[meteorite-list] Early Moon Photos Revealed More Than Was Known

From: Ron Baalke <baalke_at_meteoritecentral.com>
Date: Mon, 14 May 2007 17:34:07 -0700 (PDT)
Message-ID: <200705150034.RAA12439_at_zagami.jpl.nasa.gov>

http://www.space.com/scienceastronomy/070514_moon_images.html

Early Moon Photos Revealed More Than Was Known
By David Powell
space.com
14 May 2007

Newly reprocessed images of the Moon's far side taken by Soviet
spacecraft more than 40 years ago may have confirmed that the Moon's
biggest impact scar was glimpsed far earlier than previously thought.

The images were acquired by the Luna 3 and Zond 3 spacecraft in October
1959 and July 1965 respectively and provided the first look at the
Moon's forever hidden far side.

The original murky and noisy images have now been re-processed by
amateur astronomer Ricardo Nunes and add weight to a proposal by V.V.
Shevchenko and V.I.Chikmachev of the Sternberg State Astronomical
Institute in Moscow that a dark smudge visible on the Moon's limb in
Luna 3 images is part of the western edge of the enormous South
Pole-Aitken Basin (SPAB).

Gargantuan basin

The SPAB is a gargantuan impact basin-1,550 miles (2,500 kilometers)
diameter-that sprawls between the lunar South Pole and the crater
Aitken. The basin is 8 miles (12 kilometers) deep.

Despite its size, over subsequent years only slivers of the basin were
seen in images and it took until 1992 for the SPAB to be seen in its
entirety; courtesy of the Galileo spacecraft while en-route to Jupiter.

Further image processing work by Nunes on images captured by Zond 3
reveal the eastern portion of the SPAB's mountainous outer rings. Those
now-eroded peaks were thrust up 4.1 billion years ago, and the yawning
basin they encircle is an important tool for looking deep into lunar
history.

"The formation of SPAB was a huge event in early lunar history, and its
influence was likely felt all across the Moon," said Lisa Gaddis of the
Astrogeology Program at the U.S. Geological Survey. "Not only is SPAB
the biggest 'hole' in our solar system, but it must have dug down deeply
enough to expose and excavate materials from deep within the Moon."

The Moon's mantle is the region buried more than 62 miles (100
kilometers) below the impact-pummelled outer crust, and only the most
powerful impacts can liberate the well concealed mantle material. It is
still hotly debated how much mantle material resides within the basin,
although high levels of the iron and thorium-thought to be abundant in
the mantle-are present.

Moon rocks

The Apollo missions returned 842 pounds (382 kilograms) of Moon
rock, but none of it was from the mantle.

Scientists would love to study this well-guarded material "It would tell
us a lot about what exists at depth within the Moon," Gaddis says. "It
would also help us to understand how a large impact event behaves, when
the event occurred, how much material might have been thrown out, how
much melted and the composition of the mantle or lower crust."

The SPAB may also harbor some far-flung samples, as Gaddis explains:
"Although it's generally believed that most material currently seen
within SPAB is derived locally, there may be small amounts of 'foreign'
materials in SPAB from other, younger impacts on the Moon. So it's
possible that we'd find compositions that have not yet been sampled on
the Moon. We'd also learn something about the early history of the
Earth/Moon system and how it formed."

Theorists say the Moon was carved from Earth in a spectacular collision
by a Mars-sized object.

Far-side exploration

Researchers now understand the importance of the SPAB, but had the basin
been seen fully in those first far side images, lunar exploration may
have steered a different course.

"It would likely have changed lunar maps and our understanding of the
occurrence and distribution of large impacts on terrestrial planets. It
also might have influenced exploration or at least imaging of the far
side at an earlier time," Gaddis said.

The next time we lay eyes on the SPAB may well be courtesy of NASA's
Lunar Reconnaissance Orbiter (LRO) to be launched in 2008. LRO is
bristling with instrumentation and will provide our best look at the
SPAB, nearly 50 years after it was stumbled upon by Luna 3.

"I think we'll learn a great deal more [from LRO] about the topography
and composition of the SPAB," Gaddis said. "Of course, then we'll want
samples."
Received on Mon 14 May 2007 08:34:07 PM PDT