Direction of magnetic field Figure 3.27 Particles of iron-bearing magnetite occur naturally in basaltic magma. As this rock forms new sea- bed, the magnetic particles cool, "locking" their mag- netic orientation to that of Earths prevailing magnetic field. If Earths magnetic field changes direction later, the "locked" particles will not respond, but magnetic Particles in magma -These can move particles in any new (hot) magma above will orient to the new field direction. -These cannot move Particles in rigid rock Magnetic particles Cengage Learning

Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
Section: Chapter Questions
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Can you explain the matching magnetic alignments seen south of Iceland (as shown)?

Direction of
magnetic field
Figure 3.27 Particles of iron-bearing magnetite occur
naturally in basaltic magma. As this rock forms new sea-
bed, the magnetic particles cool, "locking" their mag-
netic orientation to that of Earths prevailing magnetic
field. If Earths magnetic field changes direction later,
the "locked" particles will not respond, but magnetic
Particles in
magma
-These can move
particles in any new (hot) magma above will orient to
the new field direction.
-These cannot move
Particles in
rigid rock
Magnetic particles
Cengage Learning
Transcribed Image Text:Direction of magnetic field Figure 3.27 Particles of iron-bearing magnetite occur naturally in basaltic magma. As this rock forms new sea- bed, the magnetic particles cool, "locking" their mag- netic orientation to that of Earths prevailing magnetic field. If Earths magnetic field changes direction later, the "locked" particles will not respond, but magnetic Particles in magma -These can move particles in any new (hot) magma above will orient to the new field direction. -These cannot move Particles in rigid rock Magnetic particles Cengage Learning
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