The circulation of electrical currents in the magma, roughly parallel to the Equator, causes the Earth's magnetic Field. There is also a few% derived from the flow of the Solar Wind - a flow of charged particles from the Sun. [The interior of the Earth is over 5000 deg C, and much too hot to maintain a magnet. see Curie Point.]
It is Earths' "Magnetosphere".
The geologist should consult academic journals, geological surveys, or other peer-reviewed publications related to geology to gather more information about the new discovery in his field. These sources are credible and provide in-depth insights on geological findings.
Earth's magnetic field is strongest at the magnetic North Pole and the magnetic South Pole.
When convection occurs in Earth's outer core, it generates electric currents due to the movement of the molten iron and nickel. These electric currents create a magnetic field around the planet, known as the Earth's magnetic field. This magnetic field plays a crucial role in protecting Earth from solar winds and cosmic rays.
The strength of Earth's magnetic field is strongest at the magnetic poles, which are not necessarily aligned with the geographic poles. The magnetic field is weakest at the magnetic equator.
Yes.
because it has the hydro electric power to control the earths magnetic field
magnetic field.
When you are not an expert in the field being studied in the experiment
The Earth's Iron Core
The core is a dense chunck of metal that influence the earths magnetic field.
It is made by the movement of the earths core and magma field
Mafic rocks in the mantle can contribute to Earth's magnetic field through the presence of minerals like magnetite that can become magnetized in aligning with the planet's magnetic field. However, the main driver of Earth's magnetic field is the movement of molten iron in the outer core.
First one is artificial where as the latter is natural We could increase or decrease the strength of magnetic field but we cannot vary earth's Intense field could be produced but earth's field is feeble in comparison with artificial
Yes, primary sources can sometimes be difficult to read due to factors such as old language, handwriting, or technical language specific to the time period or field. One may need additional context or background knowledge to fully understand the contents of a primary source.
It is Earths' "Magnetosphere".
The Earth's Magnetic field.