point in the Arctic at which Earth's magnetic field points vertically downwards, at 86°N 175°E in the Arctic Ocean as of 2019
Location of the north magnetic pole and the north geomagnetic pole in 2017. The magnetic-north of the earth as a magnet is actually on the southern hemisphere: The north side of magnets are by definition attracted to the magnetic south pole (which is the one in the geographic north), and opposite poles attract.
The north magnetic pole, also known as the magnetic north pole, is a point on the surface of Earth's Northern Hemisphere at which the planet's magnetic field points vertically downward (in other words, if a magnetic compass needle is allowed to rotate in three dimensions, it will point straight down). There is only one location where this occurs, near (but distinct from) the geographic north pole. The Earth's magnetic north pole is actually considered the "south pole" in terms of a typical magnet, meaning that the north pole of a magnet would be attracted to the Earth's magnetic north pole.
Discovered by embedding cosine similarity (sentence-transformers MiniLM, 384-dim).