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| This mosaic of microscopic images includes six types of soil found in Eagle Crater by the rover Opportunity. Each picture covers an area about 0.8 inches by 0.8 inches.
Punaluu has the largest particles. They are similar to those seen in Eagle Crater outcropping of bedrock. There also are smaller, more irregular rounded particles that probably were carried there by the wind.
Lanikai is a finer-grain soil with irregularly shaped, light-colored, 0.04 inch particles. They are more angular and less-rounded the particles elsewhere in the crater.
Neopolitan is a border area between two different types of soil. A lighter, finer-grained particle is on the left, and a darker, coarser-grained particle is on the right.
Cookies and Cream is a mixture of light and dark soil particles in the Neopolitan area. There are several different types of particles held in surrounding fine-grained sands – rounded spheres, angular, irregular fragments with small cavities and smaller 0.04 inch rounded particles.
Vanilla has small grains at 0.04 inch or less in size and somewhat lighter in color than those in other particles observed in Eagle Crater.
Mudpie is representative of soils found lower in the crater, away from the bedrock outcrop. It has spheres and irregularly shaped cavities in a dark sand.
Brian's Choice in the Black Forest area has irregularly shaped particles, which are low in hematite content. according to readings by the rover's miniature thermal emission spectrometer. Presumably, the particles in this area are more affected by winds since they are on the outer part of Eagle Crater. They may have been re-distributed frequently by wind.
Photo by Mars exploration rover Opportunity
image credit: NASA/JPL
click image to enlarge
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