as seen from the ascending node. The segments of orbits south of the ecliptic are plotted in darker colors. The perihelia (q) and aphelia (Q) are labelled with the date of the nearest passage.
- Main article: Moons of Mars
Both satellites were discovered in 1877 by Asaph Hall, and are named after the characters Phobos (panic/fear) and Deimos (terror/dread) who, in Greek mythology, accompanied their father Ares, god of war, into battle. Ares was known as Mars to the Romans.
From the surface of Mars, the motions of Phobos and Deimos appear very different from that of our own 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 very slowly. Despite the 30 hour orbit of Deimos, it takes 2.7 days to set in the west as it slowly falls behind the rotation of Mars, then just as long again to rise.
Because Phobos' orbit is below synchronous altitude, the tidal forces from the planet Mars are gradually lowering its orbit. In about 50 million years it will either crash into Mars’ surface or break up into a ring structure around the planet.
It is not well understood how or when Mars came to capture its two moons. Both have circular orbits, very near the equator, which is very unusual in itself for captured objects. Phobos's unstable orbit would seem to point towards a relatively recent capture. There is no known mechanism for an airless Mars to capture a lone asteroid, so it is likely that a third body was involved — however, asteroids as large as Phobos and Deimos are rare, and binaries rarer still, outside the asteroid belt.
Dark Slope StreaksEdit
The photo below shows a dark streak. Such streaks are very common on Mars. They occur on steep slopes of craters, troughs, and valleys. The streaks are dark at first and get lighter with age. Sometimes they start in a small area, then spread out and go for hundreds of metres. They have been seen to travel around obstacles, such as boulders. It is believed that they are dark underlying layers of soil revealed after avalanches of bright dust. However, several ideas have been advanced to explain them, some of which involve water or even the growth of organisms. A notable aspect of these dark streaks is that new ones occur frequently.
- Main article: Life on Mars
The current understanding of planetary habitability—the ability of a world to develop and sustain life—favors planets that have liquid water on their surface. This most often requires that the orbit of a planet lie within the habitable zone, which for the Sun currently extends from just beyond Venus to about the semi-major axis of Mars. During perihelion Mars dips inside this region, but the planet's thin (low-pressure) atmosphere prevents liquid water from existing over large regions for extended periods. The past flow of liquid water, however, demonstrates the planet's potential for habitability. Recent evidence has suggested that any water on the Martian surface would have been too salty and acidic to support terran life.
The lack of a magnetosphere and extremely thin atmosphere of Mars are a greater challenge: the planet has little heat transfer across its surface, poor insulation against bombardment and the solar wind, and insufficient atmospheric pressure to retain water in a liquid form (water instead sublimates to a gaseous state). Mars is also nearly, or perhaps totally, geologically dead; the end of volcanic activity has stopped the recycling of chemicals and minerals between the surface and interior of the planet.
Evidence suggests that the planet was once significantly more habitable than it is today, but whether living organisms ever existed there is still unclear. The Viking probes of the mid-1970s carried experiments designed to detect microorganisms in Martian soil at their respective landing sites, and had some apparently positive results, including a temporary increase of CO2 production on exposure to water and nutrients. However this sign of life was later disputed by many scientists, resulting in a continuing debate, with NASA scientist Gilbert Levin asserting that Viking may have found life. A re-analysis of the now 30-year-old Viking data, in light of modern knowledge of extremophile forms of life, has suggested that the Viking tests were also not sophisticated enough to detect these forms of life. The tests may even have killed a (hypothetical) life form. Tests conducted by the Phoenix Mars Lander have shown that the soil has a very alkaline pH and it contains magnesium, sodium, potassium and chloride. The soil nutrients may be able to support life, but life would still have to be shielded from the intense ultraviolet light.
At the Johnson space center lab organic compounds have been found in the meteorite ALH84001, which is supposed to have come from Mars. They concluded that these were deposited by primitive life forms extant on Mars before the meteorite was blasted into space by a meteor strike and sent on a 15 million-year voyage to Earth. Also, small quantities of methane and formaldehyde recently detected by Mars orbiters are both claimed to be hints for life, as these chemical compounds would quickly break down in the Martian atmosphere. It is possible that these compounds may be replenished by volcanic or geological means such as serpentinization.
- Main article: Exploration of Mars
Roughly two-thirds of all spacecraft destined for Mars have failed in one manner or another before completing or even beginning their missions. While this high failure rate can be ascribed to technical problems, enough have either failed or lost communications for causes unknown for some to search for other explanations. Examples include an Earth-Mars "Bermuda Triangle", a Mars Curse, or even the long-standing NASA in-joke, the "Great Galactic Ghoul" that feeds on Martian spacecraft.
The first successful fly-by mission to Mars was NASA's Mariner 4, launched in 1964. On November 14, 1971 Mariner 9 became the first space probe to orbit another planet when it entered into orbit around Mars. The first successful objects to land on the surface were two Soviet probes, Mars 2 and Mars 3 from the Mars probe program, launched in 1971, but both lost contact within seconds of landing. Then came the 1975 NASA launches of the Viking program, which consisted of two orbiters, each having a lander; both landers successfully touched down in 1976. Viking 1 remained operational for six years, Viking 2 for three. The Viking landers relayed the first color pictures of Mars and also mapped the surface of Mars so well that the images are still sometimes used to this day.
The Soviet probes Phobos 1 and 2 were sent to Mars in 1988 to study Mars and its two moons. Phobos 1 lost contact on the way to Mars. Phobos 2, while successfully photographing Mars and Phobos, failed just before it was set to release two landers on Phobos's surface.
