GEOL1122 Fall 2009
1) a 10) b 19) c
2) d 11) b 20) b
3) d 12) d 21) d
4) a 13) c 22) b
5) b 14) b 23) c
6) a 15) a 24) a
7) c 16) c 25) b
8) a 17) d
9) c 18) d
26-27) Stress; strain
28) anticline
29) monocline
30-31) normal; Basin and Range
32) joints
33) thrust
34) Paleobiogeography
35-36) Coal – temperate swamps; limestone – warm, clear, shallow marine; glacial till – cold subpolar; rock salt and rock gypsum – mid-latitude deserts
36-39)
|
Type of Plate Boundary |
Volcanism |
Geologic Structures |
Example |
|
Convergent Ocean-Continent |
Very common andesite volcanism |
Thrust faults and folds |
Western South America |
|
Divergent Continent-Continent |
Very common basalt volcanism |
Normal faults and rift basins |
East Africa |
|
Transform between Any Plate Type |
None |
Strike-slip Faults |
Sand Andreas Fault |
40-41) South America, Africa, Antarctica, Australia and India
42) 10-20 cm/year
43) thermal convection
44) Mesosaurus
45-46) older; thicker; colder; and more dense
47) Benioff Zones
48-49) It has been subducted as the oceanic plates continue to form new crust along ridges and rises.
50) lithosphere
Extra Credit: Alfred Wegener – Father of Plate Tectonic Theory