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Mars, Mars, Mars:
Exploring Mars



The time is well within living memory when the idea of humans sending a spacecraft to Mars was considered idle fancy--science-fictional nonsense--perhaps something for the far future. That far future turned out to be not so far off after all: the first attempts were made as early as 1960, and by 1965 we had successfully placed a craft in orbit around Mars. By 1971, we had hardware actually arrive on the surface of Mars, though that year's two probes only crash-landed. By 1976, we were reliably getting good-quality photographs and other data from the surface of Mars. What an incredible journey!

Overview

Our explorations of Mars were once limited to what the unaided human eye could see in the night skies; in that era, which lasted till the invention of the telescope about four hundred years ago, our knowledge of Mars didn't go far beyond that it was a bright red point in the sky that--like only a very few others--didn't behave like a star. Only toward the end of that era was did we even start to realize that those few "wanderers", and our own Earth, revolved around the Sun. With the coming of the optical telescope, and--in later years--other remote-sensing devices, we discovered much about the universe in general and planets and Mars in particular. But not till we were able to actually send our instruments out to Mars, first to its planetary neighborhood, then actually down onto its surface, were we able to discover the answers to many age-old questions--as well as a whole new stack of questions to ask.



Google now offers interactive maps of Mars.

Maps, plus lots of other information, too--another great Mars resource.

Start your visit at Google Mars.


Mars Exploration

The rocket scientist and popular author Willy Ley, writing over half a century ago in The Conquest of Space (an excellent book even today, made all the more wonderful owing to the many plates of beautiful illustrations by Chesley Bonestell), observed that the history of astronomy could be divided into three eras: naked-eye observation; observation with instruments (including but not limited to telescopes); and direct observation, meaning "going there"--which last, in Ley's time, was still wishful thinking. Let us use that concept to lay out our look at the human exploration of Mars.


Naked-Eye "Exploration"

From the dawn of humanity, folk have been looking at the night skies. Every civilization has quickly noted that of the points of light in those skies, the vast majority--what we know as "stars"--were fixed, as if the sky were a sphere with us at its center and the stars painted onto the inside of that sphere, with the sphere rotating about our position. (Many early views of the construction of the universe reflected that view--the page of this site on Mars in history and culture has much more on that topic.) But they also noticed that several of those points seemed to wander about the fixed stars. Those "wanderers" were the planets. Two of them--what we today know as Mercury and Venus--could, for various reasons, only be seen in early evening and early dawn, and thus were each usually wrongly thought of as two distinct astral bodies. The three others--what we today know as Mars, Jupiter, and Saturn--were always understood each to be a single celestial body.

Ideas of what the planets were varied from culture to culture, but none bore any remotest relation to reality (there is considerably more information on this aspect of the human understandings of Mars in this site's page on Mars in history and culture

Illustration of the Ptolemaic view of the universe

In this "first era" of the "exploration" of Mars, the only real knowledge about the planet concerned its apparent movements in the sky relative to the background of "fixed" stars. The movements of the planets deeply puzzled the ancients, because they seemed quite erratic, each planet seeming first to speed up in its movement, then slow down and fall back. The crux of their problem in understanding was that they all thought that the Earth was necessarily the center of the universe, a belief amply summed up in the Ptolemaic system (after Claudius Ptolemaeus, who documented it in his work The Almagest), which for a thousand years or more dominated Western thought about cosmology. (See illustration at left.) But the impossibility of reconciling what was before their eyes to that simplistic scheme led to ever-more ludicrous "fixes" that made an already intolerably complicated system yet worse. (There is a famous remark made by Alfonso X, king of Castile in 1175 A.D., known to history as "Alfonso the Wise", on the Ptolemaic system--for which Alfonso later commissioned improved tables--that "If the Lord Almighty had consulted me before embarking on creation, I should have recommended something simpler.")

The one thing the ancients did know was the historical track of all the chief bodies visible in the skies, and they compiled immense tables of data on those movements, from which often they could make predictions of astronomical events. But these tables were just mechanics, not understanding--the planets were just bright dots in the sky.

