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Friday, May 27, 2022
Home Topography of Earth’s moon generated from data collected by the Lunar Orbiter Laser Altimeter, aboard NASA’s Lunar Reconnaissance Orbiter, with the gravity anomalies bordering the Procellarum region superimposed in blue. (NASA/Colorado School of Mines/MIT/GSFC/Scientific Visualization Studio) Topography of Earth's moon generated from data collected by the Lunar Orbiter Laser Altimeter, aboard NASA's Lunar Reconnaissance Orbiter, with the gravity anomalies bordering the Procellarum region superimposed in blue. (NASA/Colorado School of Mines/MIT/GSFC/Scientific Visualization Studio)

Topography of Earth’s moon generated from data collected by the Lunar Orbiter Laser Altimeter, aboard NASA’s Lunar Reconnaissance Orbiter, with the gravity anomalies bordering the Procellarum region superimposed in blue. (NASA/Colorado School of Mines/MIT/GSFC/Scientific Visualization Studio)

Topography of Earth's moon generated from data collected by the Lunar Orbiter Laser Altimeter, aboard NASA's Lunar Reconnaissance Orbiter, with the gravity anomalies bordering the Procellarum region superimposed in blue. (NASA/Colorado School of Mines/MIT/GSFC/Scientific Visualization Studio)

Topography of Earth’s moon generated from data collected by the Lunar Orbiter Laser Altimeter, aboard NASA’s Lunar Reconnaissance Orbiter, with the gravity anomalies bordering the Procellarum region superimposed in blue. (NASA/Colorado School of Mines/MIT/GSFC/Scientific Visualization Studio)

A view of Earth’s moon looking south across Oceanus Procellarum, representing how the western border structures may have looked while active. (NASA/Colorado School of Mines/MIT/JPL/GSFC)