The position of Earth's magnetic field changes over geologic time, pole is located near Earth's North Pole, a condition called normal polarity.
the earths magnetic signature is a negative polarity signature
in plate tectonics
The earths magnetic polarity at the time of rock formation.
Earth's magnetic orientation is locked into the rock when the rock cools
accorsing to the earths magnetic field
the earths magnetic signature is a negative polarity signature
in plate tectonics
The earths magnetic polarity at the time of rock formation.
Earths magnetic orientation is locked into the rock when the rock cools
Earths magnetic orientation is locked into the rock when the rock cools
There is no reason to believe that the Earth's magnetic field will change any time soon... or, for that matter, that anything extraordinary is going to happen in 2012.
Earths geographic North Pole is also currently a magnetic north pole. This is however not always the case because over geological time scales the Earth's magnetic poles flip as a result of changes of flow in Earth's molten core which produces Earth's magnetic field.
Earth's magnetic orientation is locked into the rock when the rock cools
accorsing to the earths magnetic field
In rock formed when the sea floor is being built, such as at the mid-Atlantic ridge, the minerals preserve the magnetic polarity. Since the flipping of the poles is fairly regular, the count of the bands can give a time.
compasses point to it. its at the north pole in the arcticNo It's not, the Magnetic North Pole is at this moment just off Ellesmere Island heading towards Russia at a rate of 40 miles (60 km) per year.AnswerIt depends what you mean by 'magnetic north pole'. If you mean the location, called 'Magnetic North' (arctic), then its polarity is south. If, by 'magnetic north pole', you mean its magnetic polarity, then it's located at Magnetic South (antarctic).
What escapes the crust is what we observe as the earths magnetic field. The outer core is a rotating mass of fluid metal that induces an electrical current which in turn generates the magnetosphere.