Following the 1992 failure of the Mars Observer orbiter, NASA launched the Mars Global Surveyor in 1996. This mission was a complete success, having finished its primary mapping mission in early 2001. Contact was lost with the probe in November 2006 during its third extended program, spending exactly 10 operational years in space. Only a month after the launch of the Surveyor, NASA launched the Mars Pathfinder, carrying a robotic exploration vehicle Sojourner, which landed in the Ares Vallis on Mars in the summer of 1997. This mission was also successful, and received much publicity, partially due to the many images that were sent back to Earth.
The most recent mission to Mars was the NASA Phoenix Mars lander, which launched August 4, 2007 and arrived on the north polar region of Mars on May 25, 2008. The lander has a robotic arm with a 2.5 m reach and capable of digging a metre into the Martian soil. The lander has a microscopic camera capable of resolving to one-thousandth the width of a human hair, and discovered a substance at its landing site on June 15, 2008, which was confirmed to be water ice on June 20. The mission was declared concluded on November 10, 2008, after engineers were unable to contact the craft.
Current missionsEditIn 2001 NASA launched the successful Mars Odyssey orbiter, which is still in orbit as of March 2009, and the ending date has been extended to September 2010. Odyssey's Gamma Ray Spectrometer detected significant amounts of hydrogen in the upper metre or so of Mars's regolith. This hydrogen is thought to be contained in large deposits of water ice.
In 2003, the European Space Agency (ESA) launched the Mars Express craft, consisting of the Mars Express Orbiter and the lander Beagle 2. Beagle 2 failed during descent and was declared lost in early February 2004. In early 2004 the Planetary Fourier Spectrometer team announced it had detected methane in the Martian atmosphere. ESA announced in June 2006 the discovery of aurorae on Mars.
Also in 2003, NASA launched the twin Mars Exploration Rovers named Spirit (MER-A) and Opportunity (MER-B). Both missions landed successfully in January 2004 and have met or exceeded all their targets. Among the most significant scientific returns has been conclusive evidence that liquid water existed at some time in the past at both landing sites. Martian dust devils and windstorms have occasionally cleaned both rovers' solar panels, and thus increased their lifespan.
On August 12, 2005 the NASA Mars Reconnaissance Orbiter probe was launched toward the planet, arriving in orbit on March 10, 2006 to conduct a two-year science survey. The orbiter will map the Martian terrain and weather to find suitable landing sites for upcoming lander missions. It also contains an improved telecommunications link to Earth, with more bandwidth than all previous missions combined. The Mars Reconnaissance Orbiter snapped the first image of a series of active avalanches near the planet's north pole, scientists said March 3, 2008.
Phoenix will be followed by the Mars Science Laboratory in 2011, a bigger, faster (90 m/h), and smarter version of the Mars Exploration Rovers. Experiments include a laser chemical sampler that can deduce the make-up of rocks at a distance of 13 m.
The joint Russian and Chinese Phobos-Grunt mission to return samples of Mars's moon Phobos is scheduled for a 2009 launch. In 2013 the ESA plans to launch its first Rover to Mars; the ExoMars rover will be capable of drilling 2 m into the soil in search of organic molecules.
The Finnish-Russian MetNet mission will land tens of small vehicles on the Martian surface to establish a widespread surface observation network to investigate the planet's atmospheric structure, physics and meteorology. A precursor mission using one or a few landers is scheduled for launch in 2009 or 2011. One possibility is a piggyback launch on the Russian Phobos-Grunt mission. Other launches will take place in the launch windows extending to 2019.
Manned Mars exploration by the United States has been explicitly identified as a long-term goal in the Vision for Space Exploration announced in 2004 by US President George W. Bush. NASA and Lockheed Martin have begun work on the Orion spacecraft, formerly the Crew Exploration Vehicle, which is currently scheduled to send a human expedition to Earth's moon by 2020 as a stepping stone to an expedition to Mars thereafter. On September 28, 2007, NASA administrator Michael D. Griffin stated that NASA aims to put a man on Mars by 2037.
ESA hopes to land humans on Mars between 2030 and 2035. This will be preceded by successively larger probes, starting with the launch of the ExoMars probe and a Mars Sample Return Mission.
Astronomy on MarsEdit
- Main article: Astronomy on Mars
With the existence of various orbiters, landers, and rovers, it is now possible to study astronomy from the Martian skies. While Mars’ moon Phobos appears about one third the angular diameter of the full Moon as it appears from Earth, Deimos appears more or less star-like, and appears only slightly brighter than Venus does from Earth.
There are also various phenomena well-known on Earth that have now been observed on Mars, such as meteors and auroras. A transit of the Earth as seen from Mars will occur on November 10, 2084. There are also transits of Mercury and transits of Venus, and the moon Deimos is of sufficiently small angular diameter that its partial "eclipses" of the Sun are best considered transits (see Transit of Deimos from Mars).
To the naked eye, Mars usually appears a distinct yellow, orange, or reddish color, and varies in brightness more than any other planet as seen from Earth over the course of its orbit. However the actually colour of Mars is closer to butterscotch, the redness seen is actually just dust in the planets atmosphere; considering this NASA's Spirit rover has taken pictures of a greenish-brown, mud-coloured landscape with blue-grey rocks and patches of light red coloured sand . The apparent magnitude of Mars varies from +1.8 at conjunction to as high as −2.9 at perihelic opposition. When farthest away from the Earth, it is more than seven times as far from the latter as when it is closest. When least favourably positioned, it can be lost in the Sun's glare for months at a time. At its most favourable times — at 15- or 17-year intervals, and always between late July and late September — Mars shows a wealth of surface detail to a telescope. Especially noticeable, even at low magnification, are the polar ice caps.
