A NEW MODEL OF MARS AS A FORMER CAPTURED SATELLITE: BI-MODAL DISTRIBUTION OF KEY FEATURES DUE TO ANCIENT TIDAL STRESS?
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A NEW MODEL OF MARS AS A FORMER CAPTURED SATELLITE: BI-MODAL DISTRIBUTION OF KEY FEATURES DUE TO ANCIENT TIDAL STRESS? Richard C. Hoagland (Principal Investigator, Enterprise Mission) Michael Bara (Executive Director, Formal Action Committee on Extraterrestrial Studies). ABSTRACT Conventional models of Mars, based on measurements by initial Mariner unmanned spacecraft, found an arid, apparently ancient environment without current liquid water. This prompted sub- sequent, highly negative assessments regarding Mars’ history, and the difficulty for the origin and/or evolution of higher forms of life. Later, the unmanned Viking missions (as well as the 1997 Pathfinder Lander) seemed to confirm this barren model. Complex, sometimes contradic- tory geologic theories to explain this desolate Mars environment have been proposed, based on a wide variety of observed surface phenomena and features. A new model that reconciles major puzzling contradictions among past models is now put forth, using new observations from MGS high-resolution images of Mars and a reevaluation of certain Viking era experiments. Small- scale surface features are identified which, it is proposed, are the direct product of wide spread ancient and recent bursts of subsurface liquid water. These water “stains” are shown to cluster (beyond statistical chance) in an unmistakable tidally-determined, bi-modal distribution on the planet: centered near the Tharsis and antipodal Arabia “bulges.” A revaluation of Mars ancient history is therefore proposed, suggesting that Mars (well after solar system formation) was cap- tured into synchronous orbital lock with a larger planetary companion (“Planet V”), accounting for the clustering of present day water bursts around the former beds of two bi-modally distrib- uted “Mars ancient oceans” as a direct result. The current Tharsis and Arabia mantle uplifts are shown to be an inevitable additional fossil signature of such former tidal stresses, induced by a close gravitational relationship with Planet V. Other heretofore inexplicable Martian surface fea- tures are shown to be consistent with such a simple "tidal model": Valles Marineris (as an eroded ancient tidal bore, formed immediately post-capture); the presence of the extremely flat terrain covering the northern hemisphere (via deposited sediments from the once tidally supported oceans, when released); and the current trench or "moat" around the Tharsis bulge (from relaxa- tion of Tharsis back into the mantle, after tidal lock was broken). The long-mysterious “Line of Dichotomy” is explained as a remnant of a “blast wave” of debris from this sudden severing of the former orbital lock relationship with Planet V, due to either a catastrophic collision or explo- sion. Chemical signatures of this extraordinary destruction event on Mars are shown to be con- sistent with the model; including the distribution of olivine preferentially below the line of di- chotomy; the presence of primitive mantle and core materials such as iron and sulfur in unusual abundance on Mars surface; and the concentration of proposed “water stains” in areas bereft of olivine. Mars unusual magnetic field “striping” is now shown to be another unique southern hemisphere signature of this destruction event, caused by standing P and S waves reverberating through the planet’s crust as a result of the massive simultaneous impacts from Planet V debris. Recently published research showing unprecedented outflow channels from the Tharsis and Ara- 1
TIDAL BULGES ON MARS: R.C. Hoagland and M. H. Bara bia bulges are shown to be consistent with the sudden relaxation of the two tidal oceans, as is the sculpting of huge amounts of material by fluvial processes north of the Arabia bulge. Two pos- sible mechanisms for the destruction of Planet V and the breaking of this tidal lock are outlined. Finally, a new timeline for Mars geologic evolution is proposed that is consistent with these ob- servations, placing these events between capture ~500 MYA and the destruction of Planet V at 65 MYA. Introduction: Man’s fascination with available liquid water on the Martian surface Mars has led to many fanciful and romantic – a key prerequisite for life. This general notions about the planet’s genesis. Early dismissal of the LRE results was immediately popular (and even some scientific) specula- challenged by the LRE’s Principal Investiga- tions focused on a planet populated by exotic tor, Gilbert Levin. Levin3 showed that liquid creatures if not warring advanced civiliza- water could flow on the present day Martian tions; these were based in large part on surface, if the available water was restricted Lowell’s turn-of-the-Century model of a to the lower 1-3 km of atmosphere, rather harsh and frigid Mars, one that was still hab- than being evenly distributed throughout its itable, though dying. It was not until the depth. Meteorological data from Mars Path- 1964 Mariner 4 mission that the general pub- finder later confirmed the Levin model for lic and the scientific community got their first atmospheric water distribution.4 close-up view of the real Mars -- as Mariner 4 flew by at a distance of 6,118 miles. The 21 One remarkable development in this re- images telemetered back to JPL surprisingly gard has been the rediscovery of 25-year-old revealed a cratered terrain more akin to the “lost” NASA data from Levin’s own experi- lifeless lunar surface than anything on Earth. ment. Joseph Miller, a neurobiologist at the With these first insitu spacecraft Mars data, University of Southern California, recently hopes for finding anything approaching an- presented evidence that the radioactive C02 other “Earth” elsewhere in this solar system release that was the heart of Levin’s experi- were permanently dashed. Subsequent mis- ment exhibited a clear 24.66-hour Martian sions confirmed that the Martian atmosphere diurnal cycle – precisely the circadian rhythm was much too thin and the temperatures too to be expected of living Martian microbes in low to allow for the presence of surface liquid the soil.5 If confirmed, this would strongly water, eliminating almost any remaining hope indicate current microbial organisms on Mars of finding current life. – despite a quarter-century of disclaimers and the apparent dearth of liquid water. Eleven years later, biology experiments conducted in 1976 by the Viking Landers (in- In striking contrast to the current apparent cluding one termed the Labeled Release Ex- aridity of Mars, analysis of images from periment, or LRE), produced positive results Mariner 9 and Viking’s later Orbiters did re- for life bearing organisms in the samples.1 veal evidence of large and catastrophic an- However, these findings were directly contra- cient water flows on Mars. They also re- dicted by other instruments’ results, which vealed evidence of a violent geological past -- indicated that the biology data were “false with huge volcanoes, extensive cratering in positives,” generated by a non-biological the southern hemisphere, and a massive can- chemical reaction with the Martian soil.2 yon system (Valles Marineris) stretching al- Among the principal reasons cited for con- most one-quarter of the way around the sensus against the LRE was the absence of planet. 2
