Saturday, December 8, 2012

With a view from beyond the moon, an astronaut talks religion, politics and possibilities


Viktor Toth posted on Google+ and Facebook this clip.  It references a very infomative article in the Seattle Times (see below).
- LRK -
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Viktor Toth

 7:55 AM  -  
 Google Reader
  -  Public
Atheist Moon »
One of my favorite photographs ever, in fact one that I even use on my Facebook timeline page as a background image, was taken by a certain Bill Anders when he was flying almost 400,000 km from the Earth. Anders was one of the first three members of our species who flew to another celestial body (albeit without landing on its surface; that came a bit later.) Yesterday, I read a very interesting article about Anders, both his trip on board Apollo ...
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The Seattle Times -  Pacific NW Magazine
Originally published December 7, 2012 at 12:01 PM | Page modified December 7, 2012 at 7:59 PM

With a view from beyond the moon, an astronaut talks religion, politics and possibilities

When you are one of the first three of your species to leave your planet and travel to another, certain things tend to stick with you, even a half-century later. Just ask Bill Anders.
Pacific NW staff writer
THE PASSAGE of time has rounded the sharp edges of some details. But on certain nights, Maj. Gen. William A. Anders, USAF, Ret., stands outside his Orcas Island home, gazes across the ink-black night sky over San Juan Channel and feels a brilliant new moon pull his mind all the way back into its orbit.
When you are one of the first three of your species to leave your planet and travel to another, certain things tend to stick with you, even a half-century later. For Anders, the brightest highlights of his historic flight on Apollo 8, from the Earth to the moon, 44 years ago this month, are more vivid than the most recent mooring of his boat, Apogee, at Deer Harbor.
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[See 12 image clips at article site. - LRK -]
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See related Apollo 8 article.  Much information an d more links.
- LRK -

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Originally published December 7, 2012 at 6:27 PM | Page modified December 7, 2012 at 7:53 PM

See the Apollo 8 mission and learn more from the astronaut who lived it

Apollo 8 astronaut Bill Anders shares views on his historic trip around the moon, his famous "Earthrise" photo, NASA and the politics of space, religion and the possibility of intelligent life in outer space.
A lot of great information about Bill Anders' Apollo 8 mission, as described in the Dec. 9 Pacific NW Magazine is available, and much of it couldn't be shoehorned into a single story. But some of his thoughts from our interviews, given their candor and historical value, were too good not to repeat. So here is a collection of supplementary material, ranging from multimedia links to Anders' own thoughts.
— Ron Judd
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More on the Apollo 8 mission.
- LRK -

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Apollo 8, the first flight to take men to the vicinity of the Moon, was a bold step forward in the development of a lunar landing capability. With only minor problems, all spacecraft systems operated as intended, and all primary mission objectives were successfully accomplished. Crew performance was admirable throughout the mission. The navigation techniques developed for translunar and lunar orbital flight proved to be more than adequate to maintain required accuracies for lunar orbit insertion and trans-Earth injection. Communications and tracking at lunar distances were excellent in all modes.
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Youtube video of Apollo 8 launch.
- LRK -

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Apollo 8 Launch


Uploaded on Jul 28, 2007
Edited footage of the Apollo 8 launch, several camera views compiled. Runs from T-00:25 through T+03:25.
See the mighty Saturn V launch vehicle in action, carrying humans for the first time. Watch out for an excellent shot of the staging sequence at the 3 minute mark in the video.

For information on how to obtain high quality footage like this visit www.spacecraftfilms.com
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Here is to looking up, maybe near, maybe far, maybe even a star.
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WHAT THE MIND CAN CONCEIVE, AND BELIEVE, IT WILL ACHIEVE - LRK -

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Thursday, December 6, 2012

LPOD Lunar photo of the day FOR December 6, 2012


I was doing some more checks on the LPOD web site and today's  image was fitting with the announcement from GRAIL about the new lunar gravity map.
- LRK -

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December 6, 2012
image by NASA/JPL-Caltech/IPGP

A windfall of first result was presented yesterday by Maria Zuber and team members of the Grail spacecraft currently orbiting the Moon. Grail's tandem spacecraft, Ebb  and Flow, yield the most precise measurements ever made of lunar gravity. Combining the new gravity data with the unexcelled topography from LRO allows the calculation of crustal thickness, as shown in this map by Wieczorek and other Grail scientists. Red marks the thickest crust, up to about 60 km, and dark blue to purple is thinnest.

