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Presents
Volume 1419

GEOGRAPHERS OF MARS I:
MATCHING MARS AND BARSOOM
A NEW APPROACH
by 
Den Valdron
Part of the Exploring Barsoom Series

 


Thuria (Phobos)
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GEOGRAPHERS OF MARS I:
MATCHING MARS AND BARSOOM
A NEW APPROACH

CONTENTS
Introduction
Geographers of Barsoom
Previous Attempts to Map Barsoom
Matching Mars and Barsoom
The Toonolian Marshes and Valles Marinis
The Gathol Seamount and Elysium Monte
The Artolian Hills and Tharsis Montes
Throxeus and Forgotten Oceans
Torquas and Hellas
Omean and the South Polar Bulge
Other Areas On Mars and Barsoom
River Iss, Valley Dor, The Lost Sea of Korus and Argyre Basin
Was Valley Dor Really at the South Pole
Megalithic Barsoom




INTRODUCTION

 For ease of appreciating this effort, we recommend that the reader reference maps of the current Mars.   There are of course, many maps of Mars on the internet showing the planet in a variety of fascinating ways, and I highly recommend browsing through them.   I shan't violate their copyright by pirating them.  They're the work of smarter and finer people than I.  But I don't hesitate to refer you to a few...

 The first is of course the satellite photography maps developed by various space probe's cameras, which contain neatly labelled features and regions.   It can be found here:


 http://marsville.enoreo.on.ca/mission/linkup/event/marsmap.htm

 The second is the MOLA Laser Altimeter Topographic Map of Mars, which depicts Mars through a series of false colour elevations.   Lowlands are depicted through deepening shades of blue.   Intermediate elevations are shown as greens, yellows and oranges.   Highlands are depicted as reds and browns with volcanic peaks showing white.  It can be found here:


http://ltpwww.gsfc.nasa.gov/tharsis/Mars_topography_from_MOLA/ 

 Just for the record, there’s a topographic map with features identified.  But it’s not really interactive, and the level of detail isn’t all that great.  But it might stand some convenient cross referencing.


 http://ltpwww.gsfc.nasa.gov/tharsis/map_lab.html

 Ready?   Keep them handy, and let’s go.


GEOGRAPHERS OF BARSOOM

 Barsoomian Geography is a tricky thing with many pitfalls for the unwary.   Although distances between cities are often given in Martian measurements or travel time, there is a complete lack of an adequate reference point.   Exum is described as the Barsoomian Greenwich, but where is Exum?   Its location is, at best, imprecise.   Certainly Earthly cartography of Mars does not use Exum as a starting point. 

 It must also be remembered that the original narrators were translating Martian terms and concepts, and Martian geography into English.   As John Carter and others discovered to the chagrin, even tiny errors could cumulatively result in major deviations.   Accordingly, we must expect some degree of error in translating Martian measurements to Earth terms.  By the same token a reference to an equator may be taken as either a specific point, a hypothetical midline of the planet, or as a broad regional belt. 

 To render travel distances and relationships on a circular globe involves complex referential mathematics.   Current Terrestrial society uses a global system of latitude and longitude, but there are hypothetically other systems.   We do not know to what extent a Martian system matches the terrestrial system, or what degrees of errors may creep in having even educated laymen translate one system into another.


PREVIOUS ATTEMPTS TO MAP BARSOOM
Schiaparelli's Mars 1888
Schiaparelli's Mars 1888

 It is acknowledged that Edgar Rice Burroughs drew crude maps to locate his John Carter’s adventures, he was not a cartographer.  As to his geographical skills, one might look to the Tarzan books which deal with the Earthly and well mapped Africa.  Even setting aside endless lost cities, hidden valleys and inaccessible regions, Burroughs grasp of geography on Earth was occasionally loose, one must assume the same applies to Barsoom. 

 Moreover, his work constitutes entirely a second hand account.  He was not the source, rather, he related tales told by John Carter.   Accordingly, as a dedicated and prolific scribe, he may be forgiven for the occasional error.

