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The Planetary Society BlogBy Emily LakdawallaPhobos: New gravity data and an update on the Phobos-Grunt landing siteOct. 16, 2008 | 11:13 PDT | 18:13 UTC
ESA issued a press release today announcing that Mars' moon Phobos is a rubble pile because it has an anomalously low density, measured during a recent flyby by Mars Express. As far as I can tell from a bit of Googling, both the fact that it's likely a rubble pile and the low density were already known, though the Mars Express measurement is supposedly more precise than previous ones. They report the mass of Phobos to be 1.072 x 1016 grams (that's 10.72 million million kilograms, in case my superscript isn't working); dividing the mass by its volume gives you a density of 1.8 grams per cubic centimeter. For reference, ice has a density just under one gram per cubic centimeter; the rocks that make up the bulk of Mars' and Earth's crust are denser, at 2.7 to 3.3 or more grams per cubic centimeter. A density of 1.8 is common for icy moons in the outer solar system, but it's pretty low for a body which shouldn't contain any ice, so Phobos likely has a lot of open pore space, and is therefore a rubble pile and not a single chunk of rock. Another line of evidence tells you it's a rubble pile, and that's the size of its giant crater, Stickney; for an impact that large to have produced just a crater and not blasted the moon to smithereens, Phobos has to be a mostly cohesionless rubble pile. There's a nice explanation of that on Bill Bottke's web page.
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