Remarkably, the crust in parts of Mare Crisium and Mare Moscoviense is only 1 km thick or less. On Earth the thinnest crust under ocean floors is about 10 km thick and attempts to drill through it to reach the Moho, the crust-mantle boundary, failed. In Crisium, a crater 5 km wide could penetrate the crust and reach the lunar mantle; such a crater would be an important sample return target. The average lunar crustal thickness is found to be about 34 km, with the thickest being about 60 km in the farside highlands, of course some of that is due to piles of ejecta from the South Pole-Aitken basin. The purple stars represent areas that data from the Japanese Kaguya spacecraft indicated to be olivine-rich. Olivine is a mineral that is thought to be associated with the mantle, and the distribution of rare olivine around basins is consistent with their excavation of mantle material (which otherwise is not indicated by geochemistry). The excess of olivine around Crisium and Moscoviense is said to be expected because of their very shallow crusts, but of course the basin-forming impact is why the crust is thin. 

Chuck Wood

Related Links
More than a dozen different maps are shown in the Grail image gallery.
The Moho Song
http://www.nasa.gov/mission_pages/grail/multimedia/gallery/gallery-index.html
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If by chance you have the time or inclination to look further into the LPOD Wikispaces you will find comments and files noted.  One PDF file for a August 2010 meeting about the morphology of the moon I found interesting.
- LRK -

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Pages and Files
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Workshop Document Briggs version 4
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Let me see if I can copy some snips from the conference agenda just to make us all feel bad that we couldn't have been there.  :-)
- LRK -

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A Lunar Morphology Workshop
Thursday, August 5, 2010

We are pleased to offer a pre-Stellafane workshop at the historic Hartness House Inn and Porter-Hartness Museum of Telescope Making located in Springfield, Vermont, cosponsored by the Antique telescope Society. Proceeds will go towards the purchase of a replacement furnace for the Museum, which is run by volunteers from the Springfield Telescope Makers. This year we have added an evening banquet and after-dinner speaker, Professor Peter Schultz from Brown University.
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3:00 – 3:45 William Sheehan A man in a far-away place with an idea far ahead of its time: A. C. Gifford and the Modern Impact Theory of Lunar Crater Formation
3:45 – 4:30 Richard Evans Lunar rock and mineral mapping using public-domain software with Clementine and Lunar Prospector data: The Geological Lunar Research Group (GLR) Experience
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7:15 – 8:15 Peter Schultz Secrets from the Shadows of the Moon: Results from LCROSS
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Bert Willard Russell W. Porter – His lunar drawings and crater Porter
While living in Port Clyde, Maine, Porter made some fanciful drawings of the moon using his 16-inch polar telescope. Having spent many years above the Arctic Circle, he likened the lunar landscape to that of the polar landscape. The drawings are from the prospective of a lunar probe about to land on the moon. These were published in Popular Astronomy magazine in 1916. They will be compared to modern photographs taken by a member of the Springfield Telescope Makers.

