Radiolab Blogland recently posted the piece below titled “Krulwich Wonders: Are Those Spidery Black Things on Mars Dangerous? (Maybe).” Read on!
“You are 200 miles directly above the Martian surface—looking down. This image was taken by the Mars Reconnaissance Orbiter on Jan. 27, 2010. (The color was added later.) What do we see? Well, sand, mostly [an average sand particle is 10-04 meters]. As you scroll down, there’s a ridge crossing through the image, then a plain, then dunes, but keep looking. You will notice, when you get to the dunes, there are little black flecks dotting the ridges, mostly on the sunny side, like sunbathing spiders [10-02 meters in diameter] sitting in rows. Can you see them?
“What are those things? They were first seen in 1998; they don’t look like anything we have here on Earth. [Earth's distance from Mars varies since both planets follow elliptical orbits around the sun. According to Universe Today, the closest recorded approach was in 2003, when Earth and Mars were 56 million, or 10+07 kilometers apart—the closest they’d been in 50,000, or 10+04, years]. To this day, no one is sure what [those spidery things] are, but we now know this: They come, then they go. Every Martian spring, they appear out of nowhere, showing up—70 percent of the time—where they were the year before. They pop up suddenly, sometimes overnight. When winter comes, they vanish. As the sun gets hotter, they get more spidery. . .[The sun's mass is 10+30 kilometers and its core is 27 million or 10+07 degrees Fahrenheit.]
“What could they be? Scientists from the U.S. Geological Survey, from Hungary, from the European Space Agency have all proposed explanations; the leading one is so weird, it’s transformed my idea of what it’s like to be on Mars. For 20 years [10+01], I’ve thought the planet to be magnificently desolate, a dead zone, painted rouge. But imagine this: Every spring, the sun beats down on a southern region of Mars, morning light melts the surface, warms up the ground below, and a thin, underground layer of frozen CO2 [with each molecule averaging 10-10 meters] turns suddenly into a roaring gas, expands, and carrying rock and ice, rushes up through breaks in the rock, exploding into the Martian air. Geysers shoot up in odd places. It feels random, like being surprise attacked by an monstrous, underground fountain. . .
“If you were there,” says Phil Christensen of Arizona State University, “you’d be standing on a slab of carbon dioxide ice. All around you, roaring jets of carbon dioxide gas are throwing sand and dust a couple hundred feet [10+02] into the air.” The ground below would be rumbling. You’d feel it in your space boots.
“That, anyway, is the leading explanation. The spidery traces. . .might be clumps of dark, basaltic sand thrown from the geysers. Or—say a group of Hungarian scientists—they might be colonies of photosynthetic Martian microorganisms, warmed from the sun, now sunbathing in plain view. We still don’t know for sure. We’ve been watching those spider-patches come and go for the last decade or so, and for a little while longer, we will have to guess why they’re there, or what they’re telling us.
“We’ll have to keep looking.”