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Earth's Moon
The document provides information about the Moon and its exploration history. It describes the Moon's size and distance from Earth. Key events in lunar exploration included Soviet missions in 1959 and US missions in the 1960s including Rangers, Lunar Orbiters, and Surveyors. The Apollo 11 mission in 1969 was the first to land humans on the Moon. The document discusses lunar geology, noting differences from Earth like the lack of an atmosphere, water, or plate tectonics. It describes lunar features such as maria, highlands, craters, and rilles. The formation of the Moon is also summarized.
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Earth's Moon
- 1. SMART-1 Small Missions for AdvancedResearch in Technology
- 2. The Moon A lookat our nearest neighbor in Space!
- 3. What is theMoon? • A natural satellite • One of more than 96 moons in our Solar System • The only moon of the planet Earth
- 4. Moon’s Location fromEarth • About 384,000 km (240,000 miles) from Earth • 3,468 km (2,155 miles) in diameter (about ¼ the size of Earth)
- 5. A Brief Historyof Lunar Exploration • 1959: Soviet Lunas 1, 2, 3 orbited around Moon • 1960’s: US Ranger - flyby mission - first space pictures - many TV cameras • 1966-67: Lunar Orbiter - 5 orbiting spacecraft - full coverage of pictures • 1966-68: Lunar Surveyor - surveying for landing sites - testing the “soil” (sink?)
- 6. Highlights from Apollo11 mission launch: July 16th 1969 arrival at Moon: July 20th 1969 first humans to land on the Moon Command Module (CM): “Columbia”
- 7. On July 20,1969, after a four day trip, the Apollo astronauts arrived at the Moon. This photo of Earthrise over the lunar horizon is one of the most famous images returned from the space program, although even the astronauts themselves cannot remember who actually took it. 13 Oct 2003 Solar System - Dr. C.C. Lang 7
- 8. First steps onthe Moon • July 20th 1969 - Neil Armstrong - “Buzz” Aldrin 13 Oct 2003 Solar System - Dr. C.C. Lang 8
- 9. Touchdown of Moonastronauts near the coast of Hawaii on July 26th 1969
- 10. Earth Moon • Active wind/water erosion • NO Activewind/water erosion • Impacts • Impacts • Active volcanoes • NO active volcanoes • Earthquakes • Small moonquakes • Active magnetic field • NO active magnetic field • Few craters • Buckets of craters Geologically Active! Geologically Inactive!
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- 12. Earth Moon HOT! Not so hot! Why sodifferent?
- 13. 3 Layers ofthe Moon 1) Crust - average thickness of about 70 kilometers 2) Mantle 3) Core - radius is between 300 and 425 kilometers
- 14. The Moon’s Surface •No atmosphere • No liquid water • Extreme temperatures Daytime = 130C Nighttime = -190C • 1/6 Earth’s gravity
- 15. Lunar Features Highlands • Mountainsup to 7500 m (25,000 ft) tall • Rilles (trenchlike valleys)
- 16. Lunar Features Craters • Upto 2500 km (1,553 miles) across • Most formed by meteorite impact on the Moon • Some formed by volcanic action inside the Moon
- 17. Lunar Features Maria • Originallythought to be “seas” by early astronomers • Darkest parts of lunar landscape • Filled by lava after crash of huge meteorites on lunar surface 3-4 billion years ago • Mostly basalt rock
- 18. Craters Can you seethe rays? Maria
- 19. Movements of theMoon • Revolution – Moon orbits the Earth every 27 1/3 days • Rotation – Moon turns on its axis every 27 days
- 20. Movements of theMoon • The moon rises in the east and sets in the west • The moon rises and sets 50 minutes later each day • Same side of Moon always faces Earth
- 21. Far Side ofthe Moon • First seen by Luna 3 Russian space probe in 1959 • Surface features different from near side –More craters –Very few maria –Thicker crust
- 22. Lunar Formation Models Themoon is a sister world that formed in orbit around Earth as the Earth formed. The moon formed somewhere else in the solar system then was captured into orbit around Earth. Early Earth spun so fast that it spun off the moon.
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- 30. Lunar Geologic History 4.5billion years ago, our Moon forms (lunar rocks and meteorites) Copyrighted, LPI
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- 32. Magma Ocean Rocks 76535 Troctolite 4.2-4.3Ga 60025 Anorthosite 4.44-4.51 Ga 95% Plag Feld (anorthite) Magma Ocean! No Water!
- 33. Lunar Geologic History Highlands- light, rough (Terrae) Mostly anorthosite (plagioclase feldspars lots of calcium and aluminum) “In place” rocks are 4.5 to 4.3 billion years old BIG Dark areas?
- 34. Lunar Impact Basins ImbriumRim Big, frequent impacts until 3.8 billion years ago Impact events continue on all moons and planets today Orientale Basin
- 36. Rays Ejecta Floor Wall Tycho Crater Rim Central Peak Young– 100 MY 85 kilometers across Fresh (rays) = young
- 37. Impacts …“the mostfundamental process on the terrestrial planets…” Eugene and Carolyn Shoemaker
- 38. Breccias and ImpactMelts 15445 Impact melt + clasts 67016 Polymict Breccia
- 39. Lunar Geologic History MareVolcanism Mare Imbrium Volcanism after impacts – most before 3 Ga (to 1 Ga) SW Mare Imbrium
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- 44. Lunar Geologic History Lowlands– dark, smooth Maria (16%) Basalt – fine grained dark igneous rock rich in iron and magnesium (stuff that sank in magma ocean) Few hundred meters thick Rocks are 4.3 to 3.1 billion years old … volcanic flows as recently as 1 billion years ago!!
- 45. And then …. Allwas quiet.
- 46. • Except forimpacts... 7 November; ~30 lb TNT 3 m-wide crater (estimate)
- 47. • No Wind •No Flowing Water • No Erosion
- 48. • Except forimpacts...
- 49. Return to theMoon! • 2012 – Develop and test technologies for resource utilization, communicati ons, power • 2014 – CEV, Ares launch vehicle
- 50. • 2018 –Humans for week-long stays • Next: 45-day stays at outposts
- 52. Free powerpoints athttp://www.worldofteaching.com