Category Archives: The Moon

Lunar Orbiter Image Recovery Project – needs a boost to cross the finish line

The Lunar Orbiter Image Recovery Project, underway since 2008, is crowd-funding the completion of the processing of images of the Moon taken by five early unmanned lunar missions and recovered from magnetic tape: Lunar Orbiter Image Recovery Project Last Mile – Indiegogo

Between further NASA funding and $62k raised by crowd funding in 2013 we have completed the process of digitizing almost 1500 tapes, the entire tape library from lunar orbiter.    This has created tens of terabytes of data, and over 1700 images.  Each medium resolution image is broken into 28 strips or framelets.  Each high resolution image is made from 98 framelets.  Each framelet is a file. We have over 107,000 of these files.  

Our task is to complete the processing of these files and publish them to the NASA  website where they will be free for everyone to enjoy.  We are also doing the paperwork to get the raw data and images to the National Space Science Data Center.   We had estimated the cost to NASA to complete this at about $400,000 dollars, of which they provided $300k after we finished the work from the 2013 crowd funded effort.  We originally thought that we were only going to get Lunar Orbiter II and III, but because of our previous crowd funded effort, we were able to leverage the additional $300k.  That puts us at about $100k short of what we needed to finish, and that is what we are asking you, the crowd funding community to help us with.  This gets us our very last mile to finish everything.  To see what we have done so far, here is our gallery at NASA Ames Solar System Exploration Research Virtual Institute web site: sservi.nasa.gov/LOIRP/loirp_gallery/

Estimating the safety of Moon tunnels + The in-space colony concept

A group at Purdue University has released an interesting study of lava tubes on the Moon in which they examined the possibility that there are ones big enough and stable enough to hold cities:

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This diagram illustrates a lava tube protecting a city the size
of Philadelphia. Purdue University/courtesy of David Blair

Lava tubes are

tunnels formed from the lava flow of volcanic eruptions. The edges of the lava cool as it flows to form a pipe-like crust around the flowing river of lava. When the eruption ends and the lava flow stops, the pipe drains leave behind a hollow tunnel, said Jay Melosh, a Purdue University distinguished professor of earth, atmospheric and planetary sciences who is involved in the research.

There is indirect evidence that lava tubes exist on the Moon. A number of large holes, for example, have been seen on the Moon and it is speculated that these could be where the roofs of lava tubes have collapsed. See Lunar and Martian Lava Tube: Exploration as Part of an Overall Scientific Survey, Daga et al. (pdf).

The Purdue study considered the case of really large tubes:

David Blair, a graduate student in Purdue’s Department of Earth, Atmospheric and Planetary Sciences, led the study that examined whether empty lava tubes more than 1 kilometer wide could remain structurally stable on the moon.

“We found that if lunar lava tubes existed with a strong arched shape like those on Earth, they would be stable at sizes up to 5,000 meters, or several miles wide, on the moon,” Blair said. “This wouldn’t be possible on Earth, but gravity is much lower on the moon and lunar rock doesn’t have to withstand the same weathering and erosion. In theory, huge lava tubes – big enough to easily house a city – could be structurally sound on the moon.”

Blair worked with Antonio Bobet, a Purdue professor of civil engineering, and applied known information about lunar rock and the moon’s environment to civil engineering technology used to design tunnels on Earth.

The team found that a lava tube’s stability depended on the width, roof thickness and the stress state of the cooled lava, and the team modeled a range of these variables. The researchers also modeled lava tubes with walls created by lava placed in one thick layer and with lava placed in many thin layers, Blair said.

Personally, rather than on the Moon I would prefer to live in a large, island-sized, in-space habitat like that promoted by the late Princeton physics professor Gerard K. O’Neill . Rotation could provide a full 1 g of spin-gravity, no lunar dust to hassle with and breath, sunlight all around, and there would be a greater sense of freedom of movement. That is, why work so hard to get out of earth’s gravity well just to jump down another one?

Every so often, someone on the web discovers the great space colony artwork from the workshops that studied such structures: How we’ll live in space, according to people in the 1970s – mashable

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Interior including human powered flight. Art work: Rick Guidice.
Image via NASA Ames Research Center.