Chuck Wood Introduction to lunar morphology

Peter Schultz Making the man in the Moon: Observing the Moon in the context of its geological history

Tom Dobbins Transient Lunacy

William Sheehan A man in a far-away place with an idea far ahead of its time: A. C. Gifford and the Modern Impact Theory of Lunar Crater Formation
The craters of the Moon, discovered by Galileo with his small telescope, are the distinguishing feature of the lunar surface. From the first, every glance at the surface of the Moon called forth the question of the origin of these remarkable features. Perhaps in part because of the name, the craters were long believed by most astronomers to be volcanic, but after it was reliably established (by Chladni and others in the 18th century) that stones--meteorites--actually fell from the sky onto the surface of the Earth, early versions of a meteorite impact theory were proposed to explain the lunar craters. These theories assumed that the meteorites fell onto the lunar surface while it was still in a plastic state and--in order to account for the uniformly circular outlines of the lunar craters--they were supposed to have dropped nearly vertically onto the lunar surface. These ideas were not, however, regarded as plausible by most astronomers.

Even the pioneer of the modern impact theory, the geologist G.K. Gilbert, who in 1892 presented his analysis that the lunar maria were formed by impacts, assumed that these structures were formed by mechanical impacts like the holes formed in a target fired from a gun. In order to account for their circularity, he too assumed they resulted from nearly vertical falls--and introduced the ad hoc assumption that the Earth must once have been surrounded by a Saturn-like ring to account for the perpendicularity of their encounters with the Moon.

The great breakthrough in understanding the formation of lunar craters came from applying basic principles of physics. In 1915, just after the beginning of World War I, the eccentric New Zealand Professor A.W. Bickerton, author of the controversial "partial impact theory" to explain novae and a host of other astronomical phenomena, realized that meteors travel with sufficient speed to produce results like those being seen with the exploding shells of the battlefields of Flanders and the Somme. Bickerton, however, was a poor mathematician; and it was left to his
friend and colleague A. C. Gifford--who as a student had won the Herschel prize for mathematical astronomy at Cambridge--to demonstrate, in 1924, the physics of impact, and to show that a collision of a meteorite with the Moon would be explosive in nature, and produce features modeling in all respects the actual forms of the lunar craters. Because Gifford published only in obscure New Zealand journals, his work remained practically unknown. However, it is now clear that Gifford anticipated all of the major ideas of the modern impact theory later developed (independently) by Ralph B. Baldwin, Eugene M. Shoemaker and others a generation later, and that he deserves to be more widely appreciated as one of the most important figures in the modern study of the Moon.
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Reading again the paragraph above:
"Because Gifford published only in obscure New Zealand journals, his work remained practically unknown. However, it is now clear that Gifford anticipated all of the major ideas of the modern impact theory later developed (independently) by Ralph B. Baldwin, Eugene M. Shoemaker and others a generation later, and that he deserves to be more widely appreciated as one of the most important figures in the modern study of the Moon."

You do notice Ralph B. Baldwin, and Eugene M. Shoemaker.  Early on it was thought that it was volcanic action that scared the lunar surface.  How could meteors make round holes in the regolith? Much discussion there.  Hmm, best sit down and do some reading in "Measure of the Moon" by Ralph B. Baldwin.

And for you folks, this may be helpful.
-LRK -

Here is to looking up, maybe near, maybe far, maybe even a star.
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WHAT THE MIND CAN CONCEIVE, AND BELIEVE, IT WILL ACHIEVE - LRK -

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Wednesday, December 5, 2012

LPOD Lunar photo of the day


I was trying to find some on-line information on the book, "The Measure of the Moon" by Ralph B. Baldwin and came across this wiki space.  A beautiful picture at the below link.
- LRK -

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image by Dani Caxete, Road of "Puerto de Navacerrada" Madrid (Spain)

This beautiful picture should really be reserved for January 1 to welcome the new year, but it is too gorgeous to hold. And I won't even write the obvious story of the Moon's increasing gravity about to pull trees out of the ground and send them into space. 

Chuck Wood

Technical Details
2012/12/2, 3:50. Nikon D7000 with Samyan 8mm lens and 30 sec exposure @ f/5.6, ISO 500, WB 4000K, air temperature -7ยบ C

Related Links
Dani's website
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You may find the site useful. Will get to why  I was there in a moment.
- LRK -

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THE-MOON WIKI

Motivation

During the late 1800s and well into the 1900s it seemed that every book that described the craters, mountains and other features of Earth's moon was titled The Moon. In my mind this came to stand for an encyclopedia-like series of descriptions of features on the lunar surface. In general, more recent books, especially those by professional scientists, describe the processes that formed and modified the Moon, and the surface features themselves are no longer described systematically. But for many lunar observers and others thinking about the Moon as a place, knowledge of individual features is important.