The point of Mars’ closest approach to the Earth is known as opposition. The length of time between successive oppositions, or the synodic period, is 780 days. Because of the eccentricities of the orbits, the times of opposition and minimum distance can differ by up to 8.5 days. The minimum distance varies between about 55 and 100 million km due to the planets' elliptical orbits. The next Mars opposition will occur on January 29, 2010.
As Mars approaches opposition it begins a period of retrograde motion, which means it will appear to move backwards in a looping motion with respect to the background stars.
2003 closest approachEdit
On August 27, 2003, at 9:51:13 UT, Mars made its closest approach to Earth in nearly 60 000 years: 55 758 006 km (0.372719 Template:Val/unitswithlink). This occurred when Mars was one day from opposition and about three days from its perihelion, making Mars particularly easy to see from Earth. The last time it came so close is estimated to have been on September 12, 57 617 BC, the next time being in 2287. However, this record approach was only very slightly closer than other recent close approaches. For instance, the minimum distance on August 22, 1924 was 0.37285 Template:Val/unitswithlink, and the minimum distance on August 24, 2208 will be 0.37279 Template:Val/unitswithlink.
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 occur every 15 or 17 years, and are distinguished because Mars is close to perihelion, making it even closer to Earth. Aristotle was among the first known writers to describe observations of Mars, noting that, as it passed behind the Moon, it was farther away than was originally believed.
By the 19th century, the resolution of telescopes reached a level sufficient for surface features to be identified. In September 1877, a perihelic opposition of Mars occurred on September 5. In that year, Italian astronomer Giovanni Schiaparelli, then in Milan, used a 22 cm telescope 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.
Influenced by the observations, the orientalist Percival Lowell founded an observatory which had a 300 and 450 mm telescope. 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. The canali were also found by other astronomers, like Henri Joseph Perrotin and Louis Thollon in Nice, using one of the largest telescopes of that time.
The seasonal changes (consisting of the diminishing of the polar caps and the dark areas formed during Martian summer) in combination with the canals lead to speculation about life on Mars, and it was a long held belief that Mars contained vast seas and vegetation. The telescope never reached the resolution required to give proof to any speculations. However, as bigger telescopes were used, fewer long, straight canali were observed. During an observation in 1909 by Flammarion with a 840 mm telescope, irregular patterns were observed, but no canali were seen.
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 have been published.
It was not until spacecraft visited the planet during NASA's Mariner missions in the 1960s that these myths were dispelled. The results of the Viking life-detection experiments started an intermission in which the hypothesis of a hostile, dead planet was generally accepted.
Some maps of Mars were made using the data from these missions, but it was not until the Mars Global Surveyor mission, launched in 1996 and operated until late 2006, that complete, extremely detailed maps were obtained. These maps are now available online, for example, at Google Mars.
Mars is named after the Roman god of war. In Babylonian astronomy, the planet was named after Nergal, their deity of fire, war, and destruction, most likely due to the planet's reddish appearance. When the Greeks equated Nergal with their god of war, Ares, they named the planet Ἄρεως ἀστἡρ (Areos aster), or "star of Ares". Then, following the identification of Ares and Mars, it was translated into Latin as stella Martis, or "star of Mars", or simply Mars. The Greeks also called the planet Πυρόεις Pyroeis meaning "fiery". In Hindu mythology, Mars is known as Mangala (मंगल). The planet is also called Angaraka in Sanskrit, after the celibate god of war, who possesses the signs of Aries and Scorpio, and teaches the occult sciences. The planet was known by the Egyptians as "Ḥr Dšr";;;; or "Horus the Red". The Hebrews named it Ma'adim (מאדים) — "the one who blushes"; this is where one of the largest canyons on Mars, the Ma'adim Vallis, gets its name. It is known as al-Mirrikh in Arabic, and Merih in Turkish. In Urdu and Persian it is written as مریخ and known as "Merikh". The etymology of al-Mirrikh is unknown. Ancient Persians named it Bahram, the Zoroastrian god of faith and it is written as بهرام. Ancient Turks called it Sakit. The Chinese, Japanese, Korean and Vietnamese cultures refer to the planet as 火星, or the fire star, a name based on the ancient Chinese mythological cycle of Five elements.astrological symbol of Mars, is a circle with a small arrow pointing out from behind. It is a stylized representation of a shield and spear used by the Roman God Mars. Mars in Roman mythology was the God of War and patron of warriors. This symbol is also used in biology to describe the male sex, and in alchemy to symbolise the element iron which was considered to be dominated by Mars whose characteristic red colour is coincidentally due to iron oxide. ♂ occupies Unicode position U+2642.
The popular idea that Mars was populated by intelligent Martians exploded 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.
Many other observations and proclamations by notable personalities added to what has been termed "Mars Fever". In 1899 while investigating atmospheric radio noise using his receivers in his Colorado Springs lab, inventor Nikola Tesla observed repetitive signals that he later surmised might have been radio communications coming from another planet, possibly Mars. In a 1901 interview Tesla said:
It was some time afterward when the thought flashed upon my mind that the disturbances I had observed might be due to an intelligent control. Although I could not decipher their meaning, it was impossible for me to think of them as having been entirely accidental. The feeling is constantly growing on me that I had been the first to hear the greeting of one planet to another.
Tesla's theories gained support from Lord Kelvin who, while visiting the United States in 1902, was reported to have said that he thought Tesla had picked up Martian signals being sent to the United States. However, Kelvin "emphatically" denied this report shortly before departing America: "What I really said was that the inhabitants of Mars, if there are any, were doubtless able to see New York, particularly the glare of the electricity."
In a New York Times article in 1901, Edward Charles Pickering, director of the Harvard College Observatory, said that they had received a telegram from Lowell Observatory in Arizona that seemed to confirm that Mars was trying to communicate with the Earth.
