Earths magnetic field Flashcards
magnetic iron binding minerals
magnetite (Fe3O4) and pyrrhotite (Fe1-xO)
magnetic field
- the earths magnetic field originates from liquid outer core (this acts as a geodynamo generating electric currents)
- align with the earths field
- used in navigation (lodestone)
Seismology
reveals a liquid outer core made mainly of iron
Geodynamo
- electrical current causes a magnetic field
- outer core convection combined with the earths spin creates helical flow and sustains magnetic field and electrical currents
disruptions to the magnetic field
Magnetic field reversals
Magnetic storms
- can disrupt field strength (can cause power supple problems)
- can disrupt global navigation satellite system (GPS)
- cause aurora (northern lights)
- normally short lived. sun spot may cause increase in magnetic storms
Palaeomagnetism
Remanent magnetism in ancient rocks recording the direction and strength of the earths magnetic field at the time of the rocks formation
- when magma cools below curie point magnetic iron-bearing minerals align with the earths magnetic field
Polar Wandering
- 1950s: discovered that magnetism of ancient rocks showed different orientations from the present magnetic field
- magnetic poles apparently moved. the apparent movement was called polar wandering. different continents had different paths.
Plate tectonic reconstructions
- by looking at the remanent magnetisation of ancient rock we can model where these rocks formed relative to the earths magnetic field.
- this can tell us the latitude of where the rock formed but not the longitude
Magnetic field reversals
- these occur infrequently from 10,000 to millions of years apart
- field strength decays to 10-30% of normal field
- reversal may take 10s to 100s years
- this can be used to set up magnetic timescale with periods of normal and reverse polarity
Seafloor spreading
- geomagnetism and the ocean floor
- symmetrical magnetic anomalies in the ocean (give dates fir the age if the crust)
- ocean lithosphere consists of upper mantle and the ocean crust
- oceans form by adding material symmetrically on either side of the mid ocean ridge
Summary
- magnetic minerals within igneous rocks align with the earths magnetic field as the rocks cools and solidifies
- ancient rocks on continents often have remanent magnetism that is different to the magnetic field of their current location
- this means that either the magnetic pole has moved or the continents have moved