National Aeronautics and Space Administration

Biographical details

National Aeronautics and Space Administration MER press briefing, March 3, 2004

You're about to hear that Opportunity has landed in an area of Mars where liquid water drenched the surface and was around for a habitable time. Today's results are a giant leap.
Steve Squyres: Ever since Opportunity touched down on Jan 24 we saw this marvelous outcrop right in front of us we've been trying to puzzle out what it has to tell us. For the last two weeks we've been attacking it with everything we have. Every piece of our payload have been used. Over the last couple of weeks the puzzle pieces were falling into place. We've concluded that these rocks were soaked in liquid water.
Source: Wikisource

National Aeronautics and Space Administration MER press briefing, February 12…

Seeing warm and cold blobs passing over the rover down near the surface. We think that the ground is warming, transmitting heat to atmosphere, warm rises and goes up to 100 meters and gives its heat up to the rest of the atmosphere and then there's a cold blob that comes down. You're watching the boiling of the atmosphere. It's really convection. This is really exciting data that will allow us to much better constrain the models that were used to understand the winds that were a danger at the landing sites.
Source: Wikisource

National Aeronautics and Space Administration MER press briefing, February 9…

You can see the layers, inherently very, very fine-grained sitting there for millions of years being sandblasted. This stuff sits there, the wind blows, these grains are striking and eroding the softer portions developing this intricate texture telling you how well indurated the rock is. Then embedded in the stuff are the little spherules. Those seem to be pretty tough. So what happens is that the rock erodes away as it gets sandblasted and the little blueberries drop out and roll down the slope where we take pictures of them. There's one in the process of being eroded out.
Source: Wikisource

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