This wiki - The-Moon - is an experiment to collect data about individual features, arranged alphabetically by name. As a wiki anyone (after registering) can add or edit every entry. I encourage folks interested in the Moon to contribute to the site. When you are ready to add to The-Moon visit the How to Help option to the left.

It turns out that this wiki is the most convenient way to find all the photos and maps of any named lunar feature!
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OK, I have the book, "The Measure of the Moon" and I had been looking for an on-line copy and found none. The next best thing was to see if hard copies might be available for those interested in what was known about the Moon before we actually went there with the Apollo missions.
- LRK -

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Ralph Baldwin: The Face of the Moon (1949) & The Measure of the Moon (1963)

(glossary entry)

Description

Two highly influential books providing evidence for the meteoritic origin of many craters on the Moon and establishing probably lunar timescales.

Additional Information

  • Baldwin's views of the Moon were influenced, in part, by his experiences developing fuses for explosives during World War II.
  • Although professionally trained as an astronomer, Baldwin's main job was running a family owned tool-making company.
  • The second book (1963) expands on the first (1949), making a much stronger case.
  • The 1965 book is a text for college students, summarizing both Baldwin's views and those of others.
Contents of The Measure of the Moon
  • Outline of the Problem
  • Modern Terrestrial Meteoritic Craters
  • Probable and Possible Terrestrial Meteoritic Craters
  • Ancient Meteroritic Craters and Cryptovolcanic Structures
  • Crater Frequency on Earth and Moon
  • Characteristics of Explosion Craters, Terrestrial Meteoritic Craters, and Lunar Craters
  • Relationships between Crater Parameters
  • Determination of Energies Needed to Produce Meteoritic Craters
  • Variations in Lunar Craters as Functions of their Ages
  • The Problem of the Moon's Motion and Shape
  • The Shape of the Moon and the New Contour Map
  • Nature of the Lunar-Surface Materials as Determined by Reflected Light
  • Nature of the Lunar-Surface Materials as Determined by Heat Measures at Infrared and Radio Frequencies
  • Tektites
  • Analyses of Earlier Theories of the Moon's History
  • The Circular Maria and Related Structures
  • The Lava Flows
  • The Atmosphere of the Moon
  • The Lunar Rays
  • The Central Peaks of Lunar Craters
  • Rilles, Wrinkles and Faults
  • The Lunar Grid System
  • Domes
  • The Heat Balance of the Moon
  • Magnetic Field of the Moon
  • Recent Changes on the Moon
  • Summary and Conclusions
  • Appendicies
    • Derivation of the Replationship between the Distance of the Moon and Geologic Time
    • Tables
    • The Lunar Tidal Bulge as a Function of the Moon's Distance
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And maybe in a library near you.
-LRK -

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The face of the moon.

The measure of the moon.

A fundamental survey of the moon

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The reason I was looking at "The Measure of the Moon" was to get a feel for what was happening with research about the Moon back when that "Nuke The Moon" rumor was festering.

Let me finger poke out one paragraph Baldwin's Introduction to "The Measure of the Moon" .

"It is beyond hope that we shall ever have a complete and definitive answer to all lunar problems. Geologists and others have been studying the earth at close range for generations, but there are many problems for which opposing solutions are still offered and others on which general agreement is not yet possible.  In a real sense they have only scratched the surface.  How much more difficult it is, then, to solve all the problems concerning a distant satellite. Landing on the moon and analyzing its materials will help greatly but will raise more problems than are solved."

