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Planetary Geology pdf - NASA

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Exercise<br />

One<br />

Suggested Correlation of Topics<br />

The Earth, geography, gradation, impact<br />

cratering, earth science introduction,<br />

tectonism, volcanism<br />

Purpose<br />

The objective of this exercise is to show the frequency<br />

and distribution of events on Earth resulting<br />

from the four major geologic processes. In this<br />

exercise, the student will process and analyze a<br />

geologic data set to produce graphic and written<br />

results. Locating event sites will improve world<br />

geography skills.<br />

Materials<br />

Suggested: magazines and newspapers, glue or<br />

tape, paper, colored pens or pencils, straightedge or<br />

ruler, atlas or world almanac (one atlas per student<br />

group). Substitutions: wall-size world map can substitute<br />

for an atlas.<br />

Background<br />

This exercise illustrates the general frequency<br />

and distribution of volcanic, tectonic, gradational,<br />

and impact cratering events. It is important that students<br />

have an introduction to these processes<br />

through lectures, videos, or slides before working<br />

the assignment. Volcanic and tectonic events (volcanic<br />

eruptions and earthquakes) are typically large<br />

in scale and short in duration. That is, each event<br />

often results in great disruption over a large area,<br />

but last only a short time. However, over long periods<br />

of time, these processes can produce large landforms<br />

such as mountains, plains, ocean basins and<br />

islands. Impact cratering is of short duration and<br />

the frequency of impacts is very low compared to a<br />

Exercise One: Geologic Events on Earth<br />

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

3<br />

2.0 hours each part<br />

(with instructor<br />

modification for grade<br />

level)<br />

Geologic Events<br />

on Earth<br />

Instructor Notes<br />

human lifespan. Early in EarthÕs history, impact cratering<br />

was much more common, but now there are<br />

fewer objects in space to act as impactors. Gradation<br />

occurs at all scales from the erosion of mountain<br />

ranges to the grinding of sand grains in streams.<br />

Gradation on Earth occurs on time scales from seconds<br />

to centuries or more.<br />

Teacher Recommendations<br />

Part One of the exercise requires the student to<br />

collect data in the form of pictures and newspaper<br />

articles. This part can be done in several ways: it can<br />

be assigned as a take-home exercise, the instructor<br />

can collect magazines and newspapers to enable<br />

completing the exercise during a single class period,<br />

students can use a library (make photocopies<br />

instead of cutting up papers), or it can be omitted.<br />

Finding pictures that illustrate landforms created by<br />

all four processes can be frustrating. Many magazine<br />

advertisments with landscapes as the background<br />

will be useful. Make sure only one representation<br />

of an individual event is used; for example,<br />

a major earthquake will get extensive coverage<br />

by the mediaÑbut only one picture of that earthquake's<br />

effects should be used. Encourage the students<br />

to explain the types of landforms they select<br />

and help them classify the formation processes.<br />

Impact cratering occurs so infrequently that it is<br />

unlikely to be represented in magazines; however,<br />

pictures of the Moon show craters and it is up to the<br />

instructor to decide if such pictures can be used. It is<br />

recommended that the exercise be limited to the<br />

Earth. Suggested modifications of Part One for different<br />

grade levels are as follows:<br />

Grades KÐ4: Eliminate procedure B; use<br />

procedure D and questions<br />

1, 2, 5, and 6 for class discussion.<br />

Work in groups, completing the<br />

exercise in class.

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