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Moon News
Window onto an abyss: Cave skylight on the Moon
Researchers on JAXA's Kaguya lunar orbiter have discovered an open pit on the Moon that is likely a window onto a sublunar world -- a skylight into a subsurface cavern. Junichi Haruyama, Kazuyuki Hioki, Motomaro Shirao, Tomokatsu Morota, Harald Hiesinger, Carolyn van der Bogert, Hideaki Miyamoto, Akira Iwasaki, Yasuhiro Yokots, Makiko Ohtake, Tsuneo Matsunaga, Seiichi Hara, Shunsuke Nakanotani, and Carlé Pieters describe the feature in a paper now in press in Geophysical Research Letters: "Possible lunar lava tube skylight observed by SELENE cameras."
A probable cave skylight on the Moon
This dark hole, 65 meters in diameter, may be a window onto a subsurface cavern on the Moon. It was photographed by the Kaguya Terrain Camera on May 20, 2008, in a photo of the Marius Hills region of the lunar nearside. Credit: ISAS / JAXA / Junichi Haruyama et al.
First, some context. The Moon will be a difficult, but not impossible, place to set up a permanent human outpost. Lacking a protective atmosphere, its surface is bathed in punishing solar radiation, not to mention a continuous rain of micrometeorites; and over the course of a lunar day (that is, about a month) its temperature ranges over more than 200 degrees Celsius (more than 450 degrees Fahrenheit). Many workers imagining future human habitation of the Moon have advanced the idea of setting up the colony inside a shelter that would provide some protection from the hazards of space radiation and the challenge of insulating against such extremes of temperature.
Digging such a shelter would be a major engineering project; we could get a head start on things if we could find a natural cave. The Moon doesn't have Earth-type limestone rocks bathed in acidic subsurface water, but there is another type of environment that might produce underground caverns: hollow lava tubes. The Moon once had active volcanic geology that has left its surface carved by numerous "sinuous rilles", some of which may once have been underground lava tubes like the ones that form on the flanks of Kilauea today. But while there are lots of rilles to be seen on the Moon, no one has ever confirmed the presence of an enclosed tube, with an intact roof, that could be used as a shelter. One study did find several possible locations where there were likely intact tubes present next to collapsed tube sections (link takes you to a 1.4 MB PDF of a paper by Cassandra Coombs and Ray Hawke), but could not confirm the presence of intact tubes. There are probably lots of intact tubes, but how to find where they're hidden?
The answer is to look for skylights, black holes in the lunar surface that are openings onto sublunar caverns. Skylights are common on Earth, and they've even been seen on the flanks of Martian volcanoes. But despite decades of searching, no one has ever discovered a lunar skylight.
Until now. Haruyama and his coauthors examined Kaguya Terrain Camera photos of an area on the Moon that is populated by numerous rilles, the volcanic complex of the Marius Hills on the lunar nearside. And their search was rewarded with the discovery of exactly one black hole too deep to be an impact crater. The hole is located at 303.3°E and 14.2°N and is, suggetively, in the middle of a small rille. It is nearly circular, 65 meters in diameter, and is equidistant from the rille walls, 250 meters on either side. Previous missions did not image it at high enough resolution to allow scientists to distinguish it from a small impact crater.
Kaguya imaged it nine times, five with the Terrain Camera and four with the lower-resolution Multi-band Imager, at a wide variety of solar incidence angles and camera look angles. A little trigonometry allowed Haruyama et al. to determine that the hole is 80 to 88 meters deep, with very steep walls. The fact that it's deeper than it is wide means it's definitely not an impact crater. But is it a cave skylight? Its location in the dead center of a rille is suggestive, but volcanic environments have a couple of other ways to make pits, such as volcanic vents. But Haruyama et al. determined that a skylight into an underground lava tube is the most likely explanation for this feature; moreover, they figured out that the cavern should be at least 370 meters wide. That's quite a lot of space to work with!
The team searched for more skylights in the region, but only found this one, and as far as they know, it's the only one anybody has ever spotted on the Moon. They concluded: "This is a potentially important discovery for both studies of lunar volcanology and future human outposts....the Marius Hills region has long been considered an important and accessible exploration target, both scientifically and technically. Indeed, the discovery of the Marius Hills Hole further supports the importance of the Marius Hills region as a future exploration target."