 In the 1940's a substantially more elaborate map was drafted, intended to overlay ERB’s Barsoom over the map of Mars as it was known then.   That original Map of Mars has turned out to be highly inaccurate, and so the superimposition of Barsoomian locations must be taken as equally inaccurate.   In fact, the most compelling thing about the 1940's map is that it was an attempt, and it was clearly ERB’s intention to superimpose Barsoom onto Martian geography.

 A second attempt to superimpose Barsoomian onto Martian geography took place in 1998.   It represents an astonishing amount of work, but sadly, it lead the author to conclude that Barsoom and Mars were two different and unrelated worlds.   His map contained numerous anomalies such as placing the Toonolian marshes in the Tharsis mound, surrounded by and atop shield volcanoes - just about the most unlikely spot on the planet. 

 One major mistake of these previous maps was to assume that the central points of reference were the same.   The Barsoomian Globe has Exum as its zero reference point.  That’s pretty damned arbitrary.   The current Martian maps are not based on a fictional Exum, but start with their own arbitrary reference points.   There’s no chance of those reference points matching.

 So, the bottom line is that in attempting to match Barsoomian and Martian geography, we have to consider Burroughs maps, latitudes and longitudes and distances as merely rough guides, and not definitive points.   And we cannot make the mistake of assuming that terrestrial mapping of Mars uses the same reference points.

Cartography by Larry Ivie for Readers Guide to Barsoom and Amtor
Cartography by Larry Ivie for Readers Guide to Barsoom and Amtor


MATCHING MARS AND BARSOOM


Lowell's Mars

 In this new approach, we would instead attempt to establish reference points between the two planets geography.   Much of John Carter’s descriptions and locations refer to Barsoomian cities, which, although picturesque, are of little assistance to us.   Similarly, visits to the north and south pole are of little help.

 But along the way, Carter and the other narrators have encountered a handful of significant geological landmarks prominent enough that their counterparts should show up on Mars.    Principal among these are the Toonolian Marshes, the Artolian mountains, and Gathol.  Less significant, but also potentially relevant are the forests of Invak and Kaol.


THE TOONOLIAN MARSHES AND VALLES MARINIS

 Toonolian Marshes:  -- 1800 earth miles of marsh stretching between Phundahl on the west to Toonol on the east, narrow winding waterways connect small bodies of water, the largest of which is a few acres in area; marsh, jungle, and water, dotted by rocky islands which may be the remains of an ancient mountain range, often forested by thick jungle. The area is densely populated by "fierce beasts and terrifying reptiles, by remnants of savage aboriginal tribes long isolated."     Phundahl:    west end of the Toonolian Marshes; located near broken canyons and hills containing tracts of sompus trees to the southwest; continually at war with Toonol.

 What are the Toonolian Marshes?   They’re one of the last vestiges of wet Mars, of the ancient Martian oceans which once covered the planet.   Are they a sea bed?   Other Marshes, around Gathol, for instance, are associated with the remnants of Martian seas, but most of the ocean beds are already dry.  Only the deepest portions would still contain even a little moisture.  But the Toonolian Marshes aren’t described as being in a particularly deep lowland.  A better explanation might be that the Marshes sit upon and are fed by deep sea canyons still filled with water.  But what canyons they must be.  The Marshes are a band stretching 1800 miles, suggesting a truly titanic canyon complex.  Such a canyon complex, even dried, would remain and be one of the most spectacular features of the planet.  Is there any such feature on our Mars?

 Yes, there is.  Valles Marinis, a 3000 mile long complex of canyons up to eight miles deep, one of Mars most spectacular and prominent features.   Only the Valles Marinis canyon complex would the one of the last great harbours of the dying martian seas.   It’s immense stagnant depths and restricted surface area would prevent its water from sublimating as quickly as in the fast flowing, shallow seas.  The Toonolian marshes are nothing less than a rain forest complex in and surrounding the Valles Marinis aquifer.