Toward the end of this first era of astronomy came a development destined to be of significance to later understandings of Mars and the cosmos in general. In 1543, the noted Polish astronomer Nicolaus Copernicus published a work many decades in the making, De Revolutionibus Orbium Coelestium, http://omniknow.com/common/wiki.php?in=en&term=Nicolaus_Copernicus in which he set forth what we today call the Copernican or "heliocentric" model of the cosmos. It put the Sun, not the Earth, at the center of the universe, and correspondingly held that the Earth and all other heavenly bodies rotated around the Sun. His work, though not the first to set forth such a position, was the first to set it forth in a detailed, useful, coherent form. This blast at the old systems, which had insisted--and long continued to insist--that our Earth was the centrum of all the cosmos, though not much celebrated when first proposed, essentially marked the beginning of the modern era of science.


Instrumented "Exploration"

Galileo's telescope

The second age of astronomy arrived with the discovery of the telescope, and it almost immediately brought great leaps forward in human understanding of the heavens, most notably an eventual shift away from the classic Earth-centered view of the universe to a much more realistic Sun-centered view. The shift was not accomplished without major clashes, but we will reserve a fuller discussion of those to the page on Mars in history and culture.

This era, which took our view of Mars from that of a bright point of light in the sky to that of another world far off in space, lasted only a relatively brief three and a half centuries. Moreover, progress occurred mainly in the early decades of that era, real additions to knowledge (as opposed to continuing small refinements of what was already known) becoming progressively fewer and fewer over time. The reason for that is the inherent limitation of trying to view a far-off astronomical body from beneath a thick atmosphere; the character of Earth's atmosphere places significant limits on the ability of any ground-based telescope to acquire data. In the early years of this era, the telescope opened up new vistas, and each increase in the power of available telescopes augmented those vistas; but eventually--and relatively early on at that--the magnifying power of telescopes reached the limits that atmospheric distortion necessarily imposes. (The smaller the detail one is trying to pick out, the more the effects of distortion--from heat-generated ripples in the air, as exemplified by stars' "twinkling", to simple haze--will interfere with viewing.)

The first known use of a telescope for astronomical purposes was in 1609 (the instrument was only invented the year before, 1608, in the Netherlands, or perhaps even earlier), when that genius Galileo turned his augmented gaze on the heavens soon discovered many new things; most immediately, he looked at the Moon, and observed mountains and valleys there, making it plain that the Moon is a "world" at least somewhat comparable to our own. (At right: Galileo's telescope.)

Another important discovery that Galileo made was that the planet Venus exhibited phases just as the Moon does; that was critical information, because it was something impossible under the then-extant Earth-centered view of the universe. At that time, though Copernicus had published his Sun-centered theory of the universe two-thirds of a century earlier, that theory was widely considered to be just an interesting mathematical exercise, rather than an actual description of reality; but evidences such as Galileo's--the Venusian phases, and the fact that a planet could have objects going round it (In 1610, Galileo had discovered the four major moons of Jupiter)--began to give plausibility to the system being literally true.

Meanwhile, in the same year Galileo began his epochal telescopic survey of the heavens, the German astronomer and mathematician Johannes Kepler had made a relatively small yet highly significant correction to the Copernican system, a correction that vastly simplified the problem of relating actual observation of the skies with the predictions of theory. Till then, the Copernican system had been largely ignored, for several reasons, perhaps the chiefest of which was that it was no less complicated (and perhaps even a bit more so) than the old Tychonian system of the Danish astronomer Tycho Brahe, who had finally updated old Ptolemy by adding to his system even more complexities--chiefly to try to account for the then-incomprehensible movements of the planets.

Kepler (using, ironically, copious tables of data compiled by Tycho) was able to educe what came to be known as "Kepler's Laws of Planetary Motion", the first of which stated that The orbit of a planet about the Sun is an ellipse with the Sun at one focus of the ellipse. By realizing that the orbits of astronomical bodies are not the perfectly circular paths that Copernicus (like all before him) had assumed, but rather were elliptical, Kepler at one stroke made the Sun-centered system relatively simple and in excellent accordance with what could actually be seen going on in the skies. (Kepler's work was later to be invaluable to Isaac Newton in his elucidation of the law of gravity and the laws of motion.)