And the rest is history.  :-)

Here is to looking up, maybe near, maybe far, maybe even a star.
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WHAT THE MIND CAN CONCEIVE, AND BELIEVE, IT WILL ACHIEVE - LRK -

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Monday, December 3, 2012

NASA Mars Rover Fully Analyzes First Martian Soil Samples - Ooops


It was just announced that the Mars Rover Facility has analyzed its its first Martian soil samples but I note a bit of caution about some of the results.  Did we bring along from Earth any contaminants that might affect the results?
- LRK -

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NASA Mars Rover Fully Analyzes First Soil Samples

December 03, 2012
PASADENA, Calif. - NASA's Mars Curiosity rover has used its full array of instruments to analyze Martian soil for the first time, and found a complex chemistry within the Martian soil. Water and sulfur and chlorine-containing substances, among other ingredients, showed up in samples Curiosity's arm delivered to an analytical laboratory inside the rover.

Detection of the substances during this early phase of the mission demonstrates the laboratory's capability to analyze diverse soil and rock samples over the next two years. Scientists also have been verifying the capabilities of the rover's instruments.

Curiosity is the first Mars rover able to scoop soil into analytical instruments. The specific soil sample came from a drift of windblown dust and sand called "Rocknest." The site lies in a relatively flat part of Gale Crater still miles away from the rover's main destination on the slope of a mountain called Mount Sharp. The rover's laboratory includes the Sample Analysis at Mars (SAM) suite and the Chemistry and Mineralogy (CheMin) instrument. SAM used three methods to analyze gases given off from the dusty sand when it was heated in a tiny oven. One class of substances SAM checks for is organic compounds -- carbon-containing chemicals that can be ingredients for life.

"We have no definitive detection of Martian organics at this point, but we will keep looking in the diverse environments of Gale Crater," said SAM Principal Investigator Paul Mahaffy of NASA's Goddard Space Flight Center in Greenbelt, Md.
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SAM tentatively identified the oxygen and chlorine compound perchlorate. This is a reactive chemical previously found in arctic Martian soil by NASA's Phoenix Lander. Reactions with other chemicals heated in SAM formed chlorinated methane compounds -- one-carbon organics that were detected by the instrument. The chlorine is of Martian origin, but it is possible the carbon may be of Earth origin, carried by Curiosity and detected by SAM's high sensitivity design. 

"We used almost every part of our science payload examining this drift," said Curiosity Project Scientist John Grotzinger of the California Institute of Technology in Pasadena. "The synergies of the instruments and richness of the data sets give us great promise for using them at the mission's main science destination on Mount Sharp." 
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A lot of effort goes into making sure you don't take things from Earth that could contaminate another planet and in the case of the Apollo missions, that you didn't bring something back from the Moon that could contaminate Earth. 
- LRK -

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FINAL PREPARATIONS: 1968

Problems with Back-Contamination Control

The receiving laboratory was only part of the scheme for preventing contamination of the earth by alien organisms. Between the spacecraft floating on the Pacific Ocean and the laboratory in Houston was a long chain of events that offered several chances to contaminate the environment. Early in 1968, spumed by expressions of concern by scientists outside the government, the Interagency Committee on Back Contamination (ICBC) revived the question of whether lunar contaminants could be completely prevented from escaping into the biosphere during recovery operations, particularly between the floating command module and the mobile quarantine facility aboard the recovery ship. For two years the committee had been uneasy about this problem, and at its February meeting the chairman opened the discussion once more. The committee asked MSC's landing and recovery division to provide
a detailed discussion on the return lunar mission [focusing on] containment countermeasures on the lunar surface, in the Lunar Module (LM) ascent stage, during LM-CM transfer, during CM earth return, splashdown, retrieval, operations onboard the recovery vessel, transfer into the mobile isolation unit, and delivery and transfer into the LRL.
Committee members also wanted details of MSC's contingency plans for biological containment in case the spacecraft came down outside the primary recovery zone.31
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There procedures and requirements and treaties involved concerning the potential for cross conamination by spacecraft.
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Office of Planetary Protection
Planetary protection is the term given to the practice of protecting solar system bodies (i.e., planets, moons, comets, and asteroids) from contamination by Earth life, and protecting Earth from possible life forms that may be returned from other solar system bodies. Planetary protection is essential for several important reasons: to preserve our ability to study other worlds as they exist in their natural states; to avoid contamination that would obscure our ability to find life elsewhere — if it exists; and to ensure that we take prudent precautions to protect Earth’s biosphere in case it does.
International Treaties and Organizations with Cognizance of Planetary Protection Activities