 But wait:  Valles Marinis is 3000 miles long, the Toonolian marshes are only a ‘mere’ 1800 miles.  There’s 1200 miles missing.  So there are.  The Valles Marinis complex itself is in a process of dessication and the Toonolian marshes have been shrinking.   At the west end, Phundahl is located near broken canyons and in forested hills, clearly a description of the drying end of the Valles Marinis. 

 One would expect to go further west, or perhaps further east, and find other pockets of forest or greenery, in emptying sections of Valles Marinis.   And in fact, the Kaolian forest may be an elevated and partially dry seciton of Valles Marinis.


THE GATHOL SEAMOUNT AND ELYSIUM MONTE

 Next up is Gathol.  NW of Helium. Titled the oldest inhabited city of Barsoom. Gathol began as an island in Throxeus and as the ocean disappeared, the city built down the emerging seamount. Surrounded by salt marshes, Gathol has never been conquered though many have tried to take possession of the fabulous diamond mines beneath the city. 

 Now, the city of Gathol is not nearly so important as its location:   A seamount island previously located in a large Ocean.   From what we can tell, Gathol is a unique or nearly unique city on Barsoom, precisely because of its nature as a former seamount. 

 A solitary mountain is undoubtedly a shield volcano, found on Mars, but exceedingly rare.   A solitary shield volcano in a lowland area should stick out like a sore thumb. 

 Well, let’s just go back to our topographic map and look around, shall we?   And what do we find?   In the middle of the northern lowlands, the hypothetical location of one of our major Martian oceans, we have a lone shield volcano Elysium Monte, with its peak stretching some 10,000 to 16,000 meters above the surrounding landscape.  Here is our candidate for Gathol.

 And Elysium Monte is broadly the right distances and relationship to Valles Marinis as Gathol is to the Toonolian Marshes.


THE ARTOLIAN HILLS AND THARSIS MONTES

 But let’s not forget about mountains, shall we.   There is another important group of mountains around Duhor.  Snow Capped Artolian Mountains.  10,500 haads NW of Helium. 7,800 haads west of Toonolian Marshes on western side of Artolian Hills (aka Snow Clad Mountains).

 For Mars, Tectonic activity ceased early in its history.  Without tectonic plate activity, we do not get mountains.  Mountains are reported elsewhere on Mars, but I think that we can safely say they do not compare with Terrestrial mountains.  Most Martian mountains are probably little more than hills or sharp escarpments.
 Still, the Artolian mountains have a unique feature on Mars.  They are snow capped, which suggests they might be tall enough to be actual mountains.   John Carter and others refer to the Artolians as hills, suggesting that they may be relatively gentle rather than steep slopes.   Other features are referred to as mountains.   But there is no other reference to snow capped peaks anywhere else on Barsoom.

 Are there any candidates?  As a matter of fact there are.  There are a group of shield volcanoes known as Tharsis Montes on the Tharsis bulge just to the east of Olympus Mons, and west of Valles Marinis.   Reaching heights of 12,000 meters or more above the planetary median, the Tharsis Montes and Olympus Mons are bound to be snow covered and constitute four out of the five major volcanoes on the planet (the fifth is Elysium Montes).

 Once again, the relationships seem to work.  The Tharsis Montes are substantially to the west of Valles Marinis, as the Artolian Hills are to the west of the Toonolian Marshes.

 Our geography of Martian cities is in general agreement.  Duhor wars with Amhor.  Amhor’s principal economic partners are Duhor, Toonol and Phundahl.   Phundahl is in the west of the Toonolian Marshes, further west from Phundahl you come to the Artolian mountains, and just west of that is Duhor. 

 It fits into the Barsoomian geographical features that match up with Martian geography, and there is enough space in the Martian geographic features to fit the Barsoomian cities.


