Chapter 2 – Instructor’s Manual
a. plates converge
b. higher density plate subducts
c. compression shortens crust, causing folding and thrust faulting
3. Transform boundaries
a. two plates slide past one another
C. Rates of plate motion
1. plate motion is a fast geologic process
2. few cm/yr (about as fast as fingernail or hair growth)
IV. A detailed look at seafloor spreading
A. Introduction
1. Wegener’s idea of continental drift lacked a solid mechanism for continental movement
a. seafloor spreading provided a mechanism for moving continents
B. Paleomagnetism
1. Definition
2. Magnetic field
a. Dipole magnetic field
3. Cooling volcanic rocks record prevailing magnetic polarity
5. What produces magnetic stripes?
6. Why is the seafloor no older than 200 million years?
a. age of ocean floors can be determined by magnetic patterns: youngest near ridges, older
C. Hot spots
1. volcanic centers from hot materials produced deep in mantle
2. as plate moves over hot spot, a chain of volcanoes is formed
a. Yellowstone volcanic region lies over a continental hotspot
V. Pangaea and present continents
A. Plate tectonics shapes continents and dictates the location of mountain ranges
1. The supercontinent of Pangaea