ters (on average) higher than the northern Despite evidence of wide-spread water sparsely cratered lowlands. flows on Mars, the general scientific consen- sus now is that any liquid water on the planet Somewhat limited by existing theories of has been confined to the very distant past solar system formation, planetary geologists (circa 3 plus billion years -- GYA), when a have tried to explain these major discrepan- much denser atmosphere allowed it to flow cies on Mars in terms of familiar models. freely across the surface. The presence of Since the northern hemisphere accounts for large numbers of eroded craters in the south is 50% of the land mass but only 7% of the cra- cited as proof that the planet has been geolog- ters, the latest idea is that Mars must have lost its “primordial crust” in the northern hemi- sphere to an ancient period of “vigorous con- vection and high heat flow”7 early in Martian history, at a time well after the last heavy bombardment period. However, the lack of smaller craters on the northern plains (based on relative dating of similar cratering statis- tics from the Moon) paradoxically implies a relatively recent date for this proposed “event.” An Alternative Model of Solar System Evolution -- In 1978, Naval Observatory as- Figure 1 - MOLA colorized image of Mars showing tronomer and celestial mechanics expert, the heavily cratered southern highlands (yellow and Thomas Van Flandern, put forth the idea orange) and the smooth, sparsely cratered northern (based on an original model by Olbers) that a lowlands (blue and green). relatively recent “exploded planet” in the as- teroid belt between Mars and Jupiter was re- ically dead for at least 3 billion years -- the sponsible for the origins of most comets and time since the last “heavy bombardment” of asteroids in the solar system.8 This notion, the inner solar system.6 called the Exploded Planet Hypothesis Other surface features present more diffi- (EPH)9, has found little support in the plane- cult problems for geologists. There are vast tary science community, but its lines of evi- differences in crater densities between the dence since its initial publication over twenty northern and southern planetary hemispheres. years ago have become increasingly compel- In the North, medium-sized craters are rarely ling. Part and parcel to this hypothesis is the seen, with significant distances between idea that half Mars visible surface was devas- them. This is in distinct contrast with the tated by this proposed explosion event, neatly South, where craters are so numerous that accounting for the cratering dichotomy be- they overlap each other, making it difficult to tween the northern and southern hemispheres, distinguish between individual impacts. This and the loss of a once dense and possibly life stark difference is mysteriously emphasized sustaining atmosphere. by a “Line of Dichotomy”: a separation line running around the circumference of the More recently, writer Graham Hancock planet at about a 35-degree angle to the Equa- has popularized an alternative catastrophic tor. The southern, heavily cratered side of the theory, which supports the conventional view line, is also (mysteriously) nearly 30 kilome- that the north was stripped of several layers of primordial crust.10 Hancock argues that a 3
TIDAL BULGES ON MARS: R.C. Hoagland and M. H. Bara large comet or planetoid somehow wandered • It possesses a large offset of center of into the Roche limit zone of Mars and was figure from the center of mass drawn into the planet in the Hellas basin, ef- fectively tearing away the older surface of the • The shape is not in equilibrium with northern hemisphere via secondary bom- its current spin bardment, and depositing the remnants of its • The “crustal dichotomy” boundary is shattered bulk into the southern highlands. nearly a great circle Hancock’s idea is based on Donald W. Patten and Samuel L. Windsor’s research,11 who • The northern hemisphere has a surmise that this object was in fact a “rogue smooth, 1-km[sic]-thick crust; the south- planet” they call “Astra,” described in their ern crust is over 20-km thick book “The Scars of Mars.” There are how- ever numerous problems with the “Astra” • Crustal thickness in the south de- concept – for instance, it cannot account for creases gradually toward the crustal the presence of the asteroid belt, while the dichotomy boundary EPH does so intrinsically. The authors of this paper believe that the EPH is the much • Lobate scarps occur at the boundary stronger hypothesis (if appropriately modi- divide, compressed perpendicular to fied), and that it has already demonstrated a the boundary capacity to survive serious falsification ef- • Huge volcanoes arose where uplift forts, qualities not shared by “Astra.” pressure from mass redistribution is maximal Extension of the EPH – Recently, Van Flandern has extended the EPH to include the • A sudden geographic pole shift of or- notion that several “planets” (Pluto, Mercury, der 90° occurred and Mars) are actually former moons of cur- rent or destroyed planets. Evidence to sup- • Much of the original atmosphere has port this hypothesis is extensive, but for our been lost purposes we will focus exclusively on the • A sudden, massive flood with no ob- evidence for Mars. Of these lines of evi- vious source occurred dence, we will address here only a few as relevant to our proposal. A more complete • Xe129, a product of nuclear fission, has analysis will be left to a follow–on paper. an excess abundance on Mars Some of the evidence, as compiled by Van Flandern: Previous to this, Dorman & Woolfson (1977), writing in the Philosophical Transac- • Mars is much less massive than any tions of the Royal Society of London, re- planet not itself suspected of being a sented a model called “the Capture Theory of former moon Planetary Formation.” They proposed that Mars was once an original (not captured) • The orbit of Mars is more elliptical moon of one of two colliding “protoplanets” than any other major planet (Pluto in the early accretion solar system phase.12 notwithstanding) They even provided one specific piece of evi- • Its spin is slower than larger planets, dence to support their idea that Mars began as except where a massive moon has in- such a satellite: Mars density is much closer tervened to that of some of the Galilean satellites than it is to Venus, the least dense inner planet. This implies a genesis more in common with 4