Early in December 1900, we received from Lowell Observatory in Arizona a telegram that a shaft of light had been seen to project from Mars (the Lowell observatory makes a specialty of Mars) lasting seventy minutes. I wired these facts to Europe and sent out neostyle copies through this country. The observer there is a careful, reliable man and there is no reason to doubt that the light existed. It was given as from a well-known geographical point on Mars. That was all. Now the story has gone the world over. In Europe it is stated that I have been in communication with Mars, and all sorts of exaggerations have spring up. Whatever the light was, we have no means of knowing. Whether it had intelligence or not, no one can say. It is absolutely inexplicable.
Pickering later proposed creating a set of mirrors in Texas with the intention of signaling Martians.
In recent decades, the high resolution mapping of the surface of Mars, culminating in Mars Global Surveyor, revealed no artifacts of habitation by 'intelligent' life, but pseudoscientific speculation about intelligent life on Mars continues from commentators such as Richard C. Hoagland. Reminiscent of the canali controversy, some speculations are based on small scale features perceived in the spacecraft images, such as 'pyramids' and the 'Face on Mars'. Planetary astronomer Carl Sagan wrote:
|“||Mars has become a kind of mythic arena onto which we have projected our Earthly hopes and fears.||”|
—Carl Sagan, Cosmos
- Main article: Mars in fiction
The depiction of Mars in fiction has been stimulated by its dramatic red color and by early scientific speculations that its surface conditions not only might support life, but intelligent life.
Thus originated a large number of science fiction scenarios, the best known of which is H. G. Wells' The War of the Worlds, published in 1898, in which Martians seek to escape their dying planet by invading Earth. A subsequent radio version of The War of the Worlds on October 30, 1938 was presented as a live news broadcast, and many listeners mistook it for the truth.
Also influential were Ray Bradbury's The Martian Chronicles, in which human explorers accidentally destroy a Martian civilization, Edgar Rice Burroughs' Barsoom series and a number of Robert A. Heinlein stories before the mid-sixties.
A comic figure of an intelligent Martian, Marvin the Martian, appeared on television in 1948 as a character in the Looney Tunes animated cartoons of Warner Brothers, and has continued as part of popular culture to the present.
Author Jonathan Swift made reference to the moons of Mars, about 150 years before their actual discovery by Asaph Hall, detailing reasonably accurate descriptions of their orbits, in the 19th chapter of his novel Gulliver's Travels.
Another reference is found in Clive Staples Lewis's Space Trilogy, and in particular in the first book entitled Out of the Silent Planet (1938). Three men, Weston, Devine and Ransom, set out for an interplanetary voyage from Earth to Mars (called Malacandra in the narrative). Ransom, who had been brought along forcefully by Weston and Devine, in order to be handed over to the Sorns, succeeds in escaping after they have landed on the red planet, and thus comes to discover the geology, flora, fauna, and cultures present on Malacandra. He also discovers the relationship of planet Earth (called Thulcandra, the silent planet, in the narrative) with the other planets and forms of life present in the Solar System.
After the Mariner and Viking spacecraft had returned pictures of Mars as it really is, an apparently lifeless and canal-less world, these ideas about Mars had to be abandoned and a vogue for accurate, realist depictions of human colonies on Mars developed, the best known of which may be Kim Stanley Robinson's Mars trilogy. However, pseudo-scientific speculations about the Face on Mars and other enigmatic landmarks spotted by space probes have meant that ancient civilizations continue to be a popular theme in science fiction, especially in film.
Another popular theme, particularly among American writers, is the Martian colony that fights for independence from Earth. This is a major plot element in the novels of Greg Bear and Kim Stanley Robinson, as well as the movie Total Recall (based on a short story by Philip K. Dick) and the television series Babylon 5. Many video games also use this element, including Red Faction and the Zone of the Enders series. Mars (and its moons) were also the setting for the popular Doom video game franchise and the later Martian Gothic.
- 2007 WD5 – asteroid that had a possible impact with Mars on January 30, 2008
- Colonization of Mars
- Darian calendar – system of time-keeping
- Extraterrestrial life
- List of artificial objects on Mars
- List of chasmata on Mars
- List of craters on Mars
- List of valles on Mars
- Terraforming of Mars
- ^ Best fit ellipsoid
- ^ There are many serpentinization reactions. Olivine is a solid solution between forsterite and fayalite whose general formula is . The reaction producing methane from olivine can be written as: Forsterite + Fayalite + Water + Carbonic acid → Serpentine + Magnetite + Methane , or (in balanced form): →
- ↑ 1.0 1.1 Ashley Yeager (July 19, 2008). "Impact May Have Transformed Mars". ScienceNews.org. Retrieved on 2008-08-12.
- ↑ 2.0 2.1 Ian Sample (June 26, 2008). "Cataclysmic impact created north-south divide on Mars". Science @ guardian.co.uk. Retrieved on 2008-08-12.
- ↑ Trudy E. Bell and Tony Phillips (March 12, 2002). "Once Upon a Water Planet". Science @ NASA. Retrieved on 2008-06-21.
- ↑ 4.0 4.1 Water ice in crater at Martian north pole http://www.esa.int/SPECIALS/Mars_Express/SEMGKA808BE_0.html
- ↑ Scientists Discover Concealed Glaciers on Mars at Mid-Latitudes http://www.jsg.utexas.edu/news/rels/112008.html
- ↑ 6.0 6.1 NASA (July 31, 2008). "NASA Spacecraft Confirms Martian Water, Mission Extended". Science @ NASA. Retrieved on 2008-08-01.
