Earth's Internal Structure: Earth Magnetism (2.3.4) Flashcards
What is the Earth’s dipole magnetic field?
- Earth possesses magnetic field approximating to dipole magnet.
- Magnetic force field a vector quantity with magnitude and direction.
- Location of Magnetic North Pole wanders with time, not same ass True North Pole.
What is declination and inclination?
Declination: horizontal direction (compass bearing).
Inclination: vertical direction/dip (not measured on compass).
Inclination of magnetic field is a function of latitude on Earth. Tangent (magnetic included) = ?x tangent (latitude).
2x
What is intensity?
Earth’s magnetic field intensity (strength) varies across planet.
What is the geodynamo theory?
- Self-exciting dynamo: proposed mechanism by which Earth generates magnetic field.
- Electrical currents flowing in slowly moving molten iron generates magnetic field.
- Shows how rotating, convecting, electrically conducting fluid maintains magnetic field over geological time scales.
- Implication of theory is that Earth’s magnetic field is dynamic and changes through time.
Convection cells carrying heat out core are?
Unstable.
Why is the iron composition of the core important?
- Required for magnetic field.
- Density and seismic velocity consistent.
- High enough cosmic abundance.
What are magnetic reversals?
- Complex fluid dynamics of convecting metal outer core leads to instabilities in magnetic field.
- May ‘flip’ field direction.
- Settles into new reversed state for some time, then repeats.
What is remanent magnetism/palaeomagnetism?
Field direction may be recorded by rocks. Magnetic minerals in rock respond to Earth’s magnetic field.
What are magnetic anomalies?
- Local measurement of magnetic field intensity may be stronger/weaker than expected regional field due to deep Earth.
- Caused by local remanent magnetisation of nearby rocks in crust.
- Positive anomaly if magnetic field of rocks is in same direction as current field.
What are the magnetic reversals in rock/time period?
- Each layer preserves record of magnetic field.
- Radiometric dating used to determine rock age.
- Palaeomagnetic measurements reveal Earth’s magnetic field changed direction in geologic past.
- Present magnetic field termed Normal while reversed is Reversed.