The 1967 United Nations Treaty on Principles Governing the Activities of States in the Exploration and Use of Outer Space, Including the Moon and Other Bodiesstates that all countries party to the treaty “shall pursue studies of outer space, including the moon and other celestial bodies, and conduct exploration of them so as to avoid their harmful contamination.” 
Internationally, technical aspects of planetary protection are developed through deliberations by the Committee on Space Research (COSPAR), part of the International Council of Science (ICSU), which consults with the United Nations in this area. The COSPAR Panel on Planetary Protection develops and makes recommendations on planetary protection policy toCOSPAR, which may adopt them as part of the official COSPAR Planetary Protection Policy.
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To get a feel for what needs to be done, take a look at some of the methods.
- LRK -

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Methods And Implementation
NASA uses a variety of methods to measure, control and reduce spacecraft microbial contamination for planetary protection purposes. Assembly of spacecraft hardware is carefully controlled and often takes place in clean-room facilities using, aseptic techniques in order to meet planetary protection requirements. Dry heat microbial reduction techniques first used on the Viking spacecraft are still used today. Measurement techniques are cultivation-based microbial assays using well characterized biological methods.
Clean Rooms and Microbial Barriers

NASA requires that planetary protection procedures involving sterile items and sample processing must be conducted in Class 100 clean rooms, as defined by federal standard (equivalent to ISO Class 5). Such clean rooms feature laminar-air-flow systems to filter out contaminants; these systems work by keeping the air within a space moving in one direction along parallel flow lines at a uniform velocity through very fine filters. Planetary protection procedures specify the types of devices that may be used for air sampling in these environments.
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Maybe no harm to Mars if you bring a bit of dirt along.
- LRK -

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Summary
Biological Contamination of Mars: Issues and Recommendations
Task Group on Planetary Protection, Space Studies Board, National Research
Council. National Academy Press, Washington, D.C (1992).

In anticipation of planned U.S. and Russian robotic missions to Mars in the early 1990s, NASA requested Space Studies Board advice on how to update the nature of planetary protection requirements to reflect changes in the years since the Apollo and Viking missions and to incorporate new thoughts about life on Mars and the growing environmental awareness of the populace. Recommendations were requested in time for the 1992 COSPAR meeting in order to update international planetary protection policies as needed.
This task group focused on making recommendations concerning the protection of Mars from forward contamination (i.e., contamination of the martian environment by terrestrial organisms) during upcoming missions. It specifically considered then-current views about the chemical and physical properties of Mars as well as the potential survival of Earth organisms on Mars and approaches to planetary protection used by the U.S. and Russia. In its deliberations, the task group distinguished between missions whose goals included reconnaissance and measurement vs. those that specifically included experiments to detect life.

