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The rocks returned from the Apollo 11 and Apollo 12 sites were both dominated by basalt. A key difference between the two sites lies in the abundance of the mineral ilmenite.
Summary[edit]
| Description |
English: The rocks returned from the Apollo 11 and Apollo 12 sites were both dominated by basalt. A key difference between the two sites lies in the abundance of the mineral ilmenite. The elongate black minerals in the Apollo 11 thin section (bottom) are ilmenite [Arizona State University]. |
| Date | |
| Source | https://www.lroc.asu.edu/posts/223 |
| Author | NASA/GSFC/Arizona State University |
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This file is in the public domain in the United States because it was solely created by NASA. NASA copyright policy states that "NASA material is not protected by copyright unless noted". (See Template:PD-USGov, NASA copyright policy page or JPL Image Use Policy.) |  |
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 15:16, 1 September 2023 | | 572 × 818 (1,016 KB) | Don-vip (talk | contribs) | Uploaded a work by NASA/GSFC/Arizona State University from https://www.lroc.asu.edu/posts/223 with UploadWizard |
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