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Description
Paleomagnetism tells us a lot about how the Earth's magnetic field has behaved in the past, and some of these results are discussed in Unit 23. Now for something completely different. As far as w...e know, the only viable theory for the origin of the magnetic field is motions in the earth's core. But is such a mechanism feasible? Obviously, we can't find out what the motions in the earth's core are like, but we think that the actions in the earth's core are something like a dynamo, and what we can do is build a model of this.
Metadata describing this Open University video programme
Module code and title: S100, Science foundation course
Item code: S100; 23
Recording date: 1971-02-08
Recording location: Alexandra Palace, London
First transmission date: 1971-07-04
Published: 1971
Rights Statement: Rights owned or controlled by The Open University
Restrictions on use: This material can be used in accordance with The Open University conditions of use. A link to the conditions can be found at the bottom of all OUDA web pages.
Duration: 00:23:58
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Director: Penny Crompton
Producer: Nat Taylor
Contributors: Michael Pentz; Peter Smith; Rod L.Wilson; Frank J. Lowes
Publisher: Open University
Subject terms: Paleomagnetism; Geomagnetism; Geodynamics; Dynamo theory (Cosmic physics); Earth (Planet)--Internal structure; Earth (Planet)--Core
Production number: JOUZ378D
Videofinder number: 2851
Available to public: no