This hole is probably not the place we'd establish a permanent base. I imagine that a place that requires a vertical descent and ascent wouldn't be optimal. You'd probably really want one that you could drive into -- an intact tube next to a collapsed part, like the possible ones identified by Coombs and Hawke, and probably ideally with a north- or south-facing opening so it wouldn't get blasted by sunlight at either end of the lunar day. I'm smiling now, because I'm thinking about how far humans have come as a species: we're beginning to expand into space, but we're still doing what our forebears did hundreds of thousands (or more) years ago, looking for a nice cave to establish our hearth in.
Lunar Orbiter IV image 157-H2: Marius Hills; location of cave skylight
The Marius Hills are a complex of volcanic domes and flows located to the south of Oceanus Procellarum, on the west side of the lunar nearside. This image is centered at 13.36°N/56.27°W and includes part of the flat Oceanus Procellarium (top) and the Marius Hills (center). Numerous sinuous rilles flow from the Marius Hills to the west. The most prominent rille, at the left edge below center, is Rima Galilei. The white rectangle outlines a region observed by the Kaguya terrain camera to contain what is likely an intact cave skylight. Credit: NASA
Kaguya captured this photo of n unnamed rille within the Marius Hills region of the Moon on May 20, 2008. The pixel scale is about 10.8 meters. The rille's topography is very subdued; it has likely been partially filled with lava from a later flow since it originally formed. Credit: ISAS / JAXA / Junichi Haruyama et al.
Thurston lava tube is located on Kilauea. When lava flows out onto the surface, it cools on top and may form a solid roof. The roof insulates the still-liquid lava below it, allowing it to continue to flow. Lava may flow through tubes like these for many kilometers. At the end of the eruption, the lava can drain completely out of the tube, leaving a hollow remnant of the flow that forms an underground cavern. This lava tube is about 3 meters in height. Credit: P. Mouginis-Mark, LPI
COURTESY-http://www.planetary.org/home/
Window onto an abyss: Cave skylight on the Moon
Researchers on JAXA's Kaguya lunar orbiter have discovered an open pit on the Moon that is likely a window onto a sublunar world -- a skylight into a subsurface cavern. Junichi Haruyama, Kazuyuki Hioki, Motomaro Shirao, Tomokatsu Morota, Harald Hiesinger, Carolyn van der Bogert, Hideaki Miyamoto, Akira Iwasaki, Yasuhiro Yokots, Makiko Ohtake, Tsuneo Matsunaga, Seiichi Hara, Shunsuke Nakanotani, and Carlé Pieters describe the feature in a paper now in press in Geophysical Research Letters: "Possible lunar lava tube skylight observed by SELENE cameras."
A probable cave skylight on the Moon

This dark hole, 65 meters in diameter, may be a window onto a subsurface cavern on the Moon. It was photographed by the Kaguya Terrain Camera on May 20, 2008, in a photo of the Marius Hills region of the lunar nearside. Credit: ISAS / JAXA / Junichi Haruyama et al.
First, some context. The Moon will be a difficult, but not impossible, place to set up a permanent human outpost. Lacking a protective atmosphere, its surface is bathed in punishing solar radiation, not to mention a continuous rain of micrometeorites; and over the course of a lunar day (that is, about a month) its temperature ranges over more than 200 degrees Celsius (more than 450 degrees Fahrenheit). Many workers imagining future human habitation of the Moon have advanced the idea of setting up the colony inside a shelter that would provide some protection from the hazards of space radiation and the challenge of insulating against such extremes of temperature.
Digging such a shelter would be a major engineering project; we could get a head start on things if we could find a natural cave. The Moon doesn't have Earth-type limestone rocks bathed in acidic subsurface water, but there is another type of environment that might produce underground caverns: hollow lava tubes. The Moon once had active volcanic geology that has left its surface carved by numerous "sinuous rilles", some of which may once have been underground lava tubes like the ones that form on the flanks of Kilauea today. But while there are lots of rilles to be seen on the Moon, no one has ever confirmed the presence of an enclosed tube, with an intact roof, that could be used as a shelter. One study did find several possible locations where there were likely intact tubes present next to collapsed tube sections (link takes you to a 1.4 MB PDF of a paper by Cassandra Coombs and Ray Hawke), but could not confirm the presence of intact tubes. There are probably lots of intact tubes, but how to find where they're hidden?
