The Curie temperature for iron is reached at about 20 km depth in the Earth, and the temperature is much higher at the outer boundary of the Earth's core so that the iron there is no longer ferromagnetic (the electron spins in the iron can no longer align). This demonstration will help students understand the magnetic field of the Earth, and can help explain the variation of the direction of the field through time (the secular variation), the non-dipole field, and the fact that the field reverses its direction periodically (polarity reversals). Educational levels: High school, Middle school, Undergraduate lower division
Principally new model of the magnetic field of the Hot Earth is proposed. Unlike the commonly accept...
The document is meant to act as a resource for elementary through middle school teachers, featuring ...
This Web site provides an illustrated, non-mathematical introduction to the magnetism of the Earth, ...
This demonstration of the magnetic field lines of Earth uses a bar magnet, iron filings, and a compa...
SIGLEAvailable from British Library Document Supply Centre- DSC:D061292 / BLDSC - British Library Do...
In laboratory experiments, we heated chondritic material up to 1400 K in a hydrogen atmosphere. Möss...
The Earth’s magnetic field is generated in the fluid region deep inside the Earth. Heat convection, ...
This teacher's guide contains four lessons that provide a way for teachers to introduce students to ...
The magnetic field of the Earth is contained in a region called the magnetosphere. The magnetosphere...
In forming any theory of the cause of terrestrial magnetism, the first question that arises is wheth...
[1] Curie point temperatures (TC) of natural and synthetic magnetic materials are commonly determine...
This demonstration shows how the Earth's magnetic field has flipped (the N pole becoming the S pole,...
In this activity students learn about Earth's magnetic reversals by reading two fiction stories and ...
Why do typical magnetic metals and oxides have different Curie temperatures (TC)? For example, TC = ...
This brief explanation of the Earth's magnetosphere starts with the work of Kristian Birkeland, a No...
Principally new model of the magnetic field of the Hot Earth is proposed. Unlike the commonly accept...
The document is meant to act as a resource for elementary through middle school teachers, featuring ...
This Web site provides an illustrated, non-mathematical introduction to the magnetism of the Earth, ...
This demonstration of the magnetic field lines of Earth uses a bar magnet, iron filings, and a compa...
SIGLEAvailable from British Library Document Supply Centre- DSC:D061292 / BLDSC - British Library Do...
In laboratory experiments, we heated chondritic material up to 1400 K in a hydrogen atmosphere. Möss...
The Earth’s magnetic field is generated in the fluid region deep inside the Earth. Heat convection, ...
This teacher's guide contains four lessons that provide a way for teachers to introduce students to ...
The magnetic field of the Earth is contained in a region called the magnetosphere. The magnetosphere...
In forming any theory of the cause of terrestrial magnetism, the first question that arises is wheth...
[1] Curie point temperatures (TC) of natural and synthetic magnetic materials are commonly determine...
This demonstration shows how the Earth's magnetic field has flipped (the N pole becoming the S pole,...
In this activity students learn about Earth's magnetic reversals by reading two fiction stories and ...
Why do typical magnetic metals and oxides have different Curie temperatures (TC)? For example, TC = ...
This brief explanation of the Earth's magnetosphere starts with the work of Kristian Birkeland, a No...
Principally new model of the magnetic field of the Hot Earth is proposed. Unlike the commonly accept...
The document is meant to act as a resource for elementary through middle school teachers, featuring ...
This Web site provides an illustrated, non-mathematical introduction to the magnetism of the Earth, ...