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Planetary Geology pdf - NASA

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Part One<br />

1. (Answers will vary.) Volcanism, tectonism,<br />

gradation.<br />

2. (Answers will vary.) Impact cratering.<br />

3. (Answers will vary.) Tectonism, gradation,<br />

volcanism.<br />

4. (Answers will vary.) Impact cratering.<br />

5. Answers will vary, but should indicate tectonism<br />

and gradation occur more often than volcanism<br />

and impact cratering (which is very<br />

rare).<br />

6. a. Answers will vary, however, volcanoes<br />

tends to form large features over a short<br />

period of time.<br />

b. Answers will vary, however, gradation can<br />

level mountains and fill in large bodies of<br />

water over the course of millions of years.<br />

c. Answers will vary. Location of population<br />

centers in relation to known areas of volcanism<br />

and tectonism and the ability to<br />

predict activity due to these processes will<br />

control their impact on society (which can<br />

be great over a short time period, or have<br />

no effect during centuries of dormancy).<br />

Large gradational events, such as floods,<br />

can do as much damage to property and<br />

cause as much loss of life as large earthquakes<br />

or volcanic eruptions.<br />

Part Two<br />

North America: B. 6 tectonic, 8 gradation,<br />

4 volcanic, 1 impact.<br />

South America: B. 6 tectonic, 4 gradation,<br />

3 volcanic, 0 impact.<br />

Europe: B. 1 tectonic, 1 gradation,<br />

0 volcanic, 0 impact.<br />

Africa: B. 2 tectonic, 1 gradation,<br />

0 volcanic, 0 impact.<br />

Exercise One: Geologic Events on Earth<br />

Answer Key<br />

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

5<br />

Asia: B. 9 tectonic, 6 gradation,<br />

4 volcanic, 0 impact.<br />

Antarctica: B. 1 tectonic, 0 gradation,<br />

0 volcanic, 0 impact.<br />

Australia: B. 6 tectonic, 0 gradation,<br />

1 volcanic, 0 impact.<br />

Atlantic Islands: B. 8 tectonic, 0 gradation,<br />

0 volcanic, 0 impact.<br />

Pacific Islands: B. 28 tectonic, 3 gradation,<br />

8 volcanic,<br />

0 impact.<br />

Complete data set: B. 67 tectonic, 23 gradation,<br />

20 volcanic,<br />

1 impact.<br />

1. Tectonism.<br />

2. Impact cratering. Not many objects in space act<br />

as meteorites, most burn up in the atmosphere<br />

before impact, many land in the oceans.<br />

3. Volcanism and most tectonic events border the<br />

Pacific Ocean (the ÒRing-of-Fire,Ó related to<br />

plate tectonics). Most tectonic events are related<br />

to plate boundaries, but due to the limited<br />

numbers, will appear to be randomly distributed<br />

except for those in the Pacific. Gradation<br />

events are randomly located. With only one<br />

event it cannot be determined from the data,<br />

but impact cratering is also random.<br />

4. Gradation. No. On the Earth, water and wind<br />

work to physically and chemically break up the<br />

surface and then move the materials to new<br />

locations for deposition. Lacking wind, water,<br />

and ice, gradation on the Moon occurs by physically<br />

breaking up the surface during impacting<br />

events. The surface materials are only transported<br />

if they are thrown out by an impacting<br />

event.

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