Researchers have discovered that the surface of Mercury is crackled with volcanic explosions for extended periods of the planet's history.
The researchers were surprised by these findings as the planet wasn't supposed to have explosive volcanism in the first place; they have also said that this could have implications for understanding how Mercury formed.
On Earth, volcanic explosions like the one that tore the lid off Mount St. Helens happen because our planet's interior is rich in volatiles-water, carbon dioxide and other compounds with relatively low boiling points. As lava rises from the depths toward the surface, volatiles dissolved within it change phase from liquid to gas, expanding in the process.
The pressure of that expansion can cause the crust above to burst like an overinflated balloon.
Mercury, however, was long thought to be bone dry when it comes to volatiles, and without volatiles there can't be explosive volcanism.
But that view started to change in 2008, after NASA's MESSENGER spacecraft made its first flybys of Mercury. Those glimpses of the surface revealed deposits of pyroclastic ash-the telltale signs of volcanic explosions-peppering the planet's surface. It was a clue that at some point in its history Mercury's interior wasn't as bereft of volatiles as had been assumed.