Phoenix Landing Area With Few Rocks
Researchers assessing the targeted landing area for NASA's Phoenix Mars Lander have used images from a powerful telescopic camera on NASA's Mars Reconnaissance Orbiter to count rocks in and around the intended landing area.
This image from the orbiter's High Resolution Imaging Science Experiment (HiRISE) camera shows ground with very few rocks, close the center of the landing target. It also shows patterned ground, fractured into polygons. Similar polygonal patterns can be found in some areas of repeated freezing and thawing on Earth. The relief of the polygons in this image is highlighted by a low sun angle.
For scale, an illustration of the Phoenix lander, which is about 5.5 meters (18 feet) by 2 meters (7 feet), is artificially superimposed on a full-resolution subset of HiRISE image (right).
HiRISE took this image on Dec. 22, 2006. The full image (most of which is shown on the left) is centered at 68.2 degrees north latitude, 233.6 degrees east longitude. It covers terrain categorized as "lowland bright" by researchers evaluating the landing site. The image is calalogued as HiRISE PSP_001906_2485.
NASA's Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the Mars Reconnaissance Orbiter for NASA's Science Mission Directorate, Washington. Lockheed Martin Space Systems, Denver, is the prime contractor for the project and built the spacecraft. The High Resolution Imaging Science Experiment is operated by the University of Arizona, Tucson, and the instrument was built by Ball Aerospace & Technologies Corp., Boulder, Colo.
The Phoenix Mission is led by the University of Arizona on behalf of NASA. Project management of the mission is by NASA's Jet Propulsion Laboratory. Spacecraft development is by Lockheed Martin Space Systems.
Image Credit: NASA/JPL-Caltech/University of Arizona
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