PIA14009: Striated Blocks in Aristarchus Crater
 Target Name:  Moon
 Is a satellite of:  Earth
 Mission:  Lunar Reconnaissance Orbiter (LRO)
 Spacecraft:  Lunar Reconnaissance Orbiter (LRO)
 Instrument:  Lunar Reconnaissance Orbiter Camera (NAC)
Lunar Reconnaissance Orbiter Camera (WAC)
 Product Size:  664 x 664 pixels (w x h)
 Produced By:  Arizona State University
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 Full-Res TIFF:  PIA14009.tif (441.6 kB)
 Full-Res JPEG:  PIA14009.jpg (84.51 kB)

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Original Caption Released with Image:

Field of striated boulders on the wall of Aristarchus crater. Uphill is towards top of image. LROC NAC image M120161915.

Aristarchus crater is located on the edge of the Aristarchus Plateau, one of the most geologically interesting regions of the Moon. It is a 40 kilometers wide, 3.5 kilometers deep, complex impact crater, which probably formed about 175 million years ago. The impact straddled the boundary of the plateau and the surrounding mare, thus excavating both very different rock types, as well as underlying crustal rocks. Previous posts have highlighted features of the Aristarchus Plateau, including Valles Schröteri and the pyroclastic deposits that blanket the plateau. Compositional differences within the central peak of the crater have also been noted, and highlight the importance of studying the geology of this crater.

On the northeastern slopes of Aristarchus, there are numerous large, stratified blocks of ejected material. These blocks are banded with alternating layers of light and dark material. Dark layers are typically less than 1 meter thick, and bright layers range between 1 and 10 meters thick. The boulders are randomly oriented, so they are not in their original position but rather appear to have tumbled down the wall of the crater from above. Unfortunately, no clear layers of rock are observed in the crater wall because it has been covered by impact melt and debris. Luckily, however, some stratified blocks are observed outside of the crater, and would be accessible for any future astronauts to sample.

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WAC mosaic of the 40 kilometers diameter Aristarchus crater. Striated blocks are presently only observed in the northeast portion of the crater

NASA's Goddard Space Flight Center built and manages the mission for the Exploration Systems Mission Directorate at NASA Headquarters in Washington. The Lunar Reconnaissance Orbiter Camera was designed to acquire data for landing site certification and to conduct polar illumination studies and global mapping. Operated by Arizona State University, LROC consists of a pair of narrow-angle cameras (NAC) and a single wide-angle camera (WAC). The mission is expected to return over 70 terabytes of image data.

Image Credit:
NASA/GSFC/Arizona State University

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