Io, Europa and Earth’s Moon than with the similar to what we are proposing led to Mars terrestrial planets. initial capture as a satellite, and then the de- struction of its “foster parent,” Planet V. To quote Woolfson (1984): “As part of the [Capture Theory] scenario, it has been The relevance of water – If Mars, prior to suggested that Mars was originally a satellite its capture (in our model) formerly had a of one of the colliding planets. The densities denser atmosphere that provided for liquid of the terrestrial bodies and some larger satel- water on the surface, it is likely that this water lites are shown in support of this suggestion – dependent on the amount -- was distributed (Figure 2). Connell & Woolfson (1983) have in lakes or oceans, much as it is here on ascribed the hemispherical asymmetry of Earth. If this was the case, there should still Mars, like that of the Moon, to abrasion by be pockets of this water trapped beneath those high-speed ejecta from the planetary collision former lake or ocean beds, relatively close to of that face of the satellite turned toward its the surface, dependent on how long ago the primary. This will give rise to a thinning of water actually flowed. If extensive “fields” the crust and for Mars such features as the of this frozen or (sometimes) liquid water centre-of-mass centre of figure offset are well were discovered near the surface, this would explained by this. If Mars as a satellite was strongly imply such former “lakes” or in synchronous rotation about its primary then “oceans” were the source. this mechanism would suggest that its spin axis should be contained in the plane of Besides Levin’s atmospheric model, the asymmetry, but it is actually 55 degrees [the best evidence for current liquid water near the 35 degree line of dichotomy, minus 90 de- surface of Mars (until recently) was provided grees] to that plane [emphasis added].” by Dr. Leonard Martin of the Lowell Obser- vatory. Martin, in 1980, compared two im- Van Flandern’s EPH Model proposes that ages of Mars taken from the Viking Orbiters there were formerly two massive planetary that clearly showed an erupting water spout.13 bodies in the current orbits of Mars and the This implied active geothermal heating of a Asteroid Belt, respectively. Both exploded. source of water not too far below the current The first (Planet K) detonated in the orbit of Martian surface. the current Belt “several hundred million years ago.” The second (Planet V) exploded In June 2000, Michael Malin and Ken near the present day orbit of Mars, some 65 Edgett of MSSS published a paper in Sci- million years ago (MYA). In Van Flandern’s ence14, proposing that grooved features on theory, additional impact damage was done to cliffs and gullies on Mars were fossil evi- Mars when a much smaller second former dence of prior erosive runoff from liquid wa- moon of Planet V exploded in Mars vicinity ter. They placed the events as recently as 1 3.2 MYA. In our modification of the EPH, MYA, but conceded the bursts could also in- we will show that it is not necessary to invoke clude present day occurrences. a literal planetary “explosion” to produce all the subsequent effects Van Flandern has pro- posed, including the formation of asteroids and comets, and the escape of most of the re- maining mass from solar influence. In doing so, we will draw upon new data not available when Van Flandern originally formulated his EPH ideas, specifically, observations of cer- tain Extra Solar planets that follow orbits 5
TIDAL BULGES ON MARS: R.C. Hoagland and M. H. Bara cally map the locations of these “seep” im- ages relative to Mars surface coordinates, to see if there was a global pattern to their dis- tribution. As a control, they also mapped randomly-selected “non-stain” images until a representative and statistically valid sampling had been completed. Immediately, two striking global patterns emerged: both pointing to present day liquid water as a source of the “stains” or “seep- ages.” In the first pattern, the map showed Figure 3 – Proposed fossilized water runoff channels. that seepage images seem to appear preferen- (MSSS/NASA) tially near equatorial latitudes, mostly be- tween 30 degrees North and South; none were In 1998, one of a growing number of “in- found above 40 degrees North and South. dependent researchers,” Byran Butcher, no- This implies that the phenomenon is restricted ticed and published on the Internet a curious to warmer areas of Mars, which would be ex- “dark area.” He casually suggested it might pected if these were truly water flows. An be “a coffee stain, water, or a shadow.”15 In equatorial pattern is also inconsistent with the July 2000, the authors published a much more “dust avalanche” model put forth by Malin specific model, based on an MOC image of and NASA as an explanation for these fea- an unusually dark, highly elongated “stain” tures.18 emanating from an exterior point source on a crater wall, proposing that it was a current The second, more important pattern dis- water flow consistent with the model Malin covered was that the water flows seemed to and Edgett had put forth a few days earlier.16 cluster preferentially around two pronounced They quickly found numerous additional ex- geological features on the Martian surface: amples. the Tharsis and Arabia mantle uplifts (“bulges” -- Figure 5). The theoretical factors behind this second (and very pronounced) bi- modal “stain” distribution pattern are the pri- mary subjects of this paper. Mars as a Tidal Locked Moon of a Companion Body – The authors are propos- ing in this paper that Mars, at some point ear- lier in solar system history, was captured by one of two larger planetary bodies orbiting near the present day orbit of Mars. This sce- Figure 4 – Proposed point source liquid water burst nario is an extension of the Capture Theory image from MO4-00072 (MSSS/NASA) model of solar system formation put forth by Subsequent to this, Palermo, England and Dorman & Woolfson (1977), as well as Van Moore also found that surface “stains” were Flandern’s Exploded Planet Hypothesis inconsistent with aeolian features, mass wast- (1978). It is also based on current observa- ing or other non-fluvial processes.17 At the tions of significantly elliptical orbits for many suggestion of one of the authors (Hoagland), newly-discovered Extra Solar planets around Palermo et-al then proceeded to systemati- nearby stars, as reported by Butler, et-al.19 6
One relevant example is the Jupiter-massed Jupiter and Mars, they would have incorpo- planet orbiting the nearby K-type star, Epsi- rated significantly more water than did Earth. lon Eridani. With an orbital period of 6.9 And, given the increased likelihood of multi- years, an orbital eccentricity of 0.6, and an ple glancing collisions in the early planetesi- average distance from its star of 3.4 astro- mal phase for this region of the solar sys- nomical units (AU), this planet’s orbit would tem,22 they probably possessed multiple natu- take it as far out as Jupiter and as close as ral satellites as well. An encounter of Mars Mars if it orbited in our own solar system.20 with such a system, billions of years after its formation (as we are proposing), would thus It is our proposal that two previous planets have a reasonable probability of encountering in the vast “gap” between the current orbits of a satellite as well. This type of encounter has Jupiter and Mars, with orbital eccentricities a much higher probability of happening than far less than the Epsilon Eridani planet, after the previous scenario presented (the three- several billion years were gradually perturbed body interaction of Planet K, Planet V, and into a series of close encounters. This even- Mars). But, this second type of encounter tually resulted in the low-probability but pos- could also result in Mars being captured by sible “three-body capture” of a third object, Planet V – via the ejection of one of Planet the formerly freely orbiting Mars, and mil- V’s own moons. Calculations examining lions of years later, the actual collision of the similar scenarios have been performed in two