The geographical poles are still and never change position the slightest, whilst the magnetic poles are always changing their position, but only slightly.
No, Earth's magnetic poles and its geographic poles are not in the same place. The geographic poles are the points where Earth's axis of rotation intersects its surface, while the magnetic poles are where the planet's magnetic field lines converge and enter/exit the Earth. The magnetic poles are constantly moving and can deviate from the geographic poles.
True. The magnetic poles move constantly.
The geographic poles and magnetic poles of the Earth are different because they are determined by different factors. The geographic poles are the points on the Earth's surface where its axis of rotation intersects, while the magnetic poles are based on the Earth's magnetic field generated by its core. The movement of molten iron in the outer core creates the Earth's magnetic field, which can cause the magnetic poles to shift and not align perfectly with the geographic poles.
Only the magnetic poles wanderD.Earth's magnetic and geographic poles are generally not in the same place.Geographic poles are defined by Earth's rotation.
The Earth spins on its true or geographic poles, which are the points where the planet's axis of rotation intersects its surface. The magnetic poles, on the other hand, are where the Earth's magnetic field lines are perpendicular to its surface, and they do not coincide exactly with the geographic poles.
No, Earth's magnetic poles and its geographic poles are not in the same place. The geographic poles are the points where Earth's axis of rotation intersects its surface, while the magnetic poles are where the planet's magnetic field lines converge and enter/exit the Earth. The magnetic poles are constantly moving and can deviate from the geographic poles.
A compass needle points to the magnetic poles, which are not the same as the geographic poles. There is nothing special about the magnetic field at the geographic poles.
True. The magnetic poles move constantly.
The geographic poles and magnetic poles of the Earth are different because they are determined by different factors. The geographic poles are the points on the Earth's surface where its axis of rotation intersects, while the magnetic poles are based on the Earth's magnetic field generated by its core. The movement of molten iron in the outer core creates the Earth's magnetic field, which can cause the magnetic poles to shift and not align perfectly with the geographic poles.
Only the magnetic poles wanderD.Earth's magnetic and geographic poles are generally not in the same place.Geographic poles are defined by Earth's rotation.
The Earth spins on its true or geographic poles, which are the points where the planet's axis of rotation intersects its surface. The magnetic poles, on the other hand, are where the Earth's magnetic field lines are perpendicular to its surface, and they do not coincide exactly with the geographic poles.
There are two types of global poles; magnetic and geographic. Neither were invented. The magnetic poles are two points on the Earth where the magnetic field is most intense. The geographic poles are the northernmost and southernmost positions on the globe.
2 geographic and magnetic
The geographic poles are the points where the Earth's axis of rotation intersects its surface, while the geomagnetic poles are where the Earth's magnetic field lines are perpendicular to the surface. The geographic poles are fixed, while the geomagnetic poles move due to changes in the Earth's magnetic field.
The Earth's magnetic poles do not align perfectly with the geographic North and South poles due to the planet's molten iron core generating a magnetic field that is not perfectly symmetrical. This causes the magnetic poles to shift and be slightly off from the true geographic poles.
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.
this is because the concentration of domains is greater at poles as compared to inside of magnet