Phobos is spaceship says famous scientist
Astrophysicist Dr. Iosif Samuilovich Shklovsky calculated the orbital motion of Martian satellite Phobos and came to the jaw-dropping conclusion that the moon is artificial, hollow, and basically a titanic spaceship.
Dr. Iosif Samuilovich Shklovsky
The scientist is world-renown for penning the classic science book, “Intelligent Life in the Universe” with famous Cornell University professor, the late Carl Sagan of PBS and Voyager space probe fame.
Fear and Horror
Mars’ two moons, Phobos and Deimos, translate into “fear” and “horror.” As Mars is named after the god of war, the names seem appropriate. Both satellites were discovered in 1877 by U.S. astronomer Asaph Hall who never guessed they were artificial.
Both moons are extremely odd, especially the tumbling moon of fear: Phobos. Shklovsky puzzled over them.
Phobos and Deimos.
Deeply troubling facts
Two facts deeply troubled Shklovsky.
First, both moons are too small. No other planet in the solar system has moons as tiny as the Martian moons. They’re unique.
Second, their origin bothered him. Were they captured asteroids as others assumed? No, they could not be! Their orbital plane was all wrong. And they’re too close to Mars. Much too close. Even more amazing–Phobos changes its speed from time to time.
Impossible, yet true!
Phobos is shaped like interstellar spaceship
Russian astronomer Dr. Cherman Struve spent months calculating the Martian moons’ orbits with extreme accuracy early in the 20th Century. Yet, Shklovsky astutely noted, as the years progressed into decades the mystery moon’s orbital velocity and position no longer matched its mathematically predicted position.
After lengthy study of the tidal, gravitic, and magnetic forces, Shklovsky came to the inescapable conclusion that no natural causes could account for the origins of the two odd moons or their bizarre behavior, particularly that exhibited by Phobos.
The orbit of that fantastic moon was so peculiar, so bizarre, that Phobos had to be a gigantic spaceship.
Every other possible cause was carefully considered and resignedly rejected. Either alternate explanations had no supporting proof or the math was wildly off.
So, Phobos had to be accelerating as it lost altitude, yet could the outer fringes of the thin Martian atmosphere be affecting it? Was the atmosphere actually causing a braking action like the deteriorating orbit of a slowing Earth satellite?
A hollowed out Martian moon
Phobos is a hollow, empty tin can
During an interview about the peculiarities surrounding Phobos, Shklovsky said, “In order to make this braking action so significant, and taking into account the extremely rarefied Martian atmosphere at this altitude, Phobos should have very small mass, that is, very low average density, approximately one thousand times smaller than the density of water.”
A density that low, less than an Earth cloud, would have dispersed Phobos eons ago. That could not be the solution.
“But can a continuous solid have such low density, probably smaller than that of air? Of course not! There’s only one way in which the requirements of coherence, constancy of shape of Phobos, and its extremely small average density can be reconciled. We must assume that Phobos is a hollow, empty body, resembling an empty tin can.”
A tin can indeed! Like a spaceship is a tin can in the cosmos. For all intents and purposes, the Apollo Lunar Excursion Module was a tin can exceedingly smaller than Phobos, of course.
Computer modeling of weird ‘moons’
“Well, can a natural celestial body be hollow? Never! Therefore, Phobos must have an artificial origin and be an artificial Martian satellite. The peculiar properties of Deimos, though less pronounced than those of Phobos, also point toward an artificial origin.”
Alien spaceships the size of small moons orbiting Mars? That makes the so-called “Face on Mars” look ridiculously feeble by comparison!
Yet, no less than the United States Naval Observatory weighed in on the Russian astrophysicist’s amazing revelation, stating: Dr. Shklovsky quite correctly calculated that if the acceleration of Phobos is true, the Martian moon must be hollow, since it cannot have the weight of a natural body and behave in the prescribed manner.
Thus, even that august American institution conceded that mysterious alien ships might be orbiting Mars…the objects’ strange origins and ultimate purposes completely unknown.
Speculations over what the giant artificial spaceships might be have ranged from massive Martian space observatories, to half-completed generational interstellar spaceships, or even gargantuan planet-killing space bombs left over from an interplanetary war waged millions of years ago.
If they are world-destroying bombs, hopefully they’re duds…
The Phobos Monolith
The Phobos monolith is a surface feature, a large rock, on the moon Phobos which orbits Mars. It is a boulder about 85 meters (~280 feet) across. A monolith is a geological feature consisting of a single massive piece of rock. Monoliths also occur naturally on Earth, but it has been suggested that the Phobos monolith may be a piece of impact ejecta.
The monolith is a bright object near Stickney crater, described as a “building sized” boulder, which casts a prominent shadow. It was discovered by Efrain Palermo, who did large surveys of Martian probe imagery, and later confirmed by Lan Fleming, an imaging sub-contractor at NASA Johnson Space Center.
The general vicinity of the monolith is a proposed landing site for a Canadian Space Agency vehicle, funded by Optech and the Mars Institute, for an unmanned mission to Phobos known as PRIME (Phobos Reconnaissance and International Mars Exploration).
The PRIME mission would be composed of an orbiter and lander, and each would carry four instruments designed to study various aspects of Phobos’ geology. At present, PRIME has not been funded and does not have a projected launch date.
The object appears in Mars Global Surveyor images SPS252603 and SPS255103, dated 1998. The object is unrelated to another monolith located on the surface of Mars, which NASA noted as an example of a common surface feature in that region.