larger planets. As noted, such theoretical connection with the anomalous Neptune sys- former solar system members have been re- tem – which consists now of a major planet- ferred to as “Planet K” and “Planet V” in Van sized satellite (Triton) in retrograde orbit, and Flandern’s original EPH model, the latter es- a smaller moon (Nereid) in a highly elliptical timated to possess approximately 4-5 Earth one. This has been viewed for years as masses. prima-facie evidence for a highly unusual Neptune encounter earlier in solar system his- We propose that, like theoretical models tory with an outside object in heliocentric or- invoked now to explain some Extra Solar bit, which reversed Triton’s orbit and ejected System observations of formerly interacting a previous moon from the system entirely. planets,21 a rare multi-planet encounter oc- That “escaped satellite” is now known as curred late in solar system history between “Pluto.”23 two planets formerly occupying the current gap between Jupiter and Mars: two massive Regardless of the precise methodology of terrestrial planets termed “K” and “V.” As a capture, the subsequent, strong tidal relation- result, Mars was robbed of a critical portion ship between Mars and the more massive of its solar angular momentum, allowing cap- Planet V (Figure 6) would have resulted in a ture in an extreme elliptical orbit as a new further, rapid loss of Mars spin angular mo- satellite of Planet V. mentum, from a “free” rotation period in solar orbit on the order of ~12 hours down to the An alternative scenario involves only one presently observed ~24. This estimate is former solar system member – Planet V. based on models of Earth’s primordial rota- tion slowed by early lunar tides ( Figure 7). 24 Given the parameters of existing solar sys- In the model, inevitable tidal evolution not tem members -- distance, density, and mass, only ultimately circularized Mars orbit especially Mars’ low density compared to the around Planet V, it resulted in Mars finally other terrestrial planets (Figure 2) -- it seems rotating/revolving around Planet V synchro- reasonable to assume that if two additional nously, in approximately 24 hours -- with one Earth-massed planets had formed between 7
TIDAL BULGES ON MARS: R.C. Hoagland and M. H. Bara side always facing Planet V, as Earth’s Moon clined about 55 degrees to that rotational axis does today. -- instead of being focused on the Tharsis re- gion itself (see details, below). It is the authors’ central proposal in this paper that it was this verifiable “Mars tidal Original capture model and conse- lock relationship” with Planet V that accounts quences – After capture, as this close orbital for a host of previously inexplicable and even relationship between Mars and Planet V contradictory Martian surface features, that evolved and the orbit circularized over hun- otherwise will remain perpetually mysterious. dreds of thousands or even millions of years, any surface water of oceanic volume would This begins with the otherwise baffling have “sloshed” back and forth across the sur- present-day Tharsis and Arabia antipodal up- face of Mars twice every Martian “day,” just lifts on the planet, which are located precisely as lunar tides do here on Earth. We assert, 180 degrees opposite (Figures 8 and 9). In based on this intrinsic tidal process, that Mars this tidal model, the Tharsis “bulge” -- a huge at the time of capture had to have been a upwelling in the mantle and crust of Mars, “warm, wet world” with both a denser atmos- unique in the solar system – is explained as a phere and a copious supply of flowing liquid combination of the extended gravitational water, otherwise it would not evidence the tidal influence of the larger Planet V acting major surface signatures of tidal movement for a significant period of time on that hemi- we will demonstrate. sphere, in concert with pre-existing internal mantle upwellings. As would be expected But first: as an intrinsic aspect of this from such a tidal situation, a smaller but still model, we begin by proposing that the puz- significant “anti-bulge” would inevitably be zling “mantle uplift” of Tharsis began long raised at the antipodal location to Tharsis -- before this dynamic capture sequence culmi- which accounts for the Arabia uplift precisely nated. Once Mars was captured and oriented 180 degrees around the planet. with the pre-capture “heavy side” (Tharsis) pointed “down” (toward Planet V), the uplift All formerly fluid or partially fluid bodies process was then further and extensively in the solar system, including the inner moons augmented by the “stretching” gravitational of Jupiter and Saturn, show signs of such tidal forces of Planet V close by. Further, we sug- evolution (Figure 10). Io, in particular, has gest that this process resulted in the relatively significant bi-modal tidal bulges, similar to brittle crust of Mars weakening at the eastern the model we are proposing now for Mars.25 base of the now stretched Tharsis rise, result- We additionally postulate that other hereto- ing in a series of radial fissures opening up – fore inexplicable geologic features, such as one of which was then radically enlarged to Valles Marineris and the Elysium Mons, were become the Valles Marineris canyon system. also an extended result of this former tidal mechanism. The authors also propose that, In the model, this original tension crack when this tidal lock relationship was severed was inevitably expanded by the erosive ef- -- by the events directly leading to the de- fects of a massive volume of directed tidal struction of Planet V -- Mars rotational polar waters – termed a “tidal bore”26 (Figure 11) -- axis obliquity, relative to the plane of its sat- rushing back and forth (at several hundred ellite orbit, dramatically shifted. This sudden kilometers per hour!) the entire ~ 1600 kilo- obliquity shift, as part of this rapidly timed meter plus length of the original fissure, twice sequence of events, is responsible in the each Martian day, in direct response to the model for the apparent discrepancy of the original spin rate of Mars and the massive “Line of Dichotomy” blast wave being in- gravitational tides caused by Planet V. Be- 8
fore Mars’ tidal lock with the larger planet was achieved, this enormous surge would This assumes that Mars, like the other have flowed, always westward, around the planets of the solar system, prior to its capture circumference of Mars in the direction oppo- had a prograde spin. Thus, the tides induced site Mars spin, until it piled up against the by Planet V forced the rising and falling wa- immobile eastern side of the pre-capture ters to always assault the eastern side of Tharsis bulge. At that point, when “high Tharsis – which is precisely where Valles tide” passed, the released waters would have Marineris formed. rushed (under Mars gravity) back down the canyon system toward the east, scouring the The newly-found bi-modal clustering of floor once more, until the next “high tide.” “stains” (current water flows) exclusively in This almost unimaginable force of rushing the Tharsis and Arabia regions of the planet water, through an expanding canyon system by Palermo (2001), 180 degrees apart, is an of parallel fissures eventually opened up by additional major indicator that this model is the fluvial erosion, would