Table 11.1 shows the three major plate margin types as well as the three possible physiographic combinations for each. Two of these combinations are rare or nonexistent (shaded boxes on table 11.1). Study figure 11.2 and complete the rest of the table by entering names of modern geographic locations that serve as examples for each of the seven characteristic plate margins.

Applications and Investigations in Earth Science (9th Edition)
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Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
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Chapter1: The Study Of Minerals
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Table 11.1 shows the three major plate margin types as well as the three possible physiographic combinations for each. Two of these combinations are rare or nonexistent (shaded boxes on table 11.1). Study figure 11.2 and complete the rest of the table by entering names of modern geographic locations that serve as examples for each of the seven characteristic plate margins.

160 Exercise 11
Continental Drift and Plate Tectonics
PART C
Characteristics of Plate Margins
Table 11.1 shows the three major plate margin
types as well as the three possible physiographic
combinations for each. Two of these combinations
are rare or nonexistent (shaded boxes on table 11.1).
Study figure 11.2 and complete the rest of the table
by entering names of modern geographic locations
that serve as examples for each of the seven charac-
teristic plate margins.
Modern Examples by Geographic Name
Plate Margin
Continent-Continent
Continent-Ocean
Ocean-Ocean
Divergent
• Tensional stresses
• Crustal lengthening
• New ocean crust
• Normal faults
• Shallow earthquakes
• Basaltic volcanism
Convergent
• Compressional stress
• Crustal shortening
• Ocean crust destroyed
• Reverse and thrust
faults
• Folds
• New continental crust
• Shallow and deep
quakes
Transform Fault
• Shear stress
• Shallow quakes
• Crust neither created
nor destroyed
• Strike-slip faults
TABLE 11.1
Table showing types and characteristics of plate margins.
Transcribed Image Text:160 Exercise 11 Continental Drift and Plate Tectonics PART C Characteristics of Plate Margins Table 11.1 shows the three major plate margin types as well as the three possible physiographic combinations for each. Two of these combinations are rare or nonexistent (shaded boxes on table 11.1). Study figure 11.2 and complete the rest of the table by entering names of modern geographic locations that serve as examples for each of the seven charac- teristic plate margins. Modern Examples by Geographic Name Plate Margin Continent-Continent Continent-Ocean Ocean-Ocean Divergent • Tensional stresses • Crustal lengthening • New ocean crust • Normal faults • Shallow earthquakes • Basaltic volcanism Convergent • Compressional stress • Crustal shortening • Ocean crust destroyed • Reverse and thrust faults • Folds • New continental crust • Shallow and deep quakes Transform Fault • Shear stress • Shallow quakes • Crust neither created nor destroyed • Strike-slip faults TABLE 11.1 Table showing types and characteristics of plate margins.
158 A
Exercise 11
Continental Drift and Plate Tectonics
168 of 307
5.4
1.8
Eurasian Plate
Eurasian Plate
North American Plate
2.3
3.7
2.0
Phillipine
Plate
African Plate
9.2
2.5
Pacific Plate
11.7
10.5
10.1
2.5
17.2
South American
Indo-
Nazca Plate
Plate
Australian
Plate
7.1
11.1
18.2
A'
A
6.2
1.7
3.7
10.3
1.3
7.2
3.4
7.7
Antarctic Plate
5000 kilometers
5.6
convergent
divergent & transform
hotspot
FIGURE 11.2 Map of the world showing the major plates, their boundaries, and direction of motion. Subduction zones are indicated by green lines.
Red circles are presently active hot spots. Numbers indicate rate of motion in cm/yr. (Rates after McKenzie and Richter, 1976.)
Transcribed Image Text:158 A Exercise 11 Continental Drift and Plate Tectonics 168 of 307 5.4 1.8 Eurasian Plate Eurasian Plate North American Plate 2.3 3.7 2.0 Phillipine Plate African Plate 9.2 2.5 Pacific Plate 11.7 10.5 10.1 2.5 17.2 South American Indo- Nazca Plate Plate Australian Plate 7.1 11.1 18.2 A' A 6.2 1.7 3.7 10.3 1.3 7.2 3.4 7.7 Antarctic Plate 5000 kilometers 5.6 convergent divergent & transform hotspot FIGURE 11.2 Map of the world showing the major plates, their boundaries, and direction of motion. Subduction zones are indicated by green lines. Red circles are presently active hot spots. Numbers indicate rate of motion in cm/yr. (Rates after McKenzie and Richter, 1976.)
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