Block Island—a half-ton meteorite found on Mars by NASA’s
Opportunity rover.Image credit, NASA/MER Opportunity
Ever been driving down a lonely desert highway when you suddenly glimpse something in the corner of your eye that makes you think, “What was that?!” You brake, tires screech, you spin the wheel and make a wild U-turn, cutting into the shoulder and leaving a rooster-tail of dust as you floor the gas to get back to what you thought you saw….

Okay, dramatic desert car scene ended. That would be the Hollywood movie version of what NASA’s Mars Exploration Rover Opportunity did recently, on the lonely desert highway that it’s scouting on Mars.

On its determined long trek from Victoria Crater to the larger Endeavour Crater (a 12-mile span that Opportunity has completed about one fifth of over the past year), the rover passed by an X-box-sized block of iron that presented the appearance of a meteorite. It snapped a picture in passing, which was eventually transmitted to Earth and examined. By this time, Opportunity had already traveled about 180 meters beyond the block (dubbed “Block Island”). This is when the rover was commanded to backtrack all the way to the find (though it’s doubtful it worked up a rooster tail).

Upon returning to Block Island—quite obviously an iron-nickel meteorite by appearance alone, but whose composition was confirmed by the rover’s alpha particle X-ray spectrometer instrument—Opportunity took more pictures, including extreme close-ups with its microscope camera, which revealed surface patterns similar to those found on Earth iron-nickel meteorites that have been exposed to long-term weathering by wind and sand.

As interesting as stumbling upon a half-ton meteorite on the dusty plains of Mars’ Meridiani Planum is, what this particular chunk of weathered iron is telling scientists sparks the imagination. In a nutshell, given the thinness of Mars’ current atmosphere, scientists wouldn’t expect a meteorite of this size to survive impact intact, at the speed it would be going. One of the possible explanations for Block Island’s rock-houndable state is that when it fell to Mars, Mars’ atmosphere was substantially thicker than it is now.

Further examination of the meteorite may reveal clues as to how long ago it fell through Martian skies. Evidence that Mars’ atmosphere was warmer and thicker in the distant past, as well as the possibility that there was liquid water on the surface, has been mounting over the years. The age of this meteorite-fall could shed more light on the history of Mars’ environment. If it fell billions of years ago, Block Island would weigh in as more evidence to support our current suspicions. If, however, we find that it fell more recently, then this could indicate that the atmosphere was more substantial later in Mars’ history than we thought.

Imagine, if you will, a Mars that looks even more Earthlike than it does now: seas of water with waves rolling into shorelines, great clouds sending downpours of rain and snow onto mountains and plains, streams and rivers snaking through the landscape. Maybe, maybe, even some form of life?

All that from a rock? Yes, rocks talk, if we listen.

37.8148 -122.178

Mars Rock Talks, Opportunity Listens 12 June,2013Ben Burress

  • sandy lundgren

    Last Thursday on deck Leonard had the meteorite on his iPhone already. Way cool.
    Color scheme of blues and purples noted too, not on his iPhone but Mars Daily likely. Too bad RAT has pooped out.

    Always pleased to see your quest-notes.

  • Tamara

    Cool… what are the ways to find out more about how long ago the meteorite fell?

  • Ben Burress

    One method is to study the condition of the meteorite’s surface for weathering and oxidation. Another way is to analyze the presence of various chemical isotopes that formed when the meteorite was in space and exposed to high energy cosmic rays. By analyzing the proportions of various isotopes, an “exposure time” in space may be estimated. And, by analyzing the proportions of any radioactive isotopes and their decay products, it’s possible to estimate how long the meteorite may have rested on Mars (or Earth), shielded from cosmic rays. This is sort of like a meteorite’s version of radiocarbon dating performed on organic material. I’m not certain if Opportunity has the capability to do much analysis along these line…so am waiting to hear more from the rover….

  • Ben Burress

    One method is to analyze certain isotopes in the meteorite. When a meteorite is in space, it is bombarded by cosmic rays, which form various isotopes–some of them radioactive. Then, after falling to a planet with an atmosphere, the bombardment ends and no more isotopes are created. Amounts of some isotopes can tell about how long the rock was in space, and the amount of certain radioactive isotopes can tell about how long it has been shielded from bombardment. It’s analogous to radiocarbon dating. But, I don’t think Opportunity has the capability to analyze the isotope content….

  • Pingback: Reality Rocks: Prospecting on Mars | QUEST Community Science Blog - KQED()


Ben Burress

Benjamin Burress has been a staff astronomer at Chabot Space & Science Center since July 1999. He graduated from Sonoma State University in 1985 with a bachelor’s degree in physics (and minor in astronomy), after which he signed on for a two-year stint in the Peace Corps, where he taught physics and mathematics in the African nation of Cameroon. From 1989-96 he served on the crew of NASA’s Kuiper Airborne Observatory at Ames Research Center in Mountain View, CA. From 1996-99, he was Head Observer at the Naval Prototype Optical Interferometer program at Lowell Observatory in Flagstaff, AZ.

Read his previous contributions to QUEST, a project dedicated to exploring the Science of Sustainability.

Sponsored by

Become a KQED sponsor