Magnetism leaves particles in molten metals lined up with north and south poles (magnetic poles, not the Earth's poles). Over time different layers of rock show that the N-S and S-N poles have switched, with S pointing in one direction and S pointing in a different direction depending on the age of the rock.
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.
It is Earths' "Magnetosphere".
No, the horizontal component of Earth's magnetic field is not equal at all places. It varies depending on the location and can be influenced by factors such as latitude, longitude, and local geological features.
Variations in the Earth's magnetic field can lead to shifts in the location and strength of the field, which can impact navigation systems like compasses. Changes in the magnetic field can also influence the behavior of charged particles in the Earth's magnetosphere, potentially affecting phenomena like the auroras.
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.
The molten iron and medals inside the earths core are the reasons for the earths magnetic core.
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
Magnetic Reversal
It is Earths' "Magnetosphere".
The amount of sunlight reaching a location at a particular time is determined by Earth's shape, axial tilt, rotation, and orbit around the sun. These factors affect the angle at which sunlight hits the Earth's surface, leading to variations in day length and intensity of sunlight throughout the year.
It is made by the movement of the earths core and magma field
The movements in the liquid inner core.
This is known as magnetic reversal when earth's magnetic poles change places.