The crater Seleucus, 42 km in diameter, is shown in sunrise along the right (west) edge of the frame. The narrowness of its rim and the abrupt contact between its raised rim and the surrounding mare prove that the final mare flooding occurred after the crater was formed. In other words, the crater predates at least the youngest mare basalts in this area.
日期
created 2014, original 1971
来源
Apollo 15 Mapping camera image cropped in Gimp. The original image is in the public domain because it is a work of the U.S. Government (NASA).
Immediate source: Lunar and Planetary Institute, Apollo Image Atlas Mapping Camera Image Catalog, Apollo 15, AS15-M-2621
{{Information |Description = Oblique view of [[Seleucus (crater)]], on the moon, while it was at the morning terminator. Facing south. |Source = [[Apollo 15]] Mapping camera image cropped in Gimp.<br>The original image is in the public domain because...
This is a virtual print of Apollo Photograph AS15-M-2621 generated by the School of Earth and Space Exploration, Arizona State University. Usage of this image is governed by the Acceptable Use Policy, which can be accessed at -{R|http://apollo.sese.asu.edu/ABOUT_SCANS/index.html}-