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Originally posted by TheBorgAnyone have a timestamp for it? That would answer this question, and at least eliminate that possibility.
Something just occurred to me. I was looking at that image again, and it almost looks like there was a geomagnetic storm going on at the time that that image was taken. Anyone have a timestamp for it? That would answer this question, and at least eliminate that possibility.
Originally posted by TheBorg...but I'm still having trouble with this whole atmosphere thing.
This is all based on what I think is a very grainy image, presented to us in all of its splendor by Zorgon.
Now, after having looked at that image again, doesn't it seem odd to you that the blurry portion of the picture seems to be almost out of focus blurry, rather than smog-filled blurry?
I understand the concept of an atmosphere and all that goes with that, but I'm still at a loss for how this image shines any light on that possibility.
To me anyway, it does nothing but damage it. I can reference countless other images, in fact 99.95% of the rest of the images, that show quite a different side to this story.
"If a theory is outweighed by overwhelming evidence to the contrary, then one must assume the obvious; that the theory is faulty." - TheBorg
Something just occurred to me. I was looking at that image again, and it almost looks like there was a geomagnetic storm going on at the time that that image was taken. Anyone have a timestamp for it? That would answer this question, and at least eliminate that possibility.
Originally posted by TheBorg...I don't believe that the Moon has an atmosphere. However, I feel that it's important to state that if such evidence did come to light that proves that in fact it does, then I'll be more than willing to retract my statements, and accept a new outlook on it.
However, a loophole in Space Law allows individuals and companies to hold Mineral Rights on the Moon, Mars and other celestial bodies. Growing concern from Scientists that these rights may be held hostage have been alleviated by a three man North American team; Dr. Joseph Resnick, Dr. Timothy R. O'Neill and Guy Cramer (ROC-Resnick/O'Neill/Cramer team) who have acquired the mineral rights for 95% of the side of the moon that faces Earth, the polar regions and 50% of the far side of the moon.
In addition to the near-surface gases and the extensive sodium-potassium cloud detected around the Moon, a small amount of dust circulates within a few metres of the lunar surface.
Originally posted by zorgon
However, a loophole in Space Law allows individuals and companies to hold Mineral Rights on the Moon, Mars and other celestial bodies. Growing concern from Scientists that these rights may be held hostage have been alleviated by a three man North American team; Dr. Joseph Resnick, Dr. Timothy R. O'Neill and Guy Cramer (ROC-Resnick/O'Neill/Cramer team) who have acquired the mineral rights for 95% of the side of the moon that faces Earth, the polar regions and 50% of the far side of the moon.
95%
and 50% of the back side???
Three guys???
Anybody else getting a cold shiver?
[edit on 26-10-2006 by zorgon]
Originally posted by zorgon
While researching what would be mined up there and preparing a page which I will post tomorrow... I came across THIS disturbling little tidbit...
Dr. Joseph Resnick, Dr. Timothy R. O'Neill and Guy Cramer (ROC-Resnick/O'Neill/Cramer team) who have acquired the mineral rights for 95% of the side of the moon that faces Earth, the polar regions and 50% of the far side of the moon.
95%
and 50% of the back side???
Three guys???
Anybody else getting a cold shiver?
Originally posted by Zarniwoop
link to the full article (I think) ...
Lunar Atmosphere
Diurnal temperature range: >100 K to
Clementine made a controversial discovery, which, if proved correct, has major implications for humans returning to the Moon. Its S-band radio unit detected abnormal reflections from the rim of a huge crater (basin) around the lunar South Pole, in areas permanently sheltered from the Sun's rays...
These reflections could be due either to water ice or to some abnormal surface roughness condition. If indeed ice is present in significant quantity, then this precious material (which supplies water needed for life and also oxygen, when broken down by electrolysis) might allow us to establish a manned base on the Moon.
The Primary Mission
Beginning on January 15, 1998, Lunar Prospector spent one year mapping the entire surface of the Moon from a distance of about 100 kilometers (60 miles). The data collected during this phase of the mission greatly improved on the quality of data collected previously. Among the early returns from the instruments were those from the Neutron Spectrometer indicating significant amounts of water ice at the lunar poles.