- ↑ "NASA Images Suggest Water Still Flows in Brief Spurts on Mars". NASA/JPL (December 6, 2006). Retrieved on 2007-01-04.
- ↑ Webster, G.; Beasley, D. (September 20, 2005). "Orbiter's Long Life Helps Scientists Track Changes on Mars". NASA. Retrieved on 2007-02-26.
- ↑ 9.0 9.1 9.2 9.3 9.4 David R. Williams (September 1, 2004). "Mars Fact Sheet". National Space Science Data Center. NASA. Retrieved on 2006-06-24.
- ↑ Peplow, Mark. "How Mars got its rust". Retrieved on 2007-03-10.
- ↑ Christensen, Philip R.; et al. (2003-06-27). "Morphology and Composition of the Surface of Mars: Mars Odyssey THEMIS Results". Science 300 (5628): 2056–2061. doi:10.1126/science.1080885. PMID 12791998.
- ↑ Golombek, Matthew P. (2003-06-27). "The Surface of Mars: Not Just Dust and Rocks". Science 300 (5628): 2043–2044. doi:10.1126/science.1082927. PMID 12829771.
- ↑ Goddard Space Flight Center. "New Map Provides More Evidence Mars Once Like Earth". Retrieved on 2006-03-17.
- ↑ Dave Jacqué (2003-09-26). "APS X-rays reveal secrets of Mars' core" (in English), Argonne National Laboratory. Retrieved on 1 July 2006.
- ↑ "Mars avalanche caught on camera". Discovery Channel. Discovery Communications (2008-03-04). Retrieved on 2009-03-04.
- ↑ "Giant Asteroid Flattened Half of Mars, Studies Suggest". Scientific American. Retrieved on 2008-06-27.
- ↑ "Huge Meteor Strike Explains Mars’s Shape, Reports Say", New York Times. Retrieved on 27 June 2008.
- ↑ "Martian soil 'could support life'", BBC News (June 27, 2008). Retrieved on 7 August 2008.
- ↑ Chang, Alicia. "Scientists: Salt in Mars soil not bad for life", Associated Press. Retrieved on 7 August 2008.
- ↑ "NASA Spacecraft Analyzing Martian Soil Data". JPL. Retrieved on 2008-08-05.
- ↑ 21.0 21.1 Haberle, R. M.; et al. (2001). "On the possibility of liquid water on present-day Mars". J. Geophys. Res.. Retrieved on 2006-10-06. 106(E10), 23,317–23,326. (abstract, full paper requires purchase or AGU subscription)
- ↑ Heldmann, Jennifer L.; et al. (2005-05-07), "Formation of Martian gullies by the action of liquid water flowing under current Martian environmental conditions" (PDF), Journal of Geophysical Research 110: Eo5004, doi:10.1029/2004JE002261, http://daleandersen.seti.org/Dale_Andersen/Science_articles_files/Heldmann%20et%20al.2005.pdf, retrieved on 17 September 2008 'conditions such as now occur on Mars, outside of the temperature-pressure stability regime of liquid water' … 'Liquid water is typically stable at the lowest elevations and at low latitudes on the planet because the atmospheric pressure is greater than the vapor pressure of water and surface temperatures in equatorial regions can reach 273 K for parts of the day [Haberle et al., 2001]'
- ↑ 23.0 23.1 Kostama, V.-P.; Kreslavsky, M. A.; Head, J. W. (June 3, 2006), "Recent high-latitude icy mantle in the northern plains of Mars: Characteristics and ages of emplacement", Geophysical Research Letters 33: L11201, doi:10.1029/2006GL025946, http://www.agu.org/pubs/crossref/2006/2006GL025946.shtml, retrieved on 12 August 2007 'Martian high-latitude zones are covered with a smooth, layered ice-rich mantle'
- ↑ "Mars' South Pole Ice Deep and Wide". NASA (March 15, 2007). Retrieved on 2007-03-16.
- ↑ Scientists Discover Concealed Glaciers on Mars at Mid-Latitudes http://www.jsg.utexas.edu/news/rels/112008.html
- ↑ Murray, John B.; et al. (March 17, 2005), "Evidence from the Mars Express High Resolution Stereo Camera for a frozen sea close to Mars' equator", Nature 434: 352–356, doi:10.1038/nature03379
- ↑ Kerr, Richard A. (March 4, 2005), "Ice or Lava Sea on Mars? A Transatlantic Debate Erupts", Science 307: 1390–1391, doi:10.1126/science.307.5714.1390a, PMID 15746395
- ↑ 28.0 28.1 Jaeger, W. L.; et al. (September 21, 2007), "Athabasca Valles, Mars: A Lava-Draped Channel System", Science 317: 1709–1711, doi:10.1126/science.1143315, PMID 17885126
- ↑ Boynton, W. V.; et al. (in press), "Concentration of H, Si, Cl, K, Fe, and Th in the low and mid latitude regions of Mars", Journal of Geophysical Research, Planets 112: E12S99, doi:10.1029/2007JE002887
- ↑ Feldman, W. C.; et al. (November 30, 2005), "Topgraphic control of hydrogen deposits at low latitudes to midlatitudes of Mars", Journal of Geophysical Research 110: E11009, doi:10.1029/2005JE002452
- ↑ Malin, Michael C. (June 30, 2000). "Evidence for Recent Groundwater Seepage and Surface Runoff on Mars". Science 288: 2330–2335. doi:10.1126/science.288.5475.2330. PMID 10875910.
- ↑ "NASA Images Suggest Water Still Flows in Brief Spurts on Mars". NASA (December 6, 2006). Retrieved on 2006-12-06.
- ↑ "Water flowed recently on Mars", BBC (December 6, 2006). Retrieved on 6 December 2006.