THROXEUS AND FORGOTTEN OCEANS

 John Carter refers to five oceans or seas on Mars, only one of which is specifically referred to, Throxeus.    Throxeus is located in the northern hemisphere, but apart from that, its dimensions and contours are uncertain.
 A look at the topographic map of Mars shows us where an immense northern ocean would have been.   But this seems to leave us a bit short.   The topographic map shows only one potential immense northern ocean in blue, and a couple of smaller blue spots in the southern hemisphere.   Three oceans or seas at best.

 But look to the northern lowlands again.  The lowlands are divided by an immense peninsula moving up from the Tharsis area and a vast seamount belt around Elysium.   So, the northern lowlands are divided into three great lobes which unite in the near polar region.

 Hence, to Martian explorers from southern or temperate regions, the great northern ocean would appear to be three great seas or oceans.


TORQUAS AND HELLAS

 In the southern hemisphere of Barsoom, there are features called the Torquas Mountains, which surround a the dry bed of a vanished body of water called the Gulf of Torquas. 

 In some usages, a Gulf refers to a round sea, far larger than a bay or lake, as in the Gulf of Mexico.

 Turning to the southern hemisphere of our topographic map of Mars we find the Hellas Planitia, an immense basin formed by a huge asteroid strike.  The basin is the deepest place on Mars, and on a wet world, would have been the site of a great sea. 

 As the site of a huge asteroid strike, the Hellas area was deformed, with high ridges or mountains, known as the Syrtis highlands, thrown up all around it.

 Thus Hellas and its jagged ring of mountains forms a fairly good match for the former Gulf of Torquas and the ringing Torquas mountains.

 Torquas, though referred to as a Gulf may well be the fourth great sea or ocean. 

 And the last of the five seas?   I’ll get to that.


OMEAN AND THE SOUTH POLAR BULGE

 Omean, the buried south polar sea might well be represented by an immense four kilometer bulge of a portion of the south polar area. 

 One can imagine a geological process wherein an ancient ice cap is covered by a layer of thousands of feet of rock and debris from a major asteroid strike, such as the south hemisphere impacts that created Hellas and Argyre basins. 

 Over time internal heat, derived from the coriolis stress of the polar axis and geological pressure causes part of the buried ice cap to melt forming a liquid, underground sea.

 Would Omean be the fifth sea referred to by Carter?   No, unfortunately.   By all evidence, it was not a part of the known ancient Barsoomian world.   The final sea still awaits us.


OTHER AREAS ON MARS AND BARSOOM

 Are there other areas which are not manmade but which represent significant geographic features? 

 There are also unnamed, but large and strikingly deep craters in roughly the correct locations for the Valley of Kamtol in the northern hemisphere and the Valley Hohr in the southern Hemisphere.   The Valley Hohr notably, is a crater, although referred to as a volcanic crater.

 There are the forests of Kaor and Invak, near the equator to account for.   Forests suggest microclimates where there is still enough water in the environment to support trees. 

 These may represent the remains of ancient isolated seas, lakes or bays, which have retained some of their moisture.  Or they may be remnants of the water stored in the canyon complexes which are part of Marinis Valles.

 Kaor appears to be relatively near the Toonolian marshes and may indeed be another temperate fragment of the Valles Marinis complex. 

 Invak is more challenging being placed substantially to the east of Gathol near Dusar.   The most likely candidate is the Amazonas Planitia, a sea bay of the polar ocean abutting the other side of the Tharsis bulge and the vast Olympus Mons shield volcano. 

 Surrounded by highlands, backed by the immense wall of Olympus Mons, the Amazonas Planitia is a natural collection point for moisture. 

 A second, less persuasive candidate is Ieidias Planitia, another bay located south and west of Gathol near the equator.   It too might be the site of the Invak forest, or another remnant ecological zone sustained by higher than average moisture.


RIVER ISS, VALLEY DOR, THE LOST SEA OF KORUS AND ARGYRE BASIN

 The most challenging zone is Otz Mountains, surrounding the golden cliffs, which contain Otz Valley and within it a section known as Valley Dor, containing Lost Sea of Korus,  all apparently nestling inside one another like a series of russian dolls. 

