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1.5. rezultāts no 100.
2. lappuse
... landing site . Similar evidence has just been discovered at the Apollo 14 site . No evidence of water or past or present life has been found on the moon thus far . Rocks and soil have been returned with ages ranging from 3.3 to 4.6 ...
... landing site . Similar evidence has just been discovered at the Apollo 14 site . No evidence of water or past or present life has been found on the moon thus far . Rocks and soil have been returned with ages ranging from 3.3 to 4.6 ...
3. lappuse
... landing sites . They have emplaced a network of 14 long - lived scien- tific instruments on the lunar surface and have returned 219 pounds of lunar samples for detailed analysis . The manufacture , assembly and factory test of most ...
... landing sites . They have emplaced a network of 14 long - lived scien- tific instruments on the lunar surface and have returned 219 pounds of lunar samples for detailed analysis . The manufacture , assembly and factory test of most ...
4. lappuse
... landing mission was launched from Kennedy Space Center on April 11 , 1970. Its major objective was to explore the Fra Mauro for- mation . Launch , earth orbital insertion , and translunar trajectory insertion all were satisfactory ...
... landing mission was launched from Kennedy Space Center on April 11 , 1970. Its major objective was to explore the Fra Mauro for- mation . Launch , earth orbital insertion , and translunar trajectory insertion all were satisfactory ...
5. lappuse
... landing . The Command Module , while still capable of supporting life of the crew for a short period , no longer contained enough consumables for the long journey around the moon and back to earth . It was , therefore , decided to ...
... landing . The Command Module , while still capable of supporting life of the crew for a short period , no longer contained enough consumables for the long journey around the moon and back to earth . It was , therefore , decided to ...
6. lappuse
... energy penetrated to a depth of 24 miles . This compares with a depth of 12.5 miles for the Apollo 13 S - IVB impact . APOLLO 14 LIFTOFF JANUARY 31 , 1971 NASA HQ MA71-5293 2-10-71 GEOLOGIC MAP OF THE MOON WITH LANDING SITES A B. 6.
... energy penetrated to a depth of 24 miles . This compares with a depth of 12.5 miles for the Apollo 13 S - IVB impact . APOLLO 14 LIFTOFF JANUARY 31 , 1971 NASA HQ MA71-5293 2-10-71 GEOLOGIC MAP OF THE MOON WITH LANDING SITES A B. 6.
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activities Aerojet aerospace AIRLOCK analysis Apollo 15 Apollo program Apollo Telescope Mount applications ASSEMBLY astronauts Boeing booster capability chamber chart checkout combustion components concept configuration contract contractors Convair cost crew earth orbit Earth Resources environment equipment evaluation facilities FIGURE function future going hardware heat injector integrated Kennedy Space Center laboratory landing launch vehicle lunar major manufacturing materials MCDONNELL DOUGLAS ment million mission MSFC NASA HQ North American Rockwell operations ORBITAL WORKSHOP payload performance phase planning preburner problems propellant propulsion reduce requirements reusable rocket S-IVB satellites Saturn IB schedule SCIENCE scientific Service Module shown SKYLAB EXPERIMENT Skylab Program SLIDE solar Space Flight space program SPACE SHUTTLE PROGRAM Space Station spacecraft stage structure studies subsystems surface tanks TEAGUE technical Telescope thermal protection system thrust tion transportation turbopumps unmanned utilization weight