In 1609 Galileo was also discovering significant things about Mars. The first and foremost, and perhaps most exciting, was that the telescope revealed that Mars was not simply a bright point, but was clearly a substantial sphere--in other words, that it was a world. Galileo also, by careful observation and record-keeping, established that Mars varied in apparent brightness and size on a regular, periodic basis; those data provided yet further substantial support to the Copernican Sun-centered theory.

Now came great clashes between the believers in the no-longer-tenable old Earth-centered system and the new Sun-centered system, most famously in the story of Galileo's persecution by the Church. But, as we noted above, our discussion of that history is elsewhere on this site. Here, we will simply recount the "second era's" major milestones in the advance of our real knowledge of Mars.

In 1659, the Dutch astronomer Christiaan Huygens, using a newer, more powerful telescope (which he designed), observed Mars and--by noting the periodic recurrence of a particular spot on Mars's surface (now thought to have been Syrtis Major)--correctly concluded that Mars has a 24-hour day (it is exactly 24.623 hours long: Huygens, almost 350 years ago, got it right to with better than 97% accuracy). And that already remarkable accuracy was bettered in 1666, when the Italian astronomer Giovanni Cassini calculated, from observations, the Martian day to be 24 hours and 40 minutes, almost perfect accuracy. In that same year, Cassini also became the first to note that Mars has a polar cap (this is the north polar ice cap).

solar diagram of Earth and Mars in opposition

Cassini later (by then working in France) made extensive observations and calculations that enabled him, in 1672, to calculate the distance from the Earth to Mars, and got it substantially correct. He made his measurement at a time when the Earth and Mars were "in opposition", meaning that they lay in a straight line out from the Sun (see diagram at left)--or, to oversimplify, when Mars was at about its closest approach to Earth (Mars is not always at the exact same distance when it is in opposition, but the distances from one opposition to another don't vary that much). The figure Cassini got--about 87 million miles, only about 6% to 7% low--was something of a shocker, for it made plain for the first time how truly huge "astronomical" distances are, and was thus another major step forward in the transition from the old, cozy view of the universe to the modern one.

In that same year of 1672, Huygens became the first observer to detect the south polar ice cap on Mars.

In 1704, the astronomer Giancomo Miraldi, using the new and--for its day--large and powerful Campani Telescope in the Paris Observatory, verified the existence of the polar caps of Mars, further noting that the south cap does not quite lie on the true south pole of Mars. Later, in 1719, Miraldi speculated (correctly, as it turns out) that the caps were constituted of ice (Mars was in that year at an especially close opposition to Earth, enabling correspondingly good telescopic viewing). Poor Miraldi--he seems almost forgotten today, though there is a lunar crater named after him--also reconfirmed the earlier measurements of the length of the Martian day.

Sir William Herschel, best remembered for his discovery of the planet Uranus in 1781, was shortly thereafter (1782) appointed the (British) "King's Astronomer" (something different from "Astronomer Royal", a title then held by Nevil Maskelyne, with whom Herschel was acquainted). As part of his wide-ranging astronomical studies, Herschel extensively examined Mars, using excellent telescopes that he built himself, including a reflector, a type much harder to make than the then-more-usual refractor; indeed, Herschel substantially advanced the art of telescope-making.

(Herschel's sister Caroline, for years his secretary and assistant, went on after his marriage to become an astronomer of some note in her own right.
portrait of Sir William Herschel

In 1784 Herschel (portrait at right) published the verbosely titled paper On the remarkable appearances at the polar regions on the planet Mars, the inclination of its axis, the position of its poles, and its spheroidal figure; with a few hints relating to its real diameter and atmosphere; in it, Herschel (perhaps to justify the length of that title) set forth much data--some refining known points, some more or less novel. Among his pronouncements:

· the Martian axial tilt is 30° (not bad--we now know it to be 25.19°);

· the length of the Martian day is 24 hours, 39 minutes, 22 seconds (only 14 seconds off);

· Mars has seasons like the Earth's save about twice as long--since the Martian year itself is about twice Earth's--and the periodic growth and shrinkage the polar ice caps are a consequence of the changes in the Martian seasons (which is so);

· the patterns of light and dark areas on the planet correspond to seas and dry land (very wrong);

· Mars has (he concluded from star-occultation observations) an atmosphere, though a thin one (correct); and,

· Mars is inhabited by intelligent creatures (Herschel believed that all the planets were so inhabited, even the Sun) who, he remarked, "probably enjoy a situation similar to our own" (quite wrong).