have recurred twice correct. This accounts not only for tidal bi- each Martian “day,” possibly for several mil- modal crustal deformation of the planet, as lion years -- until Mars’ rotation was finally predicted by the satellite model, but also im- stationary relative to Planet V. plies that major quantities of unevenly dis- tributed fluid (water) once also existed on the surface. Presumably, this water primarily re- sided after “tidal lock” in two opposing “tidal ocean bulges” – with possible dry land be- tween -- because of the inevitable bi-lobed tidal forces experienced by Mars as an ulti- mately synchronously rotating satellite of Planet V. Long Term Stasis – The evidence argues that, once Mars lost its remaining spin mo- mentum and established this stable synchro- nous orbital relationship, this was not broken or adjusted significantly until the catastrophic destruction of Planet V. The constant tidal tugging on the two opposing hemispheres of Mars from this synchronous orientation now Figure 12 – Valles Marineris, a heretofore inexplicable resulted in a continual uplift of the Tharsis trough extending one quarter of the circumference of region, and to a lesser extent Arabia, antipo- Mars, is the largest canyon in the Solar System. The authors submit that this a fluvial trench generated by dal to the Tharsis rise. The formerly racing tidal bore action during Mars’ “captured satellite” tides would also then have stabilized, and the phase. tidal erosion of Valles Marineris would have totally subsided. At this point, the only addi- It is our proposal that this “scrubbing ac- tional fluvial erosion processes likely on the tion” eventually resulted in a radical deepen- planet would have been wind-induced wave ing of the original narrow cleft to form the action and severe storms. Evidence of the present day ~7-km-deep, ~4000-km-long former should still present itself on some key canyon system known as “Valles Marineris” surface features not altered by the subsequent – a system (Figure 12) now stretching one Planet V destruction. quarter of the way around the planet Mars. 9
TIDAL BULGES ON MARS: R.C. Hoagland and M. H. Bara to similarly vertical, wind/wave action fea- tures on Earth. Ironically, this idea was first proposed in a somewhat modified form in 1973, by University of Pennsylvania geolo- gist, the late Henry Faul. Titled romantically “The Cliff of Nix Olympica” (the pre-Viking name for Olympus Mons), the paper was never accepted for publication “because of the paucity of data.”28 The Viking and MGS missions have now remedied that situation, and we hope that Henry Faul’s remarkable idea is finally given its appropriate hearing. Figure 13 – Artists conception of Mars as it might have The “White Cliffs of Dover” (Figure 15) appeared during its “Garden of Eden” period, after are a prime terrestrial example of such fea- capture by Planet V. tures. These lime-rock vertical cliffs are cre- ated by the action of the waters of the English One potential candidate for such erosive Channel. High winds in the Channel create a signatures is Olympus Mons itself. Olympus constant bashing action on the shore rocks, Mons rises some 24 kilometers high and eventually beating the rocks to a vertical face. measures 550 km in diameter, making it the Similar features are seen across the Channel largest shield volcano in the solar system. on the coast of France. According to our model, a significant portion of this volcano most likely stood above the water-line of this ancient “Tharsis Ocean,” and should still display signs of aeolian wave action. Figure 15 – The White Cliffs of Dover, a vertical, ae- olian wave action feature on Earth. Figure 14 – Olympus Mons 3D perspective image showing prominent vertical scarp at the base of the lower flanks (NASA). Further evidence that the Olympus Mons scarp feature is due to the wind-driven action Remarkably, Olympus Mons is almost of an ocean can be found in the fact that it completely encircled by a very steep, nearly envelops the entire mountain (Figure 16); if a vertical escarpment. This scarp ranges from hypothetical ocean surrounded such a rising between 2-10 km high,27 indicating that it was tectonic feature, the wind/ocean patterns carved out over time as the volcano was would be expected to erode a mostly uniform pulled/pushed upward by the continuing tidal scarp such as the one we see. force of Planet V aiding internal planetary uplift. The vertical walls of the scarp suggest that it was created by this proposed aeolian wave action, as it bears a strong resemblance 10
Stain Distribution - A major, long-term consequence of this eventual Mars synchro- nous rotation around Planet V is the present bi-modal distribution of subsurface water stains. The tidal forces from Planet V would have pushed water into sub-crustal fissures and cavities at right angles to the exerted tidal stress between Mars and Planet V (Figure 18). Over time, this would have driven addi- tional Martian water in between the two “tidal oceans” deep underground and toward one of the two “water poles” at either end of the line Figure 16 – Overhead view of Olympus Mons from Mars connecting Mars with Planet V. Global Surveyor. Prominent vertical scarp nearly encircles the base (NASA/MSSS). This important theoretical detail is neatly confirmed by the crucial observation that the It is also likely the scarp was formed after stain flow images are clustered only in the Mars assumed synchronous tidal lock around Tharsis region and Arabia, exactly 180 de- Planet V, since it does not appear to be a re- grees opposite. Any water apparently resid- sult of directional tidal forces. If the scarp ing in between these two locations seems to was tidal, it is likely the cliffs on its circum- have been driven underground by the pro- ference would be significantly more pro- posed tidal stresses on the planet. So deep, in nounced on the eastern side. Intriguingly, fact, that it is now unable to leave any surface Arthur Clarke several years ago created a indications between these two former tidal computer-generated image (Figure 17) depict- “poles.” ing precisely such an “Olympus Ocean.” Al- though projected to a time when humans have Another observation consistent with the terraformed the planet Mars, his depiction – idea that the stains reflect current water reser- especially the waters swirling around the voirs just below the surface, relates to the 22,000 foot-high cliff around the mountain – “line of dichotomy” itself. Stains observed are eerily accurate to our own model of a on Tharsis seem only to occur north of this former “tidal Mars.”29 line of demarcation. This implies that the smoother hemisphere to the north is the older geologically, as on Tharsis it possesses the majority of the subsurface water/surface stains now remaining from one of the two tidally separated oceans. If the material mak- ing up the more heavily cratered southern hemisphere is due to superimposed material on the smoother, more eroded original crust (Figure 19), then we would likely not now find much water near the surface in those re- gions – even under the former Tharsis tidal Figure 17 – Arthur C. Clarke’s projection of an “Olympus ocean. Ocean” lapping at the 22,000 foot-high-cliffs surround Olympus Mons 11
