magnetosphere
The region of the Earth's magnetic field is called the magnetosphere. It extends far into space and protects the Earth from solar wind particles and cosmic radiation. The magnetosphere is created by the interaction between the Earth's magnetic field and the solar wind.
It is Earths' "Magnetosphere".
Earth's magnetic field is strongest at the magnetic North Pole and the magnetic South Pole.
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.
Earth's magnetic field is strongest near the poles, specifically in the region known as the Magnetic North Pole in the Arctic. It is slightly weaker at the Magnetic South Pole in the Antarctic. The strength of the magnetic field diminishes as you move towards the equator.
Earth's south magnetic field is a region near the geographic South Pole where the magnetic field lines are directed towards the Earth's core. It plays a crucial role in guiding compass needles and protecting the planet from solar wind. This field also influences the auroras in the Southern Hemisphere.
It is Earths' "Magnetosphere".
It is made by the movement of the earths core and magma field
Yes.
The earths magnetic field results from deep in the earths core. Magnetic conduction from within the earths core is believed to be the cause of this.
because it has the hydro electric power to control the earths magnetic field
magnetosphere i had to do this for school in 6th grade
earths magnetic field is generated by the circulation of liquid metal.
A Magnetic Force
It is Earths' "Magnetosphere".
Magnetic freild
= An effect of the magnetic field is "Van Allen radiation belt" =
No, the Earth's magnetic field does not cause the Earth to tilt. The tilt of the Earth's axis, also known as obliquity, is believed to have been caused by the gravitational influence of other planets during the early formation of the solar system. The Earth's magnetic field is generated by the movement of molten iron in its outer core.