We have been seeing lots of small light-colored veins crossing through the outcrops here on Matijevic Hill, and we have tried to get a handle on the composition of these veins by doing multiple offsets with the APXS. It appears that the small veins are calcium sulfate, as best we can determine. In other words, they are probably gypsum like the large veins that we saw around the margins of Cape York. Here are exmples of some of theseback in the Ortiz outcrop. They are tiny, measuring at a millimeter or two in width. But they are everywhere.
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Rover Field Reports from Mars
Status Reports for MER Opportunity Rover at Endeavour Crater, Meridiani Planum
L. Crumpler, MER Science Team & New Mexico Museum of Natural History & Science
The Mars Exploration Rover Opportunity is still exploring Mars. Below is a brief field report summary of its latest activity.
Opportunity is continuing its drive down Persevereance Valley, a channel that was cut in the inner wall of the 22 km-diameter Endeavour impact crater in ancient Mars (Noachian) time. This is the second stop of a series of stops as Opportunity drives down the valley. The goal is to collect field data that will help assess the origin of the valley. While the valley looks like a water-cut valley, we cannot be sure whether other processes like wind or drive flow have cut the valley. But that is why we are taking our time and collecting data as we drive.