Origin of the Moon

The origin of the Moon is usually explained by a Mars-sized body striking the Earth, making a debris ring that eventually collected into a single natural satellite, the Moon, but there are a number of variations on this giant-impact hypothesis, as well as alternate explanations, and research into how the Moon came to be continues.[1][2] Other proposed scenarios include captured body, fission, formed together (condensation theory, Synestia), planetesimal collisions (formed from asteroid-like bodies), and collision theories.[3]

The standard giant-impact hypothesis suggests the Mars-sized body, called Theia, impacted Earth, creating a large debris ring around Earth, which then accreted to form the Moon. This collision also resulted in the 23.5° tilted axis of the earth, thus causing the seasons.[1] The Moon’s oxygen isotopic ratios seem to be essentially identical to Earth’s.[4] Oxygen isotopic ratios, which may be measured very precisely, yield a unique and distinct signature for each solar system body.[5] If Theia had been a separate protoplanet, it probably would have had a different oxygen isotopic signature from Earth, as would the ejected mixed material.[6] Also, the Moon’s titanium isotope ratio (50Ti/47Ti) appears so close to the Earth’s (within 4 ppm) that little if any of the colliding body’s mass could likely have been part of the Moon.[7]

When and How Did the Moon Form?

New studies offer contrasting scenarios for making the Moon. One argues for a one big splat early in solar-system history; a second envisions a score of lesser blows that built up the Moon over time; and a third suggests water was involved.

Given the trove of lunar samples in hand and the power of modern laboratory analyses, you’d think that by now geochemists should have completely nailed exactly how the Moon formed. But not so — in fact, there’s still lots of debate on how Earth formed.

Artwork of a Mars-sized object colliding into the Earth early in solar system history. Many planetary scientists believe that an impact such as this threw off the debris which eventually formed the Moon.
Lynette Cook / Getty Images

Here’s the basic problem: about 30 years ago, dynamicists showed that a body roughly the mass of Mars could have struck Earth a glancing blow and ejected enough debris into orbit to collect into a Moon-size object. In virtually all of those simulations, most of what ends up in the Moon came from the impactor rather than from Earth.

 

Throwing Water on the Problem

As if the How and When of the Moon’s formation weren’t complicated enough, a third new analysis argues that — despite its extreme dryness today — the Moon likely contained a lotof water when it formed. In the same issue of Nature Geoscience, Yanhao Lin (Vrije Universiteit Amsterdam) and three others describe their experimental attempts to mimic how the Moon’s magma ocean solidified. Lower density minerals would have floated to the top, forming a crust.

They find that the suite of minerals found in the lunar crust today — combined with its thickness — argue that water was part of the mix at a concentration of 270 to 1,650 ppm. This might not seem like much — but if proven true there’d be significant implications.

“A wet start of the Moon, coupled with the strong similarities between the composition of the Moon and the composition of the silicate Earth,” Lin’s team concludes, “suggests that equally high concentrations of water were present in the Earth at the time of the Moon-forming event.”

Clarinet & Clarinet Music: Feels So Good (Featuring Clarinet, Clarinet Solo and Clarinet Music)

Clarinet and clarinet music – ‘Feels So Good’. Featuring 1 hour of delightful clarinet, clarinet solo and clarinet music

This original clarinet music album is composed and recorded by Australian musician David Lewis Luong. Download this album here: http://www.reverbnation.com/davidlewi…

David LewisLuong is a member of the ‘Music for Good’ charity program on Reverbnation. For every song you buy from David’s Reberbnation site (http://www.reverbnation.com/lewisluong), 50% of the money you spend on his songs will be donated to a charity organisation. Please refer to this link for more information on how your music purchases can help: https://tinyurl.com/Music4GoodFeatured in this video are:

Track 1: Joy of spring (starts at 00:00)
Track 2: A dog’s life (starts at 2:50)
Track 3: All of me (starts at 7:40)
Track 4: My Valentine (starts at 10:21)
Track 5: Walking hand in hand (starts at 16:35)
Track 6: Under the tranquil moon (starts at 22:12)
Track 7: Feels so good (starts at 28:55)
Track 8: Sweet Alabama (starts at 39:35)
Track 9: One step at a time (starts at 42:48)
Track 10: Summer delights (starts at 46:29)
Track 11: Jolly great time (starts at 51:16)
Track 12: The wild wild west (starts at 54:56)
Track 13: Only you (starts at 56:45)

 

Spotify: http://tinyurl.com/gpknd2x