At the time, such ambitions were believed justified by the big drop in space transportation costs that would come when the Space Shuttle began to fly. The Moon would still be useful – as a source of the materials to build such huge structures. It’s low gravity would allow building materials literally to be thrown into space by mass drivers, i.e. electromagnetic catapults.

Unfortunately, the hyper-complex and fragile Shuttles failed to lower space transport costs at all. The original fully reusable design for the Shuttles was down-graded by budget cuts and the Shuttles became only partially refurbish-able, requiring a standing army of thousands to work for months to return one to flight.

Today we finally are seeing new approaches to reusable space vehicles that intend to achieve full reusability and fast turnaround. We could see the cost of getting to space drop by factors of 100 in the coming decade.

Low cost spaceflight combined with new technologies like 3D printing and advanced robotics will make it affordable to build large scale structures in space.  Today’s space pessimism towards concepts like in-space colonies will give way to taking them granted just as we take granted the giant structures on earth that once would have been considered fantasies.

Lunar flash and plume seen by amateur astronomers

Selenology Today – 2015 (pdf) and Lunar Networks blog report on a flash seen on the Moon by three members – Marco Iten, Raffaello Lena, Stefano Sposetti – of the Geological Lunar Research Group, an Italian group of advanced amateur observers. The flash was apparently produced by a meteoroid impact: Mare Nubium impact with plume captured and analyzed – Lunar Networks –

 

2015_02_26_213522_Iten_blackSee the flash and plume in top right,

Abstract: We report the detection of an interesting luminous event most probably generated by a meteoroidal impact on the lunar surface occurred at 21h 35m 22.871s ± 0.010s UT, the 26 February 2015. The position of the flash was along the terminator at selenographic coordinates 7.9° ± 0.6° W; 26.1° ± 1.6° S. The brightness of the flash 0.16 s after the initial detection was +8.0 magV. After the main lightdrop a successive residual diffuse light lasted for several seconds.

Under the assumption of a meteoroidal impact we argue that this post luminous event and its ever growing dimensions was likely caused by the sunlight reflection on ejected materials released by the impact. Thus, future high resolution orbital data, e.g., from LRO spacecraft (NAC images) could allow the detection of this crater. Because this event was captured only by one observer, we checked for satellite glints and evaluated the likelihood of a meteor hitting head on our atmosphere.

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This map shows the location of the flash at Mare Nubium:

VMA-Lippershey_P-200

Video: Watching the Moon’s phases from the other side

Here are some cool videos showing the far side of the Moon using time-lapse imagery from the Lunar Reconnaissance Orbiter :

Moon Phase and Libration, from the Other Side

A number of people who’ve seen the annual lunar phase and libration videos have asked what the other side of the Moon looks like, the side that can’t be seen from the Earth. This video answers that question.

Just like the near side, the far side goes through a complete cycle of phases. But the terrain of the far side is quite different. It lacks the large dark spots, called maria, that make up the familiar Man in the Moon on the near side. Instead, craters of all sizes crowd together over the entire far side. The far side is also home to one of the largest and oldest impact features in the solar system, the South Pole-Aitken basin, visible here as a slightly darker bruise covering the bottom third of the disk.

The far side was first seen in a handful of grainy images returned by the Soviet Luna 3 probe, which swung around the Moon in October, 1959. Lunar Reconnaissance Orbiter was launched fifty years later, and since then it has returned hundreds of terabytes of data, allowing LRO scientists to create extremely detailed and accurate maps of the far side. Those maps were used to create the imagery seen here.

A virtual telescopic view of the Moon from its far side, with the
Earth looming in the background. The camera is fixed to
the Earth-Moon line.

 

A view from the Moon’s far side, using a short focal length that
makes the distant Earth look small. The camera is fixed
to the Moon’s surface.

Video: TMRO 8.04 – Google Lunar X PRIZE

The latest TMRO program is now available: Google Lunar XPRIZE – TM –

We are joined by Leo Camacho and Nathan Wong of the XPRIZE Foundation to talk about the latest happenings with their Google Lunar XPRIZE Contest.