TIDAL BULGES ON MARS: R.C. Hoagland and M. H. Bara timescales. Volcanoes, ice, and glaciers can all erode features,” he said. “But on this large of a scale these are unlikely explanations.” Their puzzling observations are neatly ex- plained by the sudden collapse of a former “tidal ocean” previously maintained by Planet V. When Planet V “exploded,” a massive wall of water would have been released in a few hours, rushing northward – taking a good deal of Arabia Terra with it in the process – exactly as Hynek and Phillips now conclude. Figure 19 – MOLA generated 3D topography strip This, of course, also explains the current sur- showing the dramatic difference in crustal elevation face presence of stain images in this region – between the heavily cratered southern highlands and the smoother northern lowlands. Possible water stain they are the exhumed underground remains of images appear only above the crustal “line of dichot- the subsurface waters from this former “Ara- omy.” bia Ocean.” The exception to this pattern would appear The Destruction of Planet V – We have to be the location of the opposite “tidal freely used the phrase in this paper “when ocean” – the Arabia Terra plateau, which is Planet V exploded” to describe the eventual heavily cratered as if from the Planet V event, disappearance of Planet V and the release of but possesses the second highest number of Mars back into a heliocentric (solar) orbit. current water stain images (see Figure 5). Re- cent scans from MOLA have shown that the In Van Flandern’s original model, Planet crust is significantly thinner in Arabia than it K and Planet V disintegrated via literal explo- is in most of the cratered southern hemi- sions, leaving only a residue of smaller frag- sphere,30 accounting for the presence of rela- ments (the asteroids and comets); most of the tively shallow water seepages beneath this material from these (and previous) planetary former ocean. Additionally, researchers explosions, according to Van Flandern, was Brian Hynek and Roger Phillips from Wash- completely ejected from the system by the ington University in St. Louis, interpreting highly energetic nature of the events them- this new altimeter evidence from Mars Ob- selves or subsequent encounters with Jupiter. server, conclude that an enormous amount of In terms of the actual mechanism, some pre- surface material was somehow excavated viously unknown “physics process” Van from the planet's western Arabia Terra re- Flandern has argued, is responsible for de- gion.31 stroying single planets well after their forma- tion. This insistence on a heretofore unmod- “We argue that this entire region has been eled, “mysterious energy release” mechanism massively eroded," said Hynek. "The region has played a major role in Van Flandern’s used to look like the rest of the [southern] less than enthusiastic reception by the plane- highlands, but a vertical kilometer of material tary science community, in spite of the many — enough to fill the Gulf of Mexico — has other recent confirmations of his model. been relocated downslope and spread out into Since the evidence Van Flandern has mar- the northern plains." According to Hynek, shaled for the after effects of this Event is far the most likely erosional force of this magni- more important here than the precise destruc- tude is flowing water. “Lots of things can tion mechanism he’s proposed, we believe a erode planets. Wind is very effective on long shift of emphasis could retain the best fea- 12
tures in this instance, while avoiding the non- Earth's climate corresponding to natural fluc- testable aspects of Van Flandern’s original tuations in its orbit. To probe this cycle’s in- EPH model fluence on Earth's climate over the past 100 million years, Runnegar’s team constructed It is our opinion that the eventual destruc- computer models based on known variations tion of Planet V was occasioned by a simple in planetary orbits, their proximity to the Sun and direct (if not long overdue) collision with and their interactive perturbations. In running the other proposed major planetary object in the models, they found that the known fluc- Van Flandern’s celestial mechanics’ recon- tuations of the solar system's dynamics re- struction: “Planet K.” Post Apollo models for mained constant going back to 65 million the origin of the Moon have embraced a simi- years ago. Then, to their surprise, the fre- lar concept. As the three leading pre-lunar quency of perturbations to the orbits of the landing theories for lunar origin were tested inner planets suddenly changed.33 on the returning Apollo samples and found to not fit the evidence, a radical new theory was “If the orbits of Mercury, Earth and Mars proposed. In 1975, Drs. William K. Hart- were being shaken up at this time, maybe as- mann and Donald R. Davis, writing in teroids were being shaken up too,” says Run- ICARUS, suggested that the Moon was negard. formed as a side effect of a catastrophic “glancing collision” of the Earth with another Or, maybe they were being formed – in a major planetary object. Their idea was that gargantuan collision. “a Mars-sized planetisimal” collided with the early Earth, spalling off enough lightweight Aspects of this model echo another source crustal material to recondense to form the of surprising information about the solar sys- Moon. In 1984, the first planetary conference tem: cuneiform records from the earliest to specifically consider all aspects of this “high” civilization, the Sumerian. Zecharia revolutionary theory was convened, titled Sitchin has written extensively about the “Origin of the Moon.”32 It is our proposal that Sumerian’s uncanny “knowledge” of possible a similar event, simply delayed by a quirk of collisional events from this earliest period of celestial mechanics until very late in solar solar system history.34 With the latest dis- system history, precipitated the destruction of coveries of radically different extra solar two planets in the current Asteroid Belt planetary systems and current theoretical ef- ~65MYA. This event, we suggest, thus liber- forts to understand these systems in terms of ated Mars from its temporary synchronous potentially interacting planetary orbits, the orbit of Planet V to once again pursue a soli- relevance of Sitchin’s Sumerian translations tary – if significantly more elliptical than any should take on new meaning. other inner planet -- solar orbit. In our Mars tidal model, the result of such Remarkably, at a June, 2001 Earth Sys- an unimaginable collision of two massive tems Processes Global Meeting in Edinburgh, planetary objects (remember, at least 4-5 Scotland, astrobiologist Bruce Runnegar of Earth masses each) would be almost indistin- the University of California in Los Angeles guishable from a literal planetary explosion. presented some striking independent evidence The effects of the collisional destruction of that “something” major happened in the solar Planet V and K on a nearby captured Mars, system ~65 million years ago. Runnegar and orbiting less than 100,000 kilometers away, his colleagues had previously identified evi- would have been almost inconceivable. In dence of a 400,000-year cycle in ancient addition to the discovery of suddenly “shaky ocean sediments, indicating changes in planetary orbits” at ~65 MYA, such an Event 13
