LUNAR LASER RANGING Experiment Uncovers Moon's Geology

In summary, scientists have calculated "Love numbers" which show the elasticity of the Moon's surface, giving insight into the material beneath. These numbers support the idea that there is a partially melted zone above the Moon's core, as first suggested by Apollo program scientists. This phenomenon, caused by the gravitational pull of the Sun and Earth, also affects other moons in our solar system, such as Io and Europa. It is believed that the tidal massage from Jupiter and other massive objects keeps these moons from being frozen solid and instead allows for liquid water and volcanic activity. Love numbers are measures of elasticity, and the concept of tidal bulging and massage is essential in understanding the geology of these moons.
  • #1
wolram
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http://www.lunarrepublic.com/news/media_love_021302.shtml

The Moon's surface, pulled by the Sun and Earth, may bulge out and dip in as much as 10 centimeters (almost four inches) over 27 days. Love numbers show how elastic the Moon is, giving clues to the material under the surface. The newly calculated Love numbers support the idea, first suggested by Apollo program scientists, that a partially melted zone lies above the core.
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an ofshoot of the LUNAR LASER RANGING experiment.
i have never given a thought as to the moons geology
so i am suprised at this finding.
 
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  • #2
Originally posted by wolram
http://www.lunarrepublic.com/news/media_love_021302.shtml

The Moon's surface, pulled by the Sun and Earth, may bulge out and dip in as much as 10 centimeters (almost four inches) over 27 days. Love numbers show how elastic the Moon is, giving clues to the material under the surface. The newly calculated Love numbers support the idea, first suggested by Apollo program scientists, that a partially melted zone lies above the core.
-------------------------------------------------------------------
an ofshoot of the LUNAR LASER RANGING experiment.
i have never given a thought as to the moons geology
so i am suprised at this finding.

the tidal-bulge-massage that satellites get is good to know about
and most dramatically illustrated by photographs of Jupiter's
nearest large moon Io

Do you know about this already? I don't want to repeat already known stuff. Io would be frozen solid if it were not for love numbers or elasticity that make it susceptible to massage by Jupiter and the other large Jovian moons.

the massage keeps deforming Io and making it bulge slightly by changing amounts and this HEATS IT UP
and is the reason that instead of being frozen solid it has
molten sulfur and volcanos belching gas and sending loads of crud up into the sky---the eruptions have been actually photographed

-----footnote not for people who know it already------

so an isolated thing under its own gravity wants to be spherical

but it if is in the neighborhood of another massive thing it wants to be ovoid or oblong with two bulges towards and away from the massive object (like the Earth's ocean bulges towards and away fromt he moon and hightide comes twice a day)

ok so what if there are two massive objects. how can it bulge towards both of them. so there is a kind of massage going on as the directions and angles between the two attractors change. with a specially strong effect when they get aligned and reinforce each other

this tidal business heats all the main Jovian moons to some extent so that Europa for example has liquid water under the ice (and Sir Arthur Clark imagined a sea-monster living in the Europa under-ice ocean just to make the point especially clear, as I recall----the impulse to depict seamonsters in unexplored oceans has been with us for centuries and Sir Arthur gave into a common map-makers urge)

Someday people will take submarines into the Europa sub-ice ocean and it will be the massage by Jupiter and the other Jovian moons that is keeping that ocean liquid instead of frozen solid.

Never heard of love numbers but guess they are just measures of elasticity in various dimensions
 
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1. What is the Lunar Laser Ranging Experiment (LLRE)?

The Lunar Laser Ranging Experiment is a scientific project that uses lasers to measure the distance between the Earth and the Moon. It was first conducted in 1969 by scientists at NASA's Goddard Space Flight Center.

2. How does the LLRE work?

The LLRE works by firing a laser beam from a ground station on Earth towards a retroreflector placed on the surface of the Moon by astronauts from the Apollo missions. The laser beam is then reflected back to Earth and the time it takes for the light to return is measured. This allows scientists to calculate the distance between the Earth and the Moon with high accuracy.

3. What has the LLRE uncovered about the Moon's geology?

The LLRE has provided valuable information about the Moon's surface, including its topography and its rate of rotation. It has also revealed that the Moon is slowly moving away from the Earth at a rate of 3.8 centimeters per year. This information has helped scientists better understand the Moon's formation and evolution.

4. What are some of the other applications of LLRE?

In addition to studying the Moon's geology, LLRE has also been used to test Einstein's theory of general relativity, to measure the Earth's rotation, and to study the effects of the Earth's atmosphere on the laser beam. It has also been used to calibrate telescopes and other instruments used for space exploration.

5. How has the LLRE evolved over time?

Since its first successful experiment in 1969, the LLRE has evolved and improved with advancements in technology. In the beginning, the laser beams were relatively weak and could only be detected by large, specialized telescopes. Now, more powerful lasers and improved detectors allow for more accurate and frequent measurements. The LLRE is still used today and continues to contribute to our understanding of the Moon and its relationship with Earth.

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