1. Universe Eighth Edition Universe Roger A. Freedman William J. Kaufmann III CHAPTER 10 Our Barren Moon CHAPTER 10 Our Barren Moon

3. Online quizzes from Chapters 9 and 10 due Monday 10/18 Online Quiz from Chapter 11 due Wednesday 10/20 HW Update

10. Some areas of the Moon are relatively smooth, whereas other areas are heavily cratered. This is because A. meteors did not strike the flat areas because they are in the Earth’s shadow. B. weathering has smoothed parts of the Moon. C. plate tectonics has recycled parts of the lunar crust. D. in some places lava flows have covered over older craters, leaving a smoother surface. E. tidal forces between the Earth and Moon smoothed parts of the Moon. Q10.4

11. Some areas of the Moon are relatively smooth, whereas other areas are heavily cratered. This is because A. meteors did not strike the flat areas because they are in the Earth’s shadow. B. weathering has smoothed parts of the Moon. C. plate tectonics has recycled parts of the lunar crust. D. in some places lava flows have covered over older craters, leaving a smoother surface. E. tidal forces between the Earth and Moon smoothed parts of the Moon. A10.4

21. The astronaut footprint on the Moon shown in this photograph will probably A. exist for >10,000 years because there is very little weathering on the Moon. B. exist for >10,000 years because the Moon’s surface is hard and durable. C. exist for <10,000 years due to erosion from wind in the tenuous lunar atmosphere. D. exist for <10,000 years due to bombardment by large numbers of meteors. E. Both C and D are correct. Q10.1

22. The astronaut footprint on the Moon shown in this photograph will probably A. exist for >10,000 years because there is very little weathering on the Moon. B. exist for >10,000 years because the Moon’s surface is hard and durable. C. exist for <10,000 years due to erosion from wind in the tenuous lunar atmosphere. D. exist for <10,000 years due to bombardment by large numbers of meteors. E. Both C and D are correct. A10.1

29. Key Ideas Appearance of the Moon: The Earth-facing side of the Moon displays light-colored, heavily cratered highlands and dark-colored, smooth-surfaced maria. The Moon’s far side has almost no maria. Appearance of the Moon: The Earth-facing side of the Moon displays light-colored, heavily cratered highlands and dark-colored, smooth-surfaced maria. The Moon’s far side has almost no maria. Virtually all lunar craters were caused by space debris striking the surface. There is no evidence of plate tectonic activity on the Moon. Virtually all lunar craters were caused by space debris striking the surface. There is no evidence of plate tectonic activity on the Moon.

30. Key Ideas Internal Structure of the Moon: Much of our knowledge about the Moon has come from human exploration in the 1960s and early 1970s and from more recent observations by unmanned spacecraft. Internal Structure of the Moon: Much of our knowledge about the Moon has come from human exploration in the 1960s and early 1970s and from more recent observations by unmanned spacecraft. Analysis of seismic waves and other data indicates that the Moon has a crust thicker than that of the Earth (and thickest on the far side of the Moon), a mantle with a thickness equal to about 80% of the Moon’s radius, and a small iron core. Analysis of seismic waves and other data indicates that the Moon has a crust thicker than that of the Earth (and thickest on the far side of the Moon), a mantle with a thickness equal to about 80% of the Moon’s radius, and a small iron core.

31. Key Ideas The Moon’s lithosphere is far thicker than that of the Earth. The Moon’s lithosphere is far thicker than that of the Earth. The lunar asthenosphere probably extends from the base of the lithosphere to the core. The lunar asthenosphere probably extends from the base of the lithosphere to the core. The Moon has no global magnetic field today, although it had a weak magnetic field billions of years ago. The Moon has no global magnetic field today, although it had a weak magnetic field billions of years ago.

32. Key Ideas Geologic History of the Moon: The anorthositic crust exposed in the highlands was formed between 4.3 and 4.0 billion years ago. Geologic History of the Moon: The anorthositic crust exposed in the highlands was formed between 4.3 and 4.0 billion years ago. An era of heavy bombardment formed the maria basins between 4.0 and 3.8 billion years ago, and the mare basalts solidified between 3.8 and 3.1 billion years ago. An era of heavy bombardment formed the maria basins between 4.0 and 3.8 billion years ago, and the mare basalts solidified between 3.8 and 3.1 billion years ago. The Moon’s surface has undergone very little change over the past 3 billion years. The Moon’s surface has undergone very little change over the past 3 billion years.

33. Key Ideas Meteoroid impacts have been the only significant “weathering” agent on the Moon. Meteoroid impacts have been the only significant “weathering” agent on the Moon. The Moon’s regolith, or surface layer of powdered and fractured rock, was formed by meteoritic action. The Moon’s regolith, or surface layer of powdered and fractured rock, was formed by meteoritic action. All of the lunar rock samples are igneous rocks formed largely of minerals found in terrestrial rocks. All of the lunar rock samples are igneous rocks formed largely of minerals found in terrestrial rocks. The lunar rocks contain no water and also differ from terrestrial rocks in being relatively enriched in the refractory elements and depleted in the volatile elements. The lunar rocks contain no water and also differ from terrestrial rocks in being relatively enriched in the refractory elements and depleted in the volatile elements.

34. Key Ideas Origin of the Moon: The collisional ejection theory of the Moon’s origin holds that the proto-Earth was struck by a Mars-sized protoplanet and that debris from this collision coalesced to form the Moon. This theory successfully explains most properties of the Moon. Origin of the Moon: The collisional ejection theory of the Moon’s origin holds that the proto-Earth was struck by a Mars-sized protoplanet and that debris from this collision coalesced to form the Moon. This theory successfully explains most properties of the Moon. The Moon was molten in its early stages, and the anorthositic crust solidified from low-density magma that floated to the lunar surface. The mare basins were created later by the impact of planetesimals and filled with lava from the lunar interior. The Moon was molten in its early stages, and the anorthositic crust solidified from low-density magma that floated to the lunar surface. The mare basins were created later by the impact of planetesimals and filled with lava from the lunar interior. Tidal interactions between the Earth and Moon are slowing the Earth’s rotation and pushing the Moon away from the Earth. Tidal interactions between the Earth and Moon are slowing the Earth’s rotation and pushing the Moon away from the Earth.