Chapter 12
Volcanic and Tectonic Landforms
OVERVIEW
This chapter examines some of the major surface expressions of
plate tectonic activity. These include landforms produced by volcanic
activity and by the folding and faulting of crustal rocks, as
well as earthquake activity.
- The surface forms of the earth's crust are known as
landforms and the study of the processes which produce these
features is called geomorphology.
-
Initial landforms are formed by volcanic and tectonic
activity while sequential landforms are formed by the agents
of denudation such as running water, waves, wind and glacier
ice.
- Lava eruptions at the earth's surface form volcanoes.
-
Stratovolcanoes form from the eruption of thick,
gassy, felsic lavas and are most common along the converging plate
boundaries of the Pacific rim. They have steep sides and often
have explosive eruptions that form calderas.
- Broadly rounded shield volcanoes form over hotspots
and along midoceanic ridges where more fluid, less gassy basaltic
lavas erupt. These lavas can form vast flood basalts when
they erupt on continents.
- Tectonic movements can apply both compressional
and extensional forces to rock.
- Compression along converging plate boundaries initially
causes folding which produces anticlines and synclines.
Sustained compression can lead to folds being overturned and to
overthrust faulting.
- Extension along spreading boundaries generates normal
faults with upthrown and downdropped blocks that can be as
large as mountain ranges and rift valleys.
-
Transcurrent faults occur where rock masses move
horizontally past each other.
-
Earthquakes occur when tectonic forces cause rock
to suddenly fracture and move shaking the ground in the vicinity
of the fracture.
- Submarine earthquakes can produce sea waves known as tsunami.
- The Richter scale is a logarithmic scale used to
measure the energy released by an earthquake.
- Most severe earthquakes occur along tectonic plate
boundaries.
KEY TERMS
landform stratovolcano normal fault
geomorphology shield volcano transcurrent
denudation folding fault
volcano fault earthquake
tsunami
STUDY QUESTIONS
- Distinguish between initial and sequential landforms.
- Define denudation and give three examples of denudation agents.
- Discuss the way in which the internal earth processes and
denudation processes interact to produce landforms.
- Two major types of volcanoes are stratovolcanoes and shield
volcanoes. How do these two types of volcanoes differ in their
shape, material composition and usual position on lithospheric
plates?
- What is the difference between a hot spring and a geyser?
- What are compressional and extensional tectonic activity and
where do these usually occur?
- Sketch a cross-section of an anticline, a syncline and an
overturned fold.
- Sketch a cross-section of a normal fault and a reverse fault.
Label the fault plane, upthrown side, downthrown side and fault
scarp on both cross-sections.
- What is a transcurrent fault and what are some of the ways
it might be expressed on the land surface?
- Describe the global pattern of earthquake occurrence and discuss
how this is related to plate tectonics.
- Describe the cause and behavior of a tsunami.
- How is the Richter used to characterize earthquakes?
- Use the example of the Hawaiian island volcanoes to explain
and illustrate the concept of a life cycle.
Go to this chapter's quiz
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