"This is a huge surprise, though maybe it shouldn't have been," says mission principal investigator Steve Squyres (Cornell University). "I never thought we would get to use our instruments on a rock from someplace other than Mars. Think about where an iron meteorite comes from: a destroyed planet or planetesimal that was big enough to differentiate into a metallic core and a rocky mantle."
Heat Shield Rock is unlikely to tell scientists much that they don't already know about meteorites. But project scientist Joy A. Crisp (NASA/Jet Propulsion Laboratory) notes, "There are some other things we might learn about Mars from this meteorite. Any changes in the rock's outer surface might be the result of weathering in the Martian environment. We can also make inferences about the atmospheric conditions that allowed a meteorite of this size and type to make it to the surface."
If Opportunity stumbles across other meteorites (which will probably be the more common stony variety), the numbers will tell scientists about the deposition or erosion rate of Meridiani Planum. If the rover fails to encounter additional meteorites, this will indicate that dust is accumulating in the region, burying meteorites. But if more meteorites are found, it will suggest that dust particles are being blown away by winds, exposing previously buried objects.
Opportunity may have a chance to find more meteorites in about a week, when it leaves its heat shield and heads on a long trek toward a small crater named Vostok located 1.2 kilometers to the south.
On the other side of Mars, Spirit continues to make slow but steady progress climbing Husband Hill inside Gusev Crater.