- ↑ "Water May Still Flow on Mars, NASA Photo Suggests", NASA (December 6, 2006). Retrieved on 30 April 2006.
- ↑ NASA (March 3, 2004). "Mineral in Mars 'Berries' Adds to Water Story". Press release. Retrieved on 13 June 2006.
- ↑ McEwen, A. S.; et al. (September 21, 2007). "A Closer Look at Water-Related Geologic Activity on Mars". Science 317: 1706–1709. doi:10.1126/science.1143987. PMID 17885125.
- ↑ Sheehan, William. "Areographers". The Planet Mars: A History of Observation and Discovery. Retrieved on 2006-06-13.
- ↑ "Viking and the Resources of Mars" (PDF). Humans to Mars: Fifty Years of Mission Planning, 1950–2000. Retrieved on 2007-03-10.
- ↑ "Topography". Think Quest. Retrieved on 2007-03-13.
- ↑ Frommert, H.; Kronberg, C.. "Christiaan Huygens". Retrieved on 2007-03-10.
- ↑ Wright, Shawn (April 4, 2003). "Infrared Analyses of Small Impact Craters on Earth and Mars". University of Pittsburgh. Retrieved on 2007-02-26.
- ↑ "Mars Global Geography". Windows to the Universe. Retrieved on 2006-06-13.
- ↑ Wetherill, G. W. (1999). "Problems Associated with Estimating the Relative Impact Rates on Mars and the Moon". Earth, Moon, and Planets 9: 227. doi:10.1007/BF00565406, http://adsabs.harvard.edu/abs/1974Moon....9..227W. Retrieved on 26 February 2007.
- ↑ Lucchitta, B. K.; Rosanova, C. E. (August 26, 2003). "Valles Marineris; The Grand Canyon of Mars". USGS. Retrieved on 2007-03-11.
- ↑ G. E. Cushing, T. N. Titus, J. J. Wynne, P. R. Christensen. (2007). "Themis Observes Possible Cave Skylights on Mars" (PDF). Lunar and Planetary Science XXXVIII. Retrieved on 2007-08-02.
- ↑ "'Cave entrances' spotted on Mars". NAU. Retrieved on 2007-05-28.
- ↑ "Researchers find possible caves on Mars", Paul Rincon of BBC News. Retrieved on 28 May 2007.
- ↑ Philips, Tony (2001). "The Solar Wind at Mars". Science@NASA. Retrieved on 2006-10-08.
- ↑ R. Lundin, S. Barabash, H. Andersson, M. Holmström, A. Grigoriev, M. Yamauchi, J.-A. Sauvaud, A. Fedorov, E. Budnik, J.-J. Thocaven,2 D. Winningham, R. Frahm, J. Scherrer, J. Sharber, K. Asamura, H. Hayakawa, A. Coates, D. R. Linder, C. Curtis, K. C. Hsieh, B. R. Sandel, M. Grande, M. Carter, D. H. Reading, H. Koskinen, E. Kallio, P. Riihela, W. Schmidt, T. Säles, J. Kozyra, N. Krupp, J. Woch, J. Luhmann, S. McKenna-Lawler, R. Cerulli-Irelli, S. Orsini, M. Maggi, A. Mura, A. Milillo, E. Roelof, D. Williams, S. Livi, P. Brandt, P. Wurz, P. Bochsler (2004). "Solar Wind-Induced Atmospheric Erosion at Mars: First Results from ASPERA-3 on Mars Express". Science 305: 1933–1936. doi:10.1126/science.1101860. PMID 15448263.
- ↑ Lemmon; et al. (2004). "Atmospheric Imaging Results from Mars Rovers". Science 306: 1753–1756. doi:10.1126/science.1104474. PMID 15576613.
- ↑ V. Formisano, S. Atreya, T. Encrenaz, N. Ignatiev, M. Giuranna (2004). "Detection of Methane in the Atmosphere of Mars". Science 306: 1758–1761. doi:10.1126/science.1101732. PMID 15514118.
- ↑ "Mars Express confirms methane in the Martian atmosphere", ESA (March 30, 2004). Retrieved on 17 March 2006.
- ↑ Martin Baucom (2006). "Life on Mars?". American Scientist 94 (2): 119–120, http://www.americanscientist.org/template/AssetDetail/assetid/49613. Retrieved on 26 February 2007.
- ↑ 54.0 54.1 C. Oze, M. Sharma (2005). "Have olivine, will gas: Serpentinization and the abiogenic production of methane on Mars". Geophys. Res. Lett. 32: L10203. doi:10.1029/2005GL022691.
- ↑ J. T. Mellon, W. C. Feldman, T. H. Prettyman (2003). "The presence and stability of ground ice in the southern hemisphere of Mars". Icarus 169 (2): 324–340. doi:10.1016/j.icarus.2003.10.022, http://adsabs.harvard.edu/abs/2004Icar..169..324M. Retrieved on 26 February 2007.
- ↑ "Mars Rovers Spot Water-Clue Mineral, Frost, Clouds", NASA (December 13, 2004). Retrieved on 17 March 2006.
- ↑ "Mars' desert surface...". MGCM Press release. NASA. Retrieved on 2007-02-25.
- ↑ Goodman, Jason C (September 22, 1997). "The Past, Present, and Possible Future of Martian Climate". MIT. Retrieved on 2007-02-26.
- ↑ Philips, Tony (July 16, 2001). "Planet Gobbling Dust Storms". Science @ NASA. Retrieved on 2006-06-07.
- ↑ Darling, David. "Mars, polar caps, ENCYCLOPEDIA OF ASTROBIOLOGY, ASTRONOMY, AND SPACEFLIGHT". Retrieved on 2007-02-26.
