September 19, 2012
Mercury MESSENGER Finds The Planet Is Truly Of Different Origins
Lee Rannals for redOrbit.com - Your Universe Online
MESSENGER's X-ray spectrometer shows a planet whose northern volcanic plains formed through upwellings of rocks that are also unique to Mercury.
The older terrain on Mercury has higher ratios of magnesium to silicon, sulfur to silicon, and calcium to silicon, but lower ratios of aluminum to silicon.
The latest data consists of 205 measurements of the surface composition from the X-ray spectrometer, which focuses on the large expanse of smooth volcanic plains at high northern latitudes and surrounding areas that are higher in crater density and older than the northern plains.
The researchers published their findings recently in the Journal of Geophysical Research.
The Planetary Data System (PDS) released data collected during MESSENGER's seventh through twelfth month orbit around Mercury back in early September. This release made images and measurements of Mercury available to the public.
MESSENGER first reached Mercury in March 2011, and it is only the second spacecraft to reach the planet and orbit it.
Mercury is about 5 percent the size of Earth, and it revolves around the sun every 88 days. The planet has a surface temperature that reaches up to 800 degrees Fahrenheit.