Though (as we will see below) diligent astronomers after Herschel continued to add bits and pieces to our knowledge of Mars--mostly by further refining already known data--there were few if any "great leaps forward" throughout the remainder of this era of astronomy. There was (as we document on another page of this site) a great deal of wild speculation and furious argument in that time, largely based on what each "expert" thought he had seen through his telescope. (Recall that there could be such wide disagreement because the telescope had by now largely reached the limits of its ability to discern detail, owing to unavoidable distortions from Earth's atmosphere.)

Here is a summary of some of the salient developments in actual knowledge of Mars during that period:

  • 1809: French astronomer Honore Flaugergues observes yellowish features on Mars, which he concludes are phenomena of the Martian atmosphere (rather than its actual surface); he is often credited with having thus been the first to see Martian dust clouds, though there is some dispute over what he actually saw.

  • 1813: Flaugergues notes that the polar ice caps appear to melt significantly during Mars's spring (and wrongly concludes that Mars is warmer than the Earth).

  • 1839: German astronomers Wilhelm Beer and Johann von Mädler issue a detailed map of Mars (they had earlier, in 1830, made the first globe of Mars) and announce an even more accurate determination of its day length (correct to within a mere tenth of a second).

  • 1858: Italian Jesuit priest and astronomer Angelo Secchi, director of the Vatican Observatory, prepares a new and improved map of Mars.

  • Proctor's map of Mars

    1867: British astronomer Richard Anthony Proctor publishes a yet newer map of Mars (see image), seeking to improve on Secchi's. Proctor was a map expert and a respected scientist and writer, but his map was soon to be surpassed. Proctor does not work from his own observations, but rather from a set of 27 drawings by British astronomical observer William Rutter Dawes. Proctor's map contains nonexistent "continents" and "oceans", and much nomenclature later superseded (see 1877, below). But his choice of zero meridian remains the accepted convention.

  • 1867: French astronomer Pierre Jules Janssen, British astronomer Sir William Huggins, and German astronomer Hermann Vogel independently each announce the detection by spectroscope of water vapor in the atmosphere of Mars--Janssen going so far as to tote his equipment almost 11,000 feet up, to the peak of Sicily's Mt. Etna, to get above the lower layer's of Earth's own atmosphere and so get supposedly more accurate results; later work (see 1894, below), though, will controvert these announcements.

  • 1877: The Italian astronomer Giovanni Schiaparelli issues an intricately detailed map of Mars, made from his own extensive observations. His terminology immediately eclipses that of the earlier Proctor map (see 1867, above), perhaps because it takes its colorful names from mythology (notably various designations for Hell) and from ancient history. Schiaparelli continues to elaborate this map over the next ten years or so, and its final version is a standard reference virtually till the third age of space exploration begins, and his names for nearly all the major features of Mars remain the standards today. But what makes this publication so critical to human ideas of Mars is its today-famous use of the Italian word canali--which simply means "channels" or "grooves"--for certain linear features he had noted; when his work is translated into English, the word is wrongly rendered as "canals", and so the infamous "canals of Mars" are born.

  • 1877: the American astronomer Asaph Hall discovers the two tiny moons of Mars (Phobos is about 13 miles across, and Deimos only 7 to 8 miles wide); Hall's names--meaning fear and dread--are, in Greek mythology, those of two sons of Ares, the war god (the Greek equivalent of the Roman god Mars).

