原始大圖：月球勘測軌道器（LRO）拍攝的嫦娥五號着陸器_風聞
鹰击长空-黑名单专治乌贼、反智、喷子、谣棍和杠精2020-12-06 14:12
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Box indicates Chang’e 5 lander on the basaltic plains of Oceanus Procellarum (“Ocean of Storms”) on 02 December 2020 09:54 EST (14:53:55 UTC). The lander is the bright spot in the center of the outline. Outline is 1210 meters wide; north is up. LROC NAC M1361560086R [NASA/GSFC/Arizona State University].
大意為：方框所指示區域為2020年12月2日美東時間 0954 時拍攝的（世界協調時 14:53:55）嫦娥五號風暴海洋地區着陸。整個拍攝區域區域大小為 1210 米寬，圖像編號 LROC NAC M13615600086R（美國航天總署、全球空間科學基金會和亞利桑那州立大學發佈）
China’s Chang’e 5 sample return spacecraft made a safe touchdown on the lunar surface at 10:11 EST (15:11 UTC) 01 December 2020. LRO passed over the site the following day and acquired an off-nadir (13° slew) image showing the lander centered within a triangle of craters.
The LROC team computed the coordinates of the lander to be 43.0576° N, 308.0839°E, –2570 m elevation, with an estimated accuracy of plus-or-minus 20 meters.
大意為：嫦娥五號採樣返回器於美東時間 2020 年 12 月 1 日 1011 時（世界協調時 1511 時）在月球成功着陸。在着陸後的第二天，LRO（月球勘探軌道器）飛躍了着陸區並獲得了一張偏角為 13°的圖像，可以看到着陸器位於一個有隕石坑組成的三角形區域內。
LROC（LRO上的相機）小組計算出了着陸區座標位於 北緯 43.0576°，東經 308.0839°，月面高度為 -2570 米。精度誤差正負 20 米。
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LROC Wide Angle Camera context mosaic; Chang’e 5 landed in the center of the white box. The “channel” winding across the upper right (rille) was formed by an eruption of basaltic lava more than a billion years ago. The bright area to the south is a massif of older terrain protruding through the mare basalts. North is up, entire image is 61 kilometers wide [NASA/GSFC/Arizona State University].
大意：由 LROC 的廣角相機圖像組合得到的着陸區廣域地標圖：嫦娥五號位於中央白色方框內。周圍有大量的“通道”是十億年前玄武岩物質熔岩形成的。南部高亮地區為一個古老的玄武岩地表凸出的物質。整個圖像寬度為 61 公里。
The local geology consists of a broad, flat mare basalt unit. Similar to flood basalts on the Earth, this deposit was the result of a massive outpouring of very fluid, basaltic lavas. In the lunar case, this massive eruption occurred somewhere between one and two billion years ago. Chang’e 5 is now in the process of returning a small sample of this volcanic unit to Earth so that scientists can precisely determine its age and its chemistry.
大意：科學家認為這樣的玄武岩地形類似地球，由大量熔岩湧出構成，是約十億年至二十億年前月表活動的結果，嫦娥五號會將此處月球火山的樣本送回地球，以便科學家可以精確的分析他們的年齡和成分。
網站還包括了之前拍攝的嫦娥四號等着陸器的衞星照片。
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來源：http://lroc.sese.asu.edu/posts/1172