TIDAL BULGES ON MARS: R.C. Hoagland and M. H. Bara should have left a number of predictable sur- almost 90 degrees to the current orientation. face features on Mars itself – other unmistak- Such a situation is termed “polar wander,” able signatures of vast destruction. and involves the long-term mechanical re- alignment of a planet’s spin axis (relative to Signatures of a Catastrophe -- Assuming surface features) after a new mass distribution that only the top 1% of Planet V and K’s is imposed – either internally (long-term con- lithospheres survived this disruptive Event -- vective flow) or externally (material accreted as accelerated chunks of various- sized crustal from major impacts).35 This “wander” con- debris moving outward from the site of the tinues until a new rotational equilibrium is collision -- large amounts of much smaller established under the influence of the new materials from the exposed high temperature mass distribution, with a new resulting pole mantles and cores of the respective planets position. would have been ejected at high speed di- rectly towards Mars in this Event. In looking The nature of this “new mass redistribu- for resulting evidence of their impacts on tion,” which subsequently forced Mars to as- Mars, we should expect to see signatures of sume its current pole position, was assumed rapid surface heating and then freezing; catas- in this case to be the sudden addition of sig- trophic water and associated mudflows; a ma- nificant crustal mass from the disintegrating jor loss of atmosphere along with huge quan- Planet V. If Mars’ “pre-explosion” spin axis tities of water; and finally – hemispherical had been perpendicular to this incoming wave cratering on Mars from a vast amount of blast of blast debris, so this theory proposed, the debris from Planet V. momentum of the impacts coupled with the unbalanced additional mass piled on the Mars shows all these signatures and more. planet’s “side,” would have initiated a “polar wander scenario” – until Mars “toppled over” The strongest direct evidence of a debris- to reach its current position of new rotational filled “explosion Event” occurring close to equilibrium, relative to its current surface fea- Mars, is the mysterious “line of dichotomy” tures. separating the northern and southern hemi- spheres at that angle of 35 degrees. Logi- Our tidal model, and the evidence support- cally, if Mars was in synchronous orbital lock ing it presented here, emphatically forbids with Planet V when the “explosion” came, such an “easy” dynamical solution to this ma- then evidence of a wave of impacts from the jor problem. The alignment of Mars prior to destruction of the Planet should be plastered Planet V’s destruction is now firmly deter- all over Mars’ one “side,” at right angles to mined: it must have been with the Thar- the incoming debris. It is not. Instead, the sis/Arabia line aimed directly toward Planet line of dichotomy is aligned (~60 degrees) to V (Figure 6). The spin poles would then have the current Mars spin axis. And the authors been at right angles to this immovable align- acknowledge that this presents some serious ment. So, the debris from the “explosion” problems for this entire model. should have smashed into the planet at right angles to the current Mars Equator – which Without the narrow orientation constraints the line of dichotomy shows it clearly did not. now imposed by the Mars tidal model pre- sented in this paper, some previous workers It has been argued that some major debris have attempted to explain away this serious – huge ejected “pieces” of Planet V’s disinte- geometric discrepancy by proposing a com- grating crust -- reached Mars first. That these pletely different pole position for the “pre- planet-busting impacts, which left the major explosion” Mars: an original rotational axis scars known as the “Argyre” and “Hellas” 14
basins, literally “rolled Mars over on its side” planet. Shortly after that, the largest, conti- before the blast wave of smaller (but more nent-sized fragment -- which created the 2300 numerous) debris arrived. This however, is kilometer wide, 5 kilometer deep Hellas ba- not at all likely. The smaller pieces would sin, the largest on the planet Mars – impacted have been accelerated fastest, and would have south of Arabia Terra (Figure 21).36 arrived first … followed by the largest pieces last. Simple Newton’s Laws: F = MA. So, what is our solution? We propose that as it was approaching Planet V toward its ultimate collision, Planet K passed close by Mars in its orbit around Planet V (Figure 20). This close encounter gravitationally interfered with the tidal lock between Mars with Planet V. In fact, it began a radical, gravitationally induced reorienta- Figure 21 – Hellas’ 2300 km impact basin tion of the entire Mars’ spin axis relative to Planet V. This was NOT internal “polar wan- Approximately 12 hours since the collision der” relative to surface features, but an entire of Planet’s K and V had now elapsed. change of the obliquity of Mars (spin axis tilt) relative to Planet V. The effects on Mars of such an unimagin- able collision/explosion “right next door” After initiating this first major change in would not be limited to massive, visible im- Mars’ orientation in perhaps several hundred pacts on the surface. The effects of countless million years, Planet K continued inward to- megatons of smaller, accelerated mantle and ward it’s catastrophic rendezvous with Planet core material from Planet’s K and V, entering V. This impact initiated an almost inconceiv- the Martian atmosphere at hypersonic speeds, able release of energy – the equivalent of Van would literally superheat that atmosphere and Flandern’s EPH explosion – and the shattered then blow a major fraction of it into space. fragments of the crust of both worlds, accel- Any surface waters would literally boil from erated by the enormous blast, began their the shockwaves and radiant heating of incom- spherical, outward journey through the solar ing high-velocity debris, and a major fraction system. Some of them, a tiny fraction of the of that water would then join the atmosphere total mass of both exploding planets, in the in its escape. With the immediate loss of a space of a few hours eventually reached significant percentage of the atmosphere, Mars. But, by the time the first major wave temperatures on the surface would plummet, of fragments had arrived, Mars had tipped resulting in any remaining liquid water over by some ~60 degrees, presenting almost quickly freezing. Shallow underground res- the entire southern hemisphere to the “explo- ervoirs would remain liquid for a longer in- sion.” That’s why the “line of dichotomy” is terval, before also becoming ice. tilted by that ~60 degrees, relative to Mars spin axis. In fact, as Mars continued to heel It is a “snapshot” of these bi-modal, for- over and larger, slower fragments continued merly flash frozen water concentrations at the to arrive, this was when the material which moment of catastrophe – the locations of the partially covered Arabia Terra reached the two former Martian tidal oceans -- that the 15