  • The 36-inch telescope at Lick Observatory in 1890

    1894: American astronomer William Wallace Campbell at Lick Observatory (of which he will later become director), using a superior spectroscope and the Lick 36-inch refracting telescope (then the most powerful in the world--see photograph at right), finds that "the spectrum of Mars . . . appeared to be identical with that of the [airless] Moon in every respect," meaning that there seems to be no water vapor in Mars's atmosphere

  • 1909: Campbell (see above) repeats his earlier work with substantially more accurate equipment and again reports "From the first, I have had no confidence in their [see 1867, above] reported evidence of water vapor, and these spectrograms do not change my opinion."

  • 1920s: American astronomers Seth Nicholson and Edison Pettit at the Mount Wilson Observatory, using the new Hooker 100-inch telescope--till 1948 the most powerful in the world--make infrared observations of, among other celestial bodies, Mars; those measurements suggest that surface temperatures in the equatorial regions of Mars at noon hit 60° F., while temperatures along the outer edges of Mars at sunrise fall to -120° F. (Those are not grossly out of line with current measurements.)

  • 1963: Modern equipment at last detects water vapor in Mars's atmosphere. French astronomer Audouin Dollfus establishes a special-purpose telescope atop the Jungfraujoch in the Swiss Alps to search for water vapor in Mars's atmosphere, and reports success; in the same year, a three-man team (Spinrad, Münch, and Kaplan) at Mount Wilson Observatory, using its 100-inch telescope and special infrared-detection instruments, also finds water vapor. All the results, though, show virtually microscopic amounts (which is why Campbell could not detect it in his time). These results reveal a Mars dramatically drier--and with a dramatically thinner atmosphere--than had been realized till then.

And so went the second astronomical era of "exploring" the planet Mars.


True Exploration: Going There

It is not even a half a century yet since humankind entered the third era of astronomical exploration, "going there". But by now we have already sent many spacecraft toward Mars, and they have returned us a treasure-house of data, some of which have dramatically revised our older views of Mars and conditions there.

Spacecraft sent toward Mars can be of four basic kinds: a "flyby", in which the craft passes by the planet, gathering data as it goes; an "orbiter", which settles into orbit around the planet to gather data on a long-term basis; a "lander", which makes a soft touchdown on the planet's surface and gathers data from where it lies; or a "rover", which makes a soft touchdown, then moves about the surface, gathering and reporting data. Sometimes those can be combined: a mission could comprise a craft that enters orbit but also sends down a lander; or a surface mission could comprise both a fixed "base station" and a separated rover. Sometimes mission problems can convert one sort into another, as with an intended orbiter that ends up only doing a flyby. The Table below lists all Mars-bound spacecraft past, present, and--so far as is known now--planned.

At our present level of rocket capability, and for the foreseeable future, it is not possible to launch a mission to Mars at just any old time we might have the hardware ready. That is because both Mars and the Earth orbit the Sun, but not at the same speed (the farther out an orbiting object is from its "primary", the slower it moves on that orbit--that's just a law of nature). Thus, it is only every so often that their relative motions are such that they are--as planetary distances go--close to one another; one does not want to try to send a spacecraft out that would not only have to travel the distance from the Earth's orbit out to Mars's orbit, but additionally travel some great extra length to catch up with where Mars is.

Inner solar system, November 2004 Inner solar system, November 2005

That is easier to follow if you look at an orrery, a mechanical device that physically embodies the relative motions of the planets. There is a very nice online graphical orrery available at the "Solar System Live" page of John Walker's Fourmilab web site; here are two views taken from that orrery, showing (not, of course, to scale) the inner planets as they were aligned on 5 November 2004 (at left) and 5 November 2005 (at right). Notice how far Mars is from the Earth in 2004, and how close it is in 2005. The times when an astronomical target is at or near its optimum placement relative to Earth determine what are called target "launch windows"--periods of time during which it is feasible to launch a spacecraft toward that target.

Note that the launch window is not the time when the target (here, Mars) is actually closest to us--because the spacecraft takes quite some time to get to its target; thus, the launch window is the near-approach period minus the spacecraft travel time. A spacecraft is not launched toward where its target is: it's launched toward where its target will be by the time the craft gets there.