- ↑ "MIRA's Field Trips to the Stars Internet Education Program". Mira.org. Retrieved on 2007-02-26.
- ↑ Carr, Michael H. (2003). "Oceans on Mars: An assessment of the observational evidence and possible fate". Journal of Geophysical Research 108 (5042): 5042. doi:10.1029/2002JE001963, http://adsabs.harvard.edu/abs/1998RPPh...61...77K. Retrieved on 26 February 2007.
- ↑ Phillips, Tony. "Mars is Melting, Science at NASA". Retrieved on 2007-02-26.
- ↑ J. J. Plaut, G. Picardi, A. Safaeinili, A. B. Ivanov, S. M. Milkovich, A. Cicchetti, W. Kofman, J. Mouginot, W. M. Farrell, R. J. Phillips, S. M. Clifford, A. Frigeri, R. Orosei, C. Federico, I. P. Williams, D. A. Gurnett, E. Nielsen, T. Hagfors, E. Heggy, E. R. Stofan, D. Plettemeier, T. R. Watters, C. J. Leuschen, P. Edenhofer (2007). "Subsurface Radar Sounding of the South Polar Layered Deposits of Mars". Science 315: 92. doi:10.1126/science.1139672. PMID 17363628.
- ↑ Pelletier J. D. (2004). "How do spiral troughs form on Mars?". Geology 32: 365–367. doi:10.1130/G20228.2, http://www.gsajournals.org/perlserv/?request=get-abstract&doi=10.1130%2FG20228.2. Retrieved on 27 February 2007.
- ↑ "MarsToday.Com". Mars Polar Cap Mysery Solved. Retrieved on 2007-01-23.
- ↑ "Mars' Orbital eccentricity over time". Solex. Universita' degli Studi di Napoli Federico II (2003). Retrieved on 2007-07-20.
- ↑ 68.0 68.1 Jean Meeus (March 2003). "When Was Mars Last This Close?". International Planetarium Society. Retrieved on 2008-01-18.
- ↑ Ron Baalke (August 22, 2003). "Mars Makes Closest Approach In Nearly 60,000 Years". meteorite-list. Retrieved on 2008-01-18.
- ↑ "Close Inspection for Phobos". ESA website. Retrieved on 2006-06-13.
- ↑ "ARES ATTENDANTS: DEIMOS & PHOBOS". Greek Mythology. Retrieved on 2006-06-13.
- ↑ 72.0 72.1 Arnett, Bill (November 20, 2004). "Phobos". nineplanets. Retrieved on 2006-06-13.
- ↑ Ellis, Scott. "Geological History: Moons of Mars". CalSpace. Archived from the original on 2007-05-17. Retrieved on 2007-08-02.
- ↑ http://www.space.com/scienceastronomy/streaks_mars_021211.html
- ↑ A Study of Mars Global Surveyor (MGS), Mars Orbital Camera (MOC) Images Showing Probable Water Seepages. Are They Dust Slides as NASA Claims or Proof of Water on Mars? By Efrain Palermo, Jill England and Harry Moore, 2001
- ↑ Robert L. Nowack. "Estimated Habitable Zone for the Solar System". Department of Earth and Atmospheric Sciences at Purdue University. Retrieved on 2009-04-10.
- ↑ Helen Briggs (BBC science reporter, Boston) (February 15, 2008). "Early Mars 'too salty' for life", BBC News. Retrieved on 16 February 2008.
- ↑ Hannsson, Anders (1997). Mars and the Development of Life., Wiley. ISBN 0-471-96606-1.
- ↑ "New Analysis of Viking Mission Results Indicates Presence of Life on Mars", Physorg.com (January 7, 2007). Retrieved on 2 March 2007.
- ↑ "Phoenix Returns Treasure Trove for Science". NASA/JPL (2008-06-26). Retrieved on 2008-06-27.
- ↑ Vladimir A. Krasnopolsky, Jean-Pierre Maillard, Tobias C. Owen (2004). "Detection of methane in the Martian atmosphere: evidence for life?". Icarus 172: 537–547. doi:10.1016/j.icarus.2004.07.004.
- ↑ "Formaldehyde claim inflames Martian debate", Nature (February 25, 2005). Retrieved on 19 March 2006.
- ↑ Dinerman, Taylor (September 27, 2004). "Is the Great Galactic Ghoul losing his appetite?". The space review. Retrieved on 2007-03-27.
- ↑ "Mariner 9: Overview". NASA.
- ↑ "Other Mars Missions". Journey through the galaxy. Retrieved on 2006-06-13.
- ↑ "Mars Global Surveyor", CNN- Destination Mars. Retrieved on 13 June 2006.
- ↑ "Mars Pulls Phoenix In". University of Arizona Phoenix mission Website. Retrieved on 2008-05-25.
- ↑ "Phoenix: The Search for Water". NASA website. Retrieved on 2007-03-03.
- ↑ "Frozen Water Confirmed on Mars". UANews.org. Retrieved on 2008-08-24.
- ↑ "NASA Mars Mission declared dead", BBC (November 10, 2008). Retrieved on 10 November 2008.
- ↑ "NASA's Mars Odyssey Shifting Orbit for Extended Mission". nasa.com (October 9, 2008). Retrieved on 2008-11-15.
- ↑ Britt, Robert (March 14, 2003). "Odyssey Spacecraft Generates New Mars Mysteries". Space.com. Retrieved on 2006-06-13.
- ↑ Wardell, Jane (January 26, 2004). "Europe's Beagle 2 Mars Probe Stays Ominously Silent". Space.com. Retrieved on 2006-06-13.