The task group viewed the problem of forward contamination as separable into two principal issues: 1) the potential for growth of terrestrial organisms on Mars (Pg), and 2) the importation of terrestrial organic contaminants, living or dead, in amounts sufficient to compromise the search for evidence of past or present life on Mars itself.
  1. Based on current knowledge of conditions on Earth that limit cell growth and on the best estimates of surface conditions on Mars, the task group concludes that no known terrestrial organisms could grow on the martian surface. However, this fact does not alter the case as far as contamination of a possible past or extant martian biosphere is concerned. Prudence dictates that bioload reduction on all lander missions to Mars must continue to be seriously addressed. The issue of spacecraft cleanliness is particularly crucial when life-detection experiments are included in the scientific payload.
    The task group concurred unanimously that “Forward contamination, solely defined as contamination of the martian environment by growth of terrestrial organisms that have potential for growth on Mars, is not a significant hazard. However, forward contamination more broadly defined to include contamination by terrestrial organic matter associated with intact cells or cell components is a significant threat to interpretation of results of in situ experiments specifically designed to search for evidence of extant or fossil martian microorganisms.”
  2. Advances in techniques for assessing the existence of microorganisms will have a strong impact both on bioburden assessment procedures and on future life-detection experiments because of their increasingly greater sensitivity and specificity. The task group strongly recommends that efforts be made to explore current analytical methods for use in bioburden assessment and inventory procedures before spacecraft assembly and launch. Specific promising methods identified included epifluorescent microscopic techniques for directly counting viable cells, and the polymerase chain reaction which increases detection sensitivity by enzymatically amplifying specific biomarkers of even a single cell to detectable levels.
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In the case of Curiosity maybe an Ooops.
- LRK -

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Curiosity’s drill may contaminate Mars with microbes from Earth

Posted September 12th, 2012
Last week, I wrote about a hypothetical contamination of Mars and how NASA tries to prevent this. Now it seems this scenario actually could become reality.
There might be a problem with a drill bit. It was planned to sterilize all drill bits and keep them inside a box to be opened only after Curiosity’s touchdown on Mars. But engineers grew concerns that a rough landing could damage the drill mechanism. So they decided to open the box and mount one of them in the drill – just to make sure there’s at least one working bit ready for action.
This happened without consulting NASA’s planetary protection office, which tries to make sure that all parts of the spacecraft are properly sterilized before leaving Earth. So now NASA is facing the problem that microbes theoretically could propagate if they touch water or ice.
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Looks like the source for this is the Los Angeles Times.
- LRK -

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If the Mars rover finds water, it could be H2 ... uh oh!

If Curiosity locates H2O, a simmering NASA controversy will boil over. The rover's drill bits may be tainted with Earth microbes that could survive upon touching water.


For all the hopes NASA has pinned on the rover it deposited on Mars last month, one wish has gone unspoken: Please don't find water.
Scientists don't believe they will. They chose the cold, dry equatorial landing site in Mars' Gale Crater for its geology, not its prospects for harboring water or ice, which exist elsewhere on the planet.
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Here is to looking up, maybe near, maybe far, maybe even a star.
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WHAT THE MIND CAN CONCEIVE, AND BELIEVE, IT WILL ACHIEVE - LRK -

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Sunday, December 2, 2012

No we didn't nuke the Moon back in the 50's


No we didn't nuke the Moon back in the 50's, but stories about secret plans to possibly do so exist and of recent some have been circulating on the Internet.

Bob in Texas alerted me to one of these posts and I Googled a few more similar links.  I note that bold type is often used as well as twisting what was really going on.  We launched the Apollo missions that went to the Moon and accomplished many of the items that are addressed in the Project A119 report.  You can look at the SENSATIONAL links if you have not seen, but I think much more information can be had by reading the actual report that has been scanned and presented in a PDF file on line.  (link to follow below -LRK-)
- LRK -

This is the link Bob sent me.
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Same story, different link.

Here with video clips and voice over and same story.

A little more material and pictures.

Revealed: How the U.S. planned to blow up the MOON with a nuclear bomb to win Cold War bragging rights over Soviet Union

  • Scientists were hoping for giant flash on the moon that would intimidate the Soviet Union
  • Aim of mission was to launch the nuke by 1959
  • Plan was later scrapped due to possible danger to people on Earth
PUBLISHED: 14:06 EST, 25 November 2012 | UPDATED: 17:37 EST, 25 November 2012
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When contacted by the AP, the U.S. Air Force declined to comment on the project.
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Read more: http://www.dailymail.co.uk/news/article-2238242/Cold-War-era-U-S-plan-bomb-moon-nuclear-bomb-revealed.html#ixzz2DfW5m0PR
Follow us: @MailOnline on Twitter | DailyMail on Facebook
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The plan was NOT to blow up the Moon but rather to make a flash to analyze the Moon's make up.
The Wikipedia material is less sensational and informative.
- LRK -

