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Ever since Pluto got voted off the island, most astronomers have defined a planet as a body orbiting a star—dead or alive—that is a) massive enough to be rounded by its own gravity, b) not massive enough to ignite itself into starhood, and c) domineering enough to have swept its neighborhood clean of smaller planetary seedlings.

Phew, what a mouthful!

But as we know from our own solar system, not all planets are created equal, and things get really interesting when we try to define the types of planets that might support life.

Traditionally when we think of a habitable world, we think of Earth. Makes sense: To date it's our only frame of reference for a planet that supports plants, animals, even microbes. So it's as good a model as any in terms of what we'd want habitable exoplanets to look like.

kilimanjaro.jpg

A 3-D view of Mount Kilimanjaro in Tanzania, compiled from satellite data
—Image courtesy NASA/JPL/NIMA

Hence the huge emphasis among planet hunters on the so-called Goldilocks Zone, where it's not too hot and not too cold. A planet inside this zone would be just right for liquid water and life-giving sunshine.

In recent years that hypothetical zone has been getting bigger, it seems, especially as expeditions to the deep ocean and volcanic peaks have expanded the conditions in which we thought life could exist.

Enter Rory Barnes, a University of Washington postdoctoral researcher who's here to rain on that parade.

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It's tiny, it's pockmarked, and it's got almost no atmosphere. So it's probably small wonder that we cared so little for poor Mercury that we couldn't be bothered to check out a whole half of the planet until 2008.

mercury-global-color.jpg

—Image courtesy NASA/Johns Hopkins University Applied Physics Laboratory/Arizona State University/Carnegie Institute of Washington

But when we did send a probe to scope out the scene, boy did we find some doozies!

Last October the MESSENGER probe had its second sweep past the planet as it settles into an eventual orbit. Not to waste the opportunity, scientists programed the craft to collect all kinds of data during the brief flyby.

The latest issue of Science describes a whole slew of neat findings from the October visit, including:


I personally loved the magnetic twisters, which I found cool enough to assign as a news story that was deftly reported by our own Rebecca Carroll.

But that last one is also pretty impressive.

As impact basins go, the newly named Rembrandt is a sizable feature—430 miles (700 kilometers) wide, or big enough to stretch from D.C. to Boston if it was on Earth.

rembrandt-basin-earth.jpg

—Image courtesy NASA/Johns Hopkins University Applied Physics Laboratory/Carnegie Institution of Washington/Smithsonian Institution Copyright: Smithsonian Institution

For something so large, it really surprised the research team to find that the floor of the basin has remained largely unchanged for 3.9 billion years.

"This is the first time we have seen terrain exposed on the floor of an impact basin on Mercury that is preserved from when it formed," the Smithsonian's Thomas Watters said in a statement. "Terrain like this is usually completely buried by volcanic flows."

Being almost bare-bottomed means that researchers can see the patterns of ridges and troughs criss-crossing the basin floor, including evidence of a thrust fault that would rival the San Andreas in California.

"The pattern of tectonic landforms in the Rembrandt basin is truly extraordinary," Watters said. "It is unlike anything we have seen before in other impact basins on Mercury, the Moon or Mars, or in basins formed on the icy moons of the outer planets."

Mars Volcanoes' Watery Tales

Posted on March 5, 2009 | 0 Comments

Is it mold on a bathroom wall? A close-up of a Dalmatian? The results of a tragic toner-cartridge accident?

mars-volcano-frost.jpg

—Image courtesy NASA/JPL/University of Arizona

In fact, it's a Martian volcano in the process of defrosting. The ancient cauldron is part of a group of volcanoes that rings the Hellas impact basin on the red planet's southern hemisphere.

The imaging team with the recently reactivated Mars Reconnaissance Orbiter released the picture this week. Taken in January, the shot shows the volcano covered in frost, except for a few dark patches where the icy sheath is starting to melt away.

Researchers aren't sure why the patchy areas are so special, although they suggest that the spots could be dark sand dunes that soak up the sun's heat better than the surrounding soil.

This particular volcano is a patera, a type of volcanic crater where lava once erupted from vents inside the depression. Research has suggested that some of Mars's paterae could be the tops of shield volcanoes—gently sloping peaks like Hawaii's Mauna Loa—that got buried by later lava flows.

Others could have formed when groundwater mixed with magma, triggering an explosion that created the signature scalloped bowl shape.

Today Mars's volcanoes are no longer active, so it's hard to get a clear picture of how they formed. Some of the youngest known lava flows are anywhere from 20 million to 200 million years old.

Olympus Mons, the solar system's biggest volcano, appears to be a shield volcano, but it has an odd asymmetrical shape that geologists can't quite account for.

olympus-mons-photo.jpg

In a new study released this week, geophysicists used a computer model to see how Olympus might have formed.

What they found is that a bed of clay sediments would have been needed to reduce friction as the lava spread out, creating the lopsided shield. And those clays needed water to form.

—Image courtesy NASA

Evidence for water-requiring minerals on Mars is kinda old news at this point. But the new study is making waves because it also offers the tantalizing hint that liquid water—a key ingredient for life—could still be lurking underneath the massive volcano.

"This deep reservoir, warmed by geothermal gradients and magmatic heat and protected from adverse surface conditions, would be a favored environment for the development and maintenance of thermophilic organisms," the study authors conclude in last month's issue of the journal Geology.

In other words, if there's still heat under the mountain's skirts, Martian life could be hiding in its belly.

Those sneaky folks at Google. Even as waves of coverage come pouring forth about the newly launched oceans layer in Google Earth, a short NASA press release and no more than a few lines in a couple news articles note that, oh, yeah, and by the way, there's a new 3-D Mars layer too.

Wha?!?!?

Sure enough, it's in the new Google Earth version 5.0, and It's beautimous. Just launch Earth, click the top tab with the Saturn-looking icon on it, and toggle between Earth, Sky, and Mars.

google-mars-full.jpg

—Google Earth, Mars layer screenshot

[Google Sky, btw, was launched in 2007 and features a ridonkulous amount of astronomy data, from pretty pictures to current and historical sky charts. Fun.]

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HiRISE Spies a Young Martian Crater

Posted on January 23, 2009 | 0 Comments

By now folks used to reading about Mars have gotten pretty spoiled by the amazing images from the High Resolution Imaging Science Experiment (HiRISE) aboard the Mars Reconnaissance Orbiter.

This fabulous camera came online in 2006 and returned its first color images of Mars in 2007.

The current catalog of more than 8,700 images is a study in how science can become art—rippling sand dunes and scalloped craters in gentle hues of blue and red can look more like exhibits at the MoMA than data on planetary geology.

So at first blush it can be a bit of a downer when a HiRISE image looks like this:

mars-young-crater.jpg

—Image courtesy NASA/JPL/University of Arizona

But hey, this is a science experiment, and this contrasty crater is just busting with science.

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About This Blog

The moon
From dwarf planets to hot Jupiters, join NatGeo News space and tech editor Victoria Jaggard in a global discussion about all things extraterrestrial.


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