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Bradbury Landing is a landing location on the planet Mars inside Gale crater. It marks the landing site of Mars Science Laboratory ''Curiosity'' rover on August 6, 2012. The location was named by NASA for Ray Bradbury on August 22, 2012, his 92nd birthday, in honor of the author who died a few months earlier, on June 5. The coordinates of the landing site are: . ==Description== Gale Crater is the MSL landing site.〔〔〔 Within Gale Crater is a mountain, named Aeolis Mons ("Mount Sharp"),〔〔〔 of layered rocks, rising about above the crater floor, that ''Curiosity'' will investigate. The landing site is a smooth region in "Yellowknife" ''Quad 51'' of Aeolis Palus inside the crater in front of the mountain. The target landing site location was an elliptical area .〔 Gale Crater's diameter is . The final landing location for the rover was less than from the center of the planned landing ellipse, after a journey.〔 〕 The landing site contains material washed down from the wall of the crater, which will provide scientists with the opportunity to investigate the rocks that form the bedrock in this area. The landing ellipse also contains a rock type that is very dense, very brightly colored, and unlike any rock type previously investigated on Mars. It may be an ancient playa lake deposit, and it will likely be the mission's first target in checking for the presence of organic molecules.〔 A rock outcrop near the landing site has been named ''"Goulburn"''. This rock outcrop, along with several others further eastward, including ''"Link"'' and ''"Hottah"'', suggest the "vigorous" flow of water in an ancient streambed. An area of top scientific interest for ''Curiosity'' lies at the edge of the landing ellipse and beyond a dark dune field. Here, orbiting instruments have detected signatures of both clay minerals and sulfate salts.〔 Scientists studying Mars have several hypotheses about how these minerals reflect changes in the Martian environment, particularly changes in the amount of water on the surface of Mars. The rover will use its full instrument suite to study these minerals and how they formed. Certain minerals, including the clay and sulfate-rich layers near the bottom of Gale's mountain, are good at latching onto organic compounds—potential biosignatures—and protecting them from oxidation.〔 Two canyons were cut in the mound through the layers containing clay minerals and sulfate salts after deposition of the layers. These canyons expose layers of rock representing tens or hundreds of millions of years of environmental change. ''Curiosity'' may be able to investigate these layers in the canyon closest to the landing ellipse, gaining access to a long history of environmental change on the planet. The canyons also contain sediment that was transported by the water that cut the canyons;〔 this sediment interacted with the water, and the environment at that time may have been habitable. Thus, the rocks deposited at the mouth of the canyon closest to the landing ellipse form the third target in the search for organic molecules. On March 27, 2015, NASA reported the landing site was fading from view in the two-and-a-half years since landing in 2012, as shown in the following animation: 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Bradbury Landing」の詳細全文を読む スポンサード リンク
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