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Mare Insularum, bordered by the craters Copernicus on the east, and Kepler on the west. Oceanus Procellarum joins the mare to the southwest. The northern edge of Mare Cognitum is visible at the bottom of the photo, and Fra Mauro is the grey patch in the lower right.
Mare Insularum, bordered by the craters Copernicus on the east, and Kepler on the west. Oceanus Procellarum joins the mare to the southwest. The north
Imbrian
Lunar olivine basalt formed around 3.3 billion years ago. This is part of sample 15555, known as Great Scott.
Lunar olivine basalt formed around 3.3 billion years ago. This is part of sample 15555, known as Great Scott.