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http://en.wikipedia.org/wiki/Project_A119

-From Wikipedia, the free encyclopedia
Project A119, also known as "A Study of Lunar Research Flights", was a top-secret plan developed in the late 1950s by the United States Air Force. The aim of the project was to detonate a nuclear bomb on the Moon to boost public morale in the United States after the Soviet Union took an early lead in the Space Race. The existence of the project was revealed in 2000 by a former executive at the National Aeronautics and Space Administration (NASA), Leonard Reiffel, who led the project in 1958. A young Carl Sagan was part of the team responsible for predicting the effects of a nuclear explosion in low gravity.
Project A119 was never carried out, primarily because a moon landing would be a much more acceptable achievement in the eyes of the American public. The project documents remained secret for nearly 45 years, and despite Reiffel's revelations, the United States government has never officially recognized its involvement in the study
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Here is the link to the A119 report I promised.  If you take the time to read the Vol I,190 page report, there is still a bit of mystery, as Chapter 2 is contained in a Vol II, which I could not find a link to. (Probably where rumors of a more militant nature were spun. -LRK-)
-LRK-

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http://oai.dtic.mil/oai/oai?verb=getRecord&metadataPrefix=html&identifier=AD0425380
Accession Number : AD0425380
Title :   A STUDY OF LUNAR RESEARCH FLIGHTS, VOLUME I
Corporate Author : IIT RESEARCH INST CHICAGO IL
Personal Author(s) : Reiffel, L.
PDF Url : AD0425380
http://www.dtic.mil/cgi-bin/GetTRDoc?Location=U2&doc=GetTRDoc.pdf&AD=AD0425380
Report Date : 19 JUN 1959
Pagination or Media Count : 190
Abstract : Nuclear detonations in the vicinity of the moon are considered in this report along with scientific information which might be obtained from such explosions. The military aspect is aided by investigation of space environment, detection of nuclear device testing, and capability of weapons in space. A study was conducted of various theories of the moon's structure and origin, and a description of the probable nature of the lunar surface is given. The areas discussed in some detail are optical lunar studies, seismic observations, lunar surface and magnetic fields, plasma and magnetic field effects, and organic matter on the moon. (Author)
Descriptors :   *LUNAR PROBES, *MOON, NUCLEAR EXPLOSIONS, DENSITY, TEMPERATURE, MAGNETIC FIELDS, ACCELEROMETERS, MAGNETOHYDRODYNAMICS, COSMIC RAYS, SOLAR SAILS, SOLAR WIND, SEISMOGRAPHS, PHYSICAL PROPERTIES, THEORY, ELECTRONS, SEISMIC WAVES, GRAVITY, GEOPHYSICS.
Subject Categories : Unmanned Spacecraft
Distribution Statement : APPROVED FOR PUBLIC RELEASE
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A STUDY OF LUNAR RESEARCH FLIGHTS
Vol I
by
L. Reiffel
ARMOUR RESEARCH FOUNDATION
of
Illinois Institute of Technology
19 June 1959
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snip
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I hope you have the time to take a look at the PDF file.  You will see that there were different ideas of what the Moon was like and we are still changing our ideas as we get more information from satellites in orbit and looking again at the material from the Apollo missions.  Happy researching. :-)  [Glad we didn't destroy the Moon.  It would have messed up the tide tables.  How would I know when to go clamming! http://wdfw.wa.gov/fishing/shellfish/razorclams/]
- LRK -

Here is to looking up, maybe near, maybe far, maybe even a star.
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WHAT THE MIND CAN CONCEIVE, AND BELIEVE, IT WILL ACHIEVE - LRK -

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