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Lecture 10

EATS1010 - The Dynamic Earth and Space Geodesy Lecture 10

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Department
Earth, Space Science and Engineering
Course
ESSE 1010
Professor
Gary Jarvis
Semester
Fall

Description
Lecture 10 Above the T ,cThe Curie Temperature, magnetic minerals (e.g. magnetite) lose their magnetic properties (atomic dipoles become randomized, no longer lined up). T c 500°C for magnetite Only within 20km (too hot past that depth) of the earth’s interior are the rocks permanently magnetic, called the magnetized layer. This still isn’t enough magnetism to account for earth’s dipole field. There is a large steel current flowing within the planet. Iron and nickel are very good at conducting electricity and is rich in the core of the Earth. The current flow (electric current) is the highest contributing reason for earth’s dipole field. 4 x 10 Amps of electric current in the core, particularly in the liquid outer core. Secular Variations of the Earth’s magnetic field • Rapid variations in direction and magnitude of B in historic time.
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