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Planetary Geology pdf - NASA

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1. The highlands are bright, rugged and heavily<br />

cratered. The plains are dark, flat, smooth and<br />

less cratered.<br />

2. The highlands.<br />

3. The highlands.<br />

4. Younger.<br />

5. Cratered plains and rayed craters.<br />

6. Older than the lunar plains. (Lunar plains are<br />

often called maria.)<br />

7. All three surfaces have craters, although Mars<br />

has the least. Mars has more extensive smooth<br />

plains than the Moon or Mercury; no obvious<br />

volcanoes or canyons are visible on either<br />

Mercury or the Moon. Only Mars shows polar<br />

ice caps.<br />

8. Mars has a dynamic atmosphere (including<br />

dust storms). Gradation by running water<br />

occurred on Mars, but water never flowed on<br />

the Moon. Volcanic activity has been more<br />

extensive on Mars. Tectonism has occurred on<br />

Mars. On the Moon, impact cratering and<br />

plains volcanism have been the major geologic<br />

processes; on Mars, all four major geologic<br />

processes have worked to shape the surface.<br />

9. Younger.<br />

10. The southern region is older.<br />

11. Mars.<br />

12. a. Both are long and relatively narrow. The<br />

canyon on Mars is straight, the one on Venus is<br />

arcuate. [If the student says the Venus canyon<br />

is bright and the Mars canyon is dark, remind<br />

them of the differences in imaging systems:<br />

radar vs. optical camera.]<br />

13. Younger.<br />

14. a. Smooth plains, canyons (deep ocean trenches<br />

and rifts in Africa), volcanoes (represented<br />

by islands) and rough ÒhighlandsÓ (mountain<br />

ranges).<br />

b. Continents, mid-ocean rift/ridge zones.<br />

15. a. Similarities: if EarthÕs continents are thought<br />

of as Òhighlands,Ó both can be divided into<br />

highÐ and low-standing regions; low-lying<br />

regions are relatively smooth. Differences: the<br />

Moon is dominated by craters; lowlands on<br />

the Moon are formed by large impacts flooded<br />

Answer Key<br />

116<br />

by volcanic material; no linear mountain chains<br />

on the Moon; no prominent arcuate ridges or<br />

trenches on the Moon.<br />

b. Students will have difficulty finding any<br />

similarities between Earth and Mercury.<br />

Differences: Mercury is dominated by craters<br />

(impact cratering is the prominent geologic<br />

process); on this image of the Earth, impact<br />

cratering is the only geologic process that is not<br />

apparent.<br />

c. Similarities: both have volcanic and tectonic<br />

landforms. Differences: no continents or midocean<br />

ridge system on Mars, no craters seen on<br />

this global view of Earth.<br />

d. Similarities: both show arcuate mountain<br />

ranges; both show expansive smooth regions;<br />

neither shows very large craters. Differences:<br />

more extreme topography on Earth, continents<br />

and deep ocean basins, compared to more uniform<br />

topographic level on Venus; no midocean<br />

ridge systems on Venus.<br />

16. a. Oldest to youngest: Mercury, Moon, Mars,<br />

Venus, Earth.<br />

b. Answers will vary based on students perception<br />

of Òmost complex.Ó Earth has the most<br />

active geologic history reflected on its surface,<br />

however, some students may argue that Venus is<br />

more complex. Least to most complex: Mercury,<br />

the Moon, Mars, Venus, Earth.<br />

17. (This representation is ~1/3 the size of what<br />

student answer should be.)<br />

Moon Mercury Mars Venus Earth<br />

*18. Answers may vary. In general it is true that the<br />

larger the terrestrial planet, the more complex<br />

its surface. This is not strictly true, however:<br />

the Moon, despite its smaller size, is arguably<br />

more complex than Mercury. Students might<br />

wish to debate the relative complexity of Earth<br />

and Venus, or Venus and Mars, as seen at the<br />

global scale.<br />

Exercise Ten:<br />

Landform Mapping: The Terrestrial Planets<br />

Activities in <strong>Planetary</strong> <strong>Geology</strong> for the Physical and Earth Sciences EG-1998-03-109-HQ

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