From the David Ross book, UFOs and the Complete Evidence from Space

From the David Ross book, UFOs and the Complete Evidence from Space

The Viking 1 lander was released from the main orbiter,
and went down to a landing on the Chryse Plain on July 20,
1976. A parachute was used to brake the 1200 pound lander as
it plunged to the surface. We can understand a parachute
working in the Earth's atmosphere of several hundred
millibars pressure. But since NASA stated that the surface
pressure on Mars is only 7 millibars, and less than a
millibar a few miles up, what inflated the parachute and
caused any kind of drag to slow down the descending lander?
The answer is simple: the same dense atmosphere that was
photographed during the telescopic studies, and the same one
that the NASA censors deny is there.

Posted by Dean

People,

The Moon and Mars do not have enough mass to cause enough gravity effects to hold down an atmosphere. This is only so according to the Newtonian idea that the density of mass is causitive of gravity effects; or at least, always indicative of the intensity of gravity in all circumstances and all places.

So if an orb "shows up" which is too small to have the gravity necessary to hold down an atmosphere, but that there is an atmosphere anyway, then this fact would be highly suggestive that gravvity effects are not dependent upon mass. The usual alternative suggested is that gravity effects are caused by electromagnetic repulsions and attractions.

The powers-that-be don't want you to discover, nor harness, the secrets of gravity, therefore, they lie. They think that they lie for a good cause and, in many ways, they are probably right.

On the Martian Atmosphere: july

People,

A hollow cavity cannot exist in the context of Newtonian gravity because the shell of the Earth would collapse in on itself. Unless the shell was extremely thick, which would put the inner surfaces too close to each other, and too close to the inner Sun.

http://www.holloworbs.com/july.htm

http://www.holloworbs.com/Lunar_Atmosphere.htm