Here is the record (omitting planned missions later cancelled and thus never attempted) of all Mars-bound spacecraft:

In this Table, substantially successful missions appear on a green background,
partially successful ones on an
amber background,
and mostly or wholly unsuccessful ones on a
pale yellow background.
This scheme is a major oversimplification, but gives one a quick idea of success/failure rates.
Spacecraft
Name
Launch
Date
Mission
Goal(s)
Mission
Status
Marsnik 1 (Mars 1960A) 10 October 1960 Flyby launch failure
Marsnik 2 (Mars 1960B) 14 October 1960 Flyby launch failure
Sputnik 22 (Mars 1962A) 24 October 1962 Flyby broke up in Earth orbit
Mars 1 1 November 1962 Flyby contact lost in flight
Sputnik 24 (Mars 1962B) 4 November 1962 Flyby broke up in Earth orbit
Mariner 3 5 November 1964 Flyby died in flight
Mariner 4 28 November 1964 Flyby successful
Zond 2 30 November 1964 Flyby contact lost
Zond 3 18 July 1965 Lunar Flyby/Mars Flyby lunar flyby successful,
missed Mars
Mariner 6 25 February 1969 Flyby successful
Mariner 7 27 March 1969 Flyby successful
Mars 1969A 27 March 1969 Orbiter launch failure
Mars 1969B 2 April 1969 Orbiter launch failure
Mariner 8 8 May 1971 Flyby launch failure
Cosmos 419 10 May 1971 Orbiter lost from Earth orbit
Mars 2 19 May 1971 Orbiter/Lander orbiter successful;
lander crashed
Mars 3 28 May 1971 Orbiter/Lander orbiter mainly successful;
lander lost shortly after arrival
Mariner 9 30 May 1971 Orbiter successful
Mars 4 21 July 1973 Orbiter partial failure--
became a flyby
Mars 5 25 July 1973 Orbiter successful
Mars 6 5 August 1973 Lander contact lost at surface
Mars 7 9 August 1973 Lander unsuccessful--
became a flyby
Viking 1 20 August 1975 Orbiter/Lander successful
Viking 2 9 September 1975 Orbiter/Lander successful
Phobos 1 7 July 1988 Mars Orbiter/Phobos Lander communication lost in flight
Phobos 2 12 July 1988 Mars Orbiter/Phobos Lander communication lost in flight
Mars Observer 25 September 1992 Orbiter contact lost in flight
Mars Global Surveyor 7 November 1996 Orbiter successful
Mars 96 16 November 1996 Orbiter/Landers lost from Earth orbit
Mars Pathfinder 4 December 1996 Lander/Rover successful
Nozomi (Planet-B) 3 July 1998 Orbiter mostly unsuccessful,
but with some results
Mars Climate Orbiter 11 December 1998 Orbiter crashed on Mars
Mars Polar Lander 3 January 1999 Lander/Surface Penetrators apparently crash-landed
Mars Odyssey 7 April 2001 Orbiter successful
Mars Express 2 June 2003 Orbiter/Lander orbiter successful,
lander failed
MER-A Spirit 10 June 2003 Rover successful
MER-B Opportunity 7 July 2003 Rover successful
Rosetta 2 March 2004 Mission to a comet:
Mars Flyby in 2007
in flight:
Mars flyby expected February 2007
Mars Reconnaissance Orbiter 12 August 2005 Orbiter in flight:
expected to arrive March 2006
Future/Scheduled Missions:
Phoenix August 2007 Small Scout Lander   --
Phobos-Grunt October 2009 Mars Orbiter &
Phobos Sample Return
  --
Mars Telecommunications Orbiter November 2009 Orbiter (telecommunications)   --
Mars Science Laboratory 2009 or 2011 Rover   --
ExoMars 2011 Rover (ESA)   --
Mars 2011 2011 Scout Mission   --
Mars Sample Return Mission 2013 Joint ESA/NASA mission:
Aurora Programme
  --

Here are links to news on presently active missions:

The treasure trove of information the many missions have brought us (including the valuable experience with those that wholly or partially failed) is inestimable: scientists will be laboring for years yet just to complete analyses of the data we already have, and more pours in hourly. We will not here attempt to set forth all that data, or the conclusions being drawn from it--that we do chiefly on the pages of this site dedicated to discussing planets and the possibility of life on Mars.


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