(Click on the image to view a larger version in a new window.)
Earth’s magnetic field in 1945. The contours are lines of equal inclination of the geomagnetic field; the locations of the magnetic poles are indicated by plus signs (Mercator projection). The magnetic field varies with latitude and, to a lesser degree, longitude.
(Butler, R. F. (1992) Paleomagnetism: Magnetic Domains to Geologic Terranes, Blackwell Scientific Publications, Boston. Available at http://www.geo.arizona.edu/Paleomag/book/)
Home ||
Contact Us ||
Orders/Returns ||
List by Author
List by Subject Area ||
List by Title ||
View Exam Copies Requested