- ↑ 94.0 94.1 Bertaux, Jean-Loup; et al. (June 9, 2005). "Discovery of an aurora on Mars". Nature Magazine. Retrieved on 2006-06-13.
- ↑ "Mars Exploration Rovers- Science". NASA MER website. Retrieved on 2006-06-13.
- ↑ "Photo shows avalanche on Mars". CNN. Retrieved on 2008-03-04.
- ↑ "Mars Science Laboratory". NASA's MSL website. Retrieved on 2007-03-03.
- ↑ Rincon, Paul (November 10, 2006). "European Mars launch pushed back". Retrieved on 10 October 2006.
- ↑ NASA Selects 'MAVEN' Mission to Study Mars Atmosphere
- ↑ "Introduction to the MetNet Mars Mission". Finnish Meteorological Institute. Retrieved on 2008-08-28.
- ↑ 101.0 101.1 "The MetNet Mars Precursor Mission". Finnish Meteorological Institute. Retrieved on 2008-08-28.
- ↑ Britt, Robert. "When do we get to Mars?". Space.com FAQ: Bush's New Space Vision. Retrieved on 2006-06-13.
- ↑ "NASA aims to put man on Mars by 2037", AFP. (Bad link)
- ↑ "Liftoff for Aurora: Europe’s first steps to Mars, the Moon and beyond" (October 11, 2002). Retrieved on 2007-03-03.
- ↑ "Deimos". Planetary Societies's Explore the Cosmos. Retrieved on 2006-06-13.
- ↑ lloyd, john; john mitchinson (2006). The QI Book of General Ignorance. Britain: faber and faber limited. p. 102. ISBN 978-0-571-24139-2, http://en.wikipedia.org/wiki/The_Book_of_General_Ignorance.
- ↑ "Mars Observing FAQ". Shallow Sky. Retrieved on 2006-06-15.
- ↑ Rao, Joe (August 22, 2003). "NightSky Friday – Mars and Earth: The Top 10 Close Passes Since 3000 B.C.". Space.com. Retrieved on 2006-06-13.
- ↑ Breyer, Stephen (March 1979). "Mutual Occultation of Planets". Sky and Telescope 57 #3: 220.
- ↑ Snyder, Dave (May 2001). "An Observational History of Mars". Retrieved on 2007-02-26.
- ↑ Sagan, Carl (1980). Cosmos. New York, USA: Random House. p. 107. ISBN 0394502949.
- ↑ Zahnle K. (2001). "Decline and fall of the Martian empire". Nature 412: 209–213. doi:10.1038/35084148.
- ↑ Salisbury F. B. (1962). "Martian Biology". Science (journal) 136 (3510): 17–26, http://links.jstor.org/sici?sici=0036-8075%2819620406%293%3A136%3A3510%3C17%3AMB%3E2.0.CO%3B2-R. Retrieved on 26 February 2007.
- ↑ Sheehan, William (February 2, 1997). "Motions of Mars". The Planet Mars: A History of Observation and Discovery. Retrieved on 2006-06-13.
- ↑ "Planet Symbols". NASA solar system exploration. Retrieved on 2006-06-13.
- ↑ "Percivel Lowell's Canals". Retrieved on 2007-03-01.
- ↑ Fergus, Charles (May 2004). "Mars Fever". Research/Penn State 24 (2), http://www.rps.psu.edu/0305/mars.html. Retrieved on 2 August 2007.
- ↑ Tesla, Nikola (February 19, 1901). "Talking with the Planets". Collier's Weekly. Retrieved on 2007-05-04.
- ↑ Cheney, Margaret (1981). Tesla, man out of time. Englewood Cliffs, New Jersey: Prentice-Hall. p. 162. ISBN 978-0-13-906859-1. OCLC 7672251.
- ↑ "Departure of Lord Kelvin", The New York Times, May 11, 1902, p.29.
- ↑ 121.0 121.1 Professor Pickering (January 16, 1901). "The Light Flash From Mars" (PDF). The New York Times. Archived from the original on 2007-05-20. Retrieved on 2007-05-20.
- ↑ Sagan, Carl (1980). Cosmos. New York, USA: Random House. p. 106. ISBN 0394502949.
- ↑ "Radio's War of the Worlds Broadcast (1938)". Retrieved on 2007-03-01.
- ↑ "Swift, Jonathan and the moons of Mars". David Darling. Retrieved on 2007-03-01.
- ↑ Kathy Miles and Charles F Peters II. "Unmasking the Face". Retrieved on 2007-03-01.
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Learning resources from Wikiversity
- 3D maps of Mars in NASA World Wind
- Google Mars – Interactive image of Mars
- Guide to Mars – information about Mars and how to observe it.
- Nine Planets Mars page
- On Mars: Exploration of the Red Planet 1958–1978 from the NASA History Office.
- Martian Law – a CATO white paper
- Computer Simulation of a flyby through Mariner Valley
- Mars Unearthed – Comparisons of terrains between Earth and Mars
- Ralph Aeschliman's Online Atlas of Mars
- Be on Mars – Anaglyphs from the Mars Rovers (3D)
- NASA/JPL OnMars WMS Server for Mars Data – Work as Google Earth client overlays
- Exploring Mars: Image Center
- Mars Astronomy Cast episode #52, includes full transcript.
- BBC News update on Mars Express' findings of polar water ice and water-eroded features on the surface
- BBC News Mars pictures reveal frozen sea
- Feb 07: ESA Prepares for a Human Mission to Mars
- Mars' apparent relative size at opposition as seen by HST
- Mars articles in Planetary Science Research Discoveries
- Flight Into Mariner Valley – NASA/JPL/Arizona State University 3D flythrough of Valles Marineris
- Geody Mars – World's search engine that supports NASA World Wind, Celestia, and other applications
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