1. Compared to oceanic crust, continental crust is
a. denser.
b. usually formed
with less than 50 percent silica and is rich in iron and magnesium.
c. generally more
complex in content and structure.
d. essentially
composed of basalt.
e. thinner.
2. The evidence that convinced most geologists that the Earth's crust was comprised of individual, non-stationary plates was
a. bands of
crystalline rock near mid-oceanic ridges in which magnetic orientation
of crystals alternated as one moved away from the ridge.
b. the existence
of mountain ranges near the leading edges of the hypothesized plates.
c. similarities
of plants and animals on the east coast of South America and west coast
of Africa.
d. existence of
similar mineral ore bodies on opposite sides of the Atlantic Ocean.
e. geological
strata found in Montana that contained fossils of tropical organisms -
the region had to have been in the tropics at an earlier time.
3. Which of the following is not
an example of a kind of tectonic plate boundary?
a. Convergent
boundary - two plates collide.
b. Divergent boundary - two plates are pushed away
from each other by magma intrusion in a spreading sea floor zone.
c. Transform fault boundary - two plates move
laterally in different directions.
d. Normal fault boundary - tensional forces pull two
plates away from one another.
e. None of these answers is a kind of tectonic plate
boundary.
a. convergent
plate boundary
b. divergent
plate boundary
c. island arc
along a subduction zone
d. shield
or craton
e. mountain range
5. Vertical elevation differences in local landscape are referred to as
a. relief.
b. an order of
relief.
c. topography.
d. crust.
e. slope angle.
6. The undulating form that gives Earth's surface its character and general configuration is called
a. relief. a. tectonic
activity.
b. gravity.
c. weathering.
d. erosion.
e. all of these
answers are correct.
17. Which of the following is not true of terranes?
a. They are
smaller-scale migrating crustal pieces, i.e. microplates.
b. They may
accrete onto continents and thereby increase the size of the continents.
c. They are
framed by fracture zones.
d. They are very
similar in composition to the continents to which they attach.
e. They can move
thousands of kilometers from their place of origin.