 The Otz valley drains the immense river Iss from the north, and holds the Valley of Lost souls between it and the South Pole.  The location is indistinct.  The area is depicted as being at the south pole, but this cannot be literally true. 

 The lost sea of Korus is, of course, the last of the five seas of ancient Barsoom, and uniquely is, apart from the Toonolian Marshes, the last major body of open water on the planet. 

  Whatever its true history, the Otz/Dor/Korus complex is home to the unique plant men, a  life form unknown elsewhere on Barsoom.   This suggest that the Otz/Dor/Korus complex may have been an extremely isolated region, an ecological ‘island’ zone largely cut off from the rest of the planet where such a bizarre creature might have evolved safely?

 Once again, we have a candidate.  Between latitude -55 and -60, and longitude -60 and  -30 in the southern hemisphere is the Argyre Planitatae.   A relatively small circular lowland, of a quarter of a million square miles.  It is bounded on the northwest by the imposing Tharsis bulge, and to the northeast by the Syrtis plateau.  Directly above towards the equator is Valles Marinis.   It is the furthest south of any major depression or lowland, even slightly to the south of the Hellas Planitatae.

 Argyre seems to be a perfect site for Otz/Dor/Korus.   One factor is its isolation, only about 1900 miles from the south pole, 2400 miles from Valles Marinis, and 2700 miles from the Hellas Planitae, it is the most isolated lowlands on the planet. 

 The network of sharp ridges surrounding it are effective candidates for the Otz mountains.   It’s location near the southeast end of the Tharsis mound further isolates it and may have formed an atmospheric barrier for water loss, enhanced by the Syrtis Plateau, and protected by the high ridges/mountains surrounding it.. 

  Above Argyre is a slender gap between the highlands, the potential site of the river Iss which would drain from the vicinity of the Toonolian Marshes down into the Korus.   A close up examination of the area literally allows us to trace the course of the Iss. 

 The Argye is slightly closer to the south pole at its lowest extremities than Hellas.  Immediately to the south, there is a separate large shallow depression or crater, a candidate for Valley of Lost Souls, which brings it even closer to the south pole.   Argyre would be the logical starting point for a canal project to attempt to drain water from the south polar cap.   And in fact, we have some evidence that this may have been done, and that there is a canal/river connection between Korus and the south polar cap through the valley of lost souls.

 The Toonolian marshes have survived because of the immense depth of the Valles Marinis.  The Argyre Planitae is a much shallower feature, shallower than the deep reaches of Hellas or the northern lowlands, but it has managed to retain its water through a combination of features, drainage from the south pole, drainage from the river Iss, and the geographical isolation beween the Tharsis bulge and syrtis highlands.


WAS VALLEY DOR REALLY AT THE SOUTH POLE?

 Of course, traditionally, the Otz Mountains, Valley Dor and Lost Sea of Korus are supposed to be located at the south pole of Barsoom.   A series of concentric bulls-eye rings surrounded by the polar ice cap.

 But come on now.   How is this even remotely possible.  What warms the Valley Dor?  Why doesn’t the Sea of Korus freeze solid?   There are other anomalies to be found.   John Carter experiences days and nights in fairly normal succession.   Well, at the absolute bottom of the planet, assuming that its standing perfectly upright with no axial tilt, you won’t get days or nights, just and endless waxing and waning twighlight. 

 And forget about photosynthesis in a place like that.   The Otz mountains would cast permanent shadows into the Valley and the sea would be eternally in darkness.   In fact, there are places like this on the moon, polar craters whose bottoms are eternally shadowed, and thus are believed to contain the moon’s only water.   Despite this, the Valley Dor is one of the lushest locations on Barsoom.

 Or we might have a wandering axial tilt, in which case, as on Earth, polar days would last six months, and the inhabitants would experience a ‘midnight sun.’   Again, that doesn’t seem to be the case.