TIDAL BULGES ON MARS: R.C. Hoagland and M. H. Bara current “stain images” now seem to be con- For Mars presents us with a greater para- firming. dox than sulfur. We must ask a far more ba- sic question: why is it so red? Mars redness, Chemical Signatures of a Collision we now know from TES data,39 results from Event - Several current geochemical puzzles the extensive drifts of iron oxide strewn regarding Mars are solved with the introduc- across the surface. A fundamental question tion of this “Martian satellite model.” When then becomes: if the original iron source was Viking carried out the first insitu surface metallic iron, from the exploding/colliding composition measurements in 1976, one of planets’ cores, where did the free oxygen the puzzling results was an unusually high come from to eventually oxidize that iron percentage of sulfur in the soil. Compared to down on Mars? Even primordial free oxygen, an average surface abundance on Earth of capable of oxidizing iron in geological strata 0.07%, Viking reported a Mars sulfur abun- termed “banded-iron formations” and “red dance of over 3% -- 43 times more. Simi- beds” on Earth, it is agreed, derived from one larly, iron on the surface of the Earth is 3.8%, main source: growing biological activity.40 while on the surface of Mars it measures over 15%.37 In the iron-rich, rusted sands of Mars, are we seeing striking evidence of similar bio- Models for planetary formation generally logical activity? Did the “rain of iron” falling agree that iron and a host of other “heavy from the sky from the destruction of Planet V elements” sink to the centers of newly form- encounter an atmosphere containing copious ing worlds to form high-temperature cores.38 free oxygen – bringing to a tragic end a bio- Another generally agreed upon core constitu- logical “Garden of Eden” era for the captured ent, present to approximately 10%, is sulfur – Mars? as FeS. In the awesome collision of two such massive planetary bodies, it is inevitable that Mars Global Surveyor surface composition copious amounts of these high-temperature data indicates another major surface anomaly materials would be ejected directly into on Mars that supports this tidal model. Using space. It is our proposal in this paper that not the information from TES, Robert N. Clarke only did this occur, but that Mars swept up and Todd M. Hoefen, of the U.S. Geological precisely these abundant core materials; Survey, have reported the identification of which is why they now exhibit such unusual widespread abundances of olivine [(Mg, Fe)2 and misleading abundances in the surface SiO4] on the Martian surface (Figure 22).41 materials mantling the planet. As olivine (an iron-magnesium silicate) quickly weathers into other minerals in the Recent Surveyor composition data from presence of liquid water, its surprising abun- the Thermal Emission Spectrometer (TES) dance according to all conventional Mars has revealed that this anomalous sulfur is in models would indicate that the planet has the form of sulfates, as opposed to iron sul- been “cold and dry” for the last several billion fide – the form of the original FeS we are years. It’s widespread presence, according to proposing. It is obvious, in our model, that Clark, seems to effectively preclude former the original FeS falling out of space became models of a “warmer, wetter Mars.” oxidized, turning into sulfates. A similar fate seems to have befallen the anomalous iron Our interpretation is quite different: that that also rained on Mars from this catastro- the source of Mars’ olivine (like its anoma- phe. lous iron and sulfur) is totally external -- also coming from the destruction of Planet V, 16
rather than from conventional internal ancient fundamental problem. On a planet otherwise volcanism. exhibiting abundant evidence of extensive water flows and its attendant weathering of Because olivine is thought to be a major olivine, how can the current surface distribu- component of the mantles of the inner tion of this mineral support an ancient south- “rocky” planets, its dispersion into space in a ern hemisphere? The answer is: it can’t. major planetary collision would be inevitable. Thus, we take this wide-spread olivine as Like the anomalous presence of iron and sul- strong confirmation that a) the source of this fur in the Martian surface soils (in our model, material is new, and b) is external to Mars’ from the collisionally-exposed planetary underlying landscape; more precisely, that it’s cores), we now propose that the unexpected simply accreted mantle material from the dis- global abundance of olivine is also precisely integration of Planet’s K& V. in accord with the hypothesis presented here: that a collision/explosion of two major Earth- Point number two: by overlaying Pal- type planets released enormous quantities of ermo’s “stain global distribution” with the mantle material directly into space. And that USGS TES mineral map from Clark and Hoe- Mars inevitably swept up a significant fen, we can easily assess the second correla- amount of this rapidly condensed material. tion. As one can see (Figure 23), the “water Because Mars’ climate radically changed stain” image clusters occupy – almost exclu- immediately after this Event, and its remain- sively – areas with little or no olivine. This is ing water froze, the presence of large quanti- also entirely consistent with the model we’ve ties of unweathered olivine on Mars can only proposed, that these stains are evidence of be another striking signature of. Mars’ former current, extensive, ground-based liquid water. existence as a satellite of Planet V -- which (the olivine confirms) was then catastrophi- Further corroborating evidence for this cally destroyed. dramatic sequence of events comes from ad- ditional TES data. As reported in If our model is correct, there should be SCIENCE,42 two distinct surface spectral sig- two additional observations strongly support- natures have now been identified on Mars ing this assertion. First, the olivine that TES from low-albedo regions of the planet. Com- detected should be primarily concentrated in parisons with spectra of terrestrial rock sam- the areas defined as being from the blast wave ples indicate that the two compositions are a pattern of Planet V’s destruction. Second, the basaltic mix dominated by plagioclase feld- current water “stains” should cluster in areas spar and clinopyroxene, and an andesitic with low current olivine detection. (silicic) composition dominated by plagio- clase feldspar and volcanic glass. The distri- Point number one: examination of the bution of these two distinct mineral composi- global olivine distribution map from TES tions is, again, split roughly along the plane- (Figure 22), shows that over 90% of this im- tary dichotomy line. The basaltic composi- portant mineral is concentrated in areas south tion is confined to the heavily cratered terrain of the “line of dichotomy” on Mars – where in the south, and the more silicic composition impact debris from Planet V is also concen- is concentrated in the northern plains. trated. Again, olivine in this amount would normally be found in unweathered volcanic This separation of Mars into two distinct fields newly erupted from the planetary man- mineralogical regimes, composed now of two tle. Since the standard model for explaining very different surface materials – one consid- Mars’ heavily cratered southern hemisphere ered “primitive” (because the chemistry is assumes a very ancient surface, this presents a simple), and the other “complex” (because its 17
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