Planetary Geology pdf - NASA
Planetary Geology pdf - NASA
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.