 Another anomaly?  John Carter from the Valley Dor observes the passage of Barsoomian moons.   No way.   If these moons are at all similar in orbit to their counterparts in this Universe, there’s no way Carter could see them.

 All of which goes to suggest that the Otz/Dor/Korus complex is not located at the Martian south pole in the traditional sense, despite Burroughs writings.

 So, how do we reconcile this?   There is a solution. On Earth, we have three different sets of poles.  The magnetic poles which wander, the poles of the axis of rotation, which are inclined and provide the earth with seasons, and the poles of axis of revolution.  Perhaps we have a similar situation on Mars in John Carter’s time.   Perhaps the Barsoomian axis of rotation is permanently skewed or very slow moving (compared to earth), and that the centre of the axis of rotation is in or at the edges of the Otz/Dor/Korus complex.

 If this is the case, this might explain why Carter can still see the Moons of Barsoom, and why the complex seems central to rotation.  If the south axis is permanently inclined towards the sun  would be a normal day night cycle with plenty of light, and the possibility of a hospitable local climate.

 In short, if we accept this hypthosis for Otz/Dor/Korus, or if we merely set the whole thing aside, we’ve got an excellent set of correspondances between real Mars and John Carter’s Barsoom, and within a fifteen or twenty percent margin of error, everything seems to be where it should be in relation to each other.


MEGALITHIC BARSOOM
Cydonia FaceCraters of UtopiaCydonia Complex with artistic enhancement
 On Mars, there are a variety of sites and artifacts which folklore attributes to potentially intelligent design.   There is the Cydonia complex, with the face, tholus, fortress, city complex and D&M pyramid.  There is the Utopia complex, with the tie, another face, and a runway.  There is the Inca City complex near the south pole, with its own face.  There are pyramids in Elysium, a pyramid on the lip of a crater elsewhere, and the ‘crowned face’ formation.

 John Carter travelled across much of Barsoom, but never encountered pyramids or gigantic faces.   On the other hand, other fictional Martian travellers, notably Doctor Who encountered Pyramids.   Rocketship XM found a gigantic (but not geologic scale face) and the ruins of a domed city.

 Does the fact that John Carter and other correspondents never referred to pyramids and faces mean that they weren’t there?   Not necessarily.  Although we don’t have specific references to these features, there are plenty of references to cyclopean engineering.

 The Atmosphere Plant was a construction four miles square and 200 feet high, a match for any Cydonian structure.   We may also consider the two towers of the twin cities of helium, each a mile high.  Or the hundred mile circumference of the polar city of Okar.  Finally, there is the immense network of canals.   Nor is Barsoom short of megalomaniac egotists, the Jeddak of Jahar is an example.

 In short, the modern Martian ‘relics’ certainly would not be beyond the capacity of the ancient Barsoomians, nor beyond their sensibility. Cydonia would fit well into Barsoom.

 So, while we cannot directly link hypothetical megalithic locations on Mars to locations on Barsoom, we can at least acknowledge that Barsoom was prone to works on the megalithic scales folklore attributes to Mars.

 This concludes the first part of our tour of Mars.   We hope that our effort to match Martian geography to Barsoomian landmarks has been interesting and hopefully persuasive.

 It is, of course, all based on coincidence.   At the turn of the 20th Century, there was no chance that any human could have the detailed knowledge of Martian geography that we have now.   We have received a wealth of knowledge from almost forty years of space probes which have steadily revealed gigantic volcanoes, vast plains, fields of craters, mighty chasms and oddly evocative faces. 

 Burroughs could not have known any of this.   His own marshes and mountains, the great swamps and lost oceans, were purely the products of invention.   The maps of the time would not even support bare speculation.   He made it all up.

 Nevertheless, it is a pleasing and satisfying thing to be able to look at our neighboring planet, and to so easily and reliably find the magical images of fabled Barsoom, like ghosts upon its landscape.

 In another paper, I will take the liberty of extending this exercise to the cities and man made works of Barsoom, locating them in the Martian landscape.


Huck's Map of Barsoom from ERBzine 0246m

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