The answer is to look for skylights, black holes in the lunar surface that are openings onto sublunar caverns. Skylights are common on Earth, and they've even been seen on the flanks of Martian volcanoes. But despite decades of searching, no one has ever discovered a lunar skylight.
Until now. Haruyama and his coauthors examined Kaguya Terrain Camera photos of an area on the Moon that is populated by numerous rilles, the volcanic complex of the Marius Hills on the lunar nearside. And their search was rewarded with the discovery of exactly one black hole too deep to be an impact crater. The hole is located at 303.3°E and 14.2°N and is, suggetively, in the middle of a small rille. It is nearly circular, 65 meters in diameter, and is equidistant from the rille walls, 250 meters on either side. Previous missions did not image it at high enough resolution to allow scientists to distinguish it from a small impact crater.
Kaguya imaged it nine times, five with the Terrain Camera and four with the lower-resolution Multi-band Imager, at a wide variety of solar incidence angles and camera look angles. A little trigonometry allowed Haruyama et al. to determine that the hole is 80 to 88 meters deep, with very steep walls. The fact that it's deeper than it is wide means it's definitely not an impact crater. But is it a cave skylight? Its location in the dead center of a rille is suggestive, but volcanic environments have a couple of other ways to make pits, such as volcanic vents. But Haruyama et al. determined that a skylight into an underground lava tube is the most likely explanation for this feature; moreover, they figured out that the cavern should be at least 370 meters wide. That's quite a lot of space to work with!
The team searched for more skylights in the region, but only found this one, and as far as they know, it's the only one anybody has ever spotted on the Moon. They concluded: "This is a potentially important discovery for both studies of lunar volcanology and future human outposts....the Marius Hills region has long been considered an important and accessible exploration target, both scientifically and technically. Indeed, the discovery of the Marius Hills Hole further supports the importance of the Marius Hills region as a future exploration target."
This hole is probably not the place we'd establish a permanent base. I imagine that a place that requires a vertical descent and ascent wouldn't be optimal. You'd probably really want one that you could drive into -- an intact tube next to a collapsed part, like the possible ones identified by Coombs and Hawke, and probably ideally with a north- or south-facing opening so it wouldn't get blasted by sunlight at either end of the lunar day. I'm smiling now, because I'm thinking about how far humans have come as a species: we're beginning to expand into space, but we're still doing what our forebears did hundreds of thousands (or more) years ago, looking for a nice cave to establish our hearth in.


Lunar Orbiter IV image 157-H2: Marius Hills; location of cave skylight
The Marius Hills are a complex of volcanic domes and flows located to the south of Oceanus Procellarum, on the west side of the lunar nearside. This image is centered at 13.36°N/56.27°W and includes part of the flat Oceanus Procellarium (top) and the Marius Hills (center). Numerous sinuous rilles flow from the Marius Hills to the west. The most prominent rille, at the left edge below center, is Rima Galilei. The white rectangle outlines a region observed by the Kaguya terrain camera to contain what is likely an intact cave skylight. Credit: NASA

Kaguya captured this photo of n unnamed rille within the Marius Hills region of the Moon on May 20, 2008. The pixel scale is about 10.8 meters. The rille's topography is very subdued; it has likely been partially filled with lava from a later flow since it originally formed. Credit: ISAS / JAXA / Junichi Haruyama et al.

Thurston lava tube is located on Kilauea. When lava flows out onto the surface, it cools on top and may form a solid roof. The roof insulates the still-liquid lava below it, allowing it to continue to flow. Lava may flow through tubes like these for many kilometers. At the end of the eruption, the lava can drain completely out of the tube, leaving a hollow remnant of the flow that forms an underground cavern. This lava tube is about 3 meters in height. Credit: P. Mouginis-Mark, LPI
COURTESY-http://www.planetary.org/home/