The initial estimate of the amount, to be determined more accurately with later observations, is 30 to 300 million metric tons (recent thinking has raised the upper limit to perhaps as high as 3 billion tons). If melted, this larger number would fill a "lake" 10 square kilometers in area (3.1 x 3.1 km) to a depth of 10 meters. Surprisingly, the North Pole region contains about 50% more ice than its southern counterpart. The source of the water ice is probably residues from cometary bodies that impacted the polar regions, forming craters but allowing much of the comet mass to survive embedded in the target. The implications are encouraging for future exploration of the Moon, to the extent that we can establish and occupy a manned base facility over extended time because of the availability of vital water
Information on the distribution of radioactivity on the lunar surface was one goal of Lunar Prospector. This map shows that the element thorium is highest on the front side of the Moon, mainly in the highlands south of Mare Imbrium. The correspondence with the Imbrium Basin suggests that the basaltic lavas that filled it were enriched in Th. Note that corresponding highland surfaces on the farside are lower.
Thorium, as well as uranium and plutonium, can be used as fuel in a nuclear reactor. Although not fissile itself, 232Th will absorb slow neutrons to produce uranium-233 (233U), which is fissile. Hence, like 238U, it is fertile. In one significant respect 233U is better than the other two fissile isotopes used for nuclear fuel, 235U and plutonium-239 (239Pu), because of its higher neutron yield per neutron absorbed
The orange soil was brought back from the Taurus-Littrow landing site by the Apollo 17 crewmen. Scientist-Astronaut Harrison J. Schmitt discovered the orange soil at Shorty Crater. The orange particles, which are intermixed with black and black-speckled grains, are about the same size as the particles that compose silt on Earth. Chemical analysis of the orange soil material has show the sample to be similar to some of the samples brought back from the Apollo 11 (Sea of Tranquility) site several hundred miles to the southwest. Like those samples, it is rich in titanium (8%) and iron oxide (22%). But unlike the Apollo 11 samples, the orange soil is unexplainably rich in zinc. The orange soil is probably of volcanic origin and not the product of meteorite impact.
Some He3 is available on Earth. It is a by-product of the maintenance of nuclear weapons, which would supply us with about 300 kg of He3 and could continue to produce about 15 kg per year. The total supply in the U.S. strategic reserves of helium is about 29 kg, and another 187 kg is mixed up with the natural gas we have stored; these sources are not renewable at any significant rate....
In their 1988 paper, Kulcinski, et al. (see ref note below), estimate a total of 1,100,000 metric tonnes of He3 have been deposited by the solar wind in the lunar regolith. Since the regolith has been stirred up by collisions with meteorites, we'll probably find He3 down to depths of several meters.
The highest concentrations are in the lunar maria; about half the He3 is deposited in the 20% of the lunar surface covered by the maria...
The Payoff
A guess is the best we can do. Let's suppose that by the time we're slinging tanks of He3 off the moon, the world-wide demand is 100 tonnes of the stuff a year, and people are happy to pay $3 billion per tonne. That gives us gross revenues of $300 billion a year.
To put that number in perspective: Ignoring the cost of money and taxes and whatnot, that rate of income would launch a moon shot like our reference mission every day for the next 10,000 years. (At which point, we will have used up all the helium-3 on the moon and had better start thinking about something else.)
Russia's Space Corp. has developed an elaborate plan to mine helium 3 on the moon. Robots would dig up the 3-meter-deep layer of lunar dust, which contains helium 3, and heat the dirt to 300 degrees Celsius to release the gas. Since a ton of lunar soil contains just 36 grams of helium, 20 square kilometers would yield just 10 tons of helium 3. To provide energy for such an operation, Russia would build nuclear reactors the size of a tabletop. Total cost: between $40 billion and $200 billion.
Originally posted by zorgonJohn....Looks like we are to late to stake a claim... Now how in hell did they lay claim to all that before anyone evn know that was an option??
Originally posted by TheBorg When you were describing an atmosphere on the Moon, I thought you were talking about a breathable one, as in one that we humans could breathe.
Well, I was, but truth be told that is wishful thinking on my part. John seems to think so, and I suspect it may be humanly possible to catch a few gasps in the deeper recesses in the event of an emergency.
Originally posted by johnlear
with proper decompression you can stand out on the the moons surface, without a space suit or helmut, look up into the clear blue sky and take a relatively deep breath of fresh moon air.