A little more than three years after Neil Armstrong took mankind’s first steps on the moon, Apollo 17 astronauts left the last footprints on the lunar surface in December of 1972. Described by NASA as “the last, longest, and most successful” of the manned lunar landing missions, Apollo 17 yielded significant scientific discoveries and produced one of the most famous images in history of planet Earth.
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Apollo 17 Sends the First Scientist to Space
The mission began on December 7, 1972 when, at 33 minutes past midnight, the engines of a Saturn V rocket erupted and bathed Florida’s Cape Canaveral in an orange glow. As night turned to day, the fireball blinded spectators who came to see Apollo 17 roar skyward.
Within minutes, the plume of flame faded to a speckle among the stars as the Apollo program launched its final mission to the moon. The Apollo 17 crew included commander Eugene Cernan, command module pilot Ronald Evans and lunar module pilot Harrison “Jack” Schmitt—the first astronaut originally trained as a scientist to soar into space.
A geologist with a doctorate from Harvard University, Schmitt had been among six scientists selected from a pool of 1,400 applicants to join the astronaut corps in 1965. He had been assigned to the crew of Apollo 18, but when budget cuts led NASA to cancel that mission along with Apollo 19 and 20, agency administrators assigned him to replace astronaut Joe Engle on the last lunar flight.
Four days after Apollo 17’s launch, Evans orbited the moon as Schmitt and Cernan landed the lunar module Challenger in the narrow Taurus-Littrow valley, which is deeper than the Grand Canyon and marked the easternmost landing site of any Apollo mission. Schmitt and Cernan—a veteran astronaut who had flown aboard Gemini 9 and Apollo 10—spent seven-hour stints on three consecutive days exploring the surrounding craters, boulders and mountains. Below a half-Earth hanging in the black sky, they assembled a science station to relay data, took gravity measurements, chipped fragments off ancient boulders and collected subsurface core samples.