it is the angle at which the compass will drift
ferromagnetic.
Yes, "drift" can be a noun. It can refer to a gradual shifting or moving from an original position or course.
No, "drift" is not an onomatopoeia. An onomatopoeia is a word that imitates the sound it represents, such as "buzz" or "whoosh." "Drift" is a verb that describes the movement of something slowly and gradually.
A Magnetic Force
Gold is not magnetic as it is a diamagnetic material, meaning it does not have a magnetic field of its own and is not attracted to magnets.
causes of magnetic drift causes of magnetic drift causes of magnetic drift
Magnetic drift can be caused by changes in the Earth's magnetic field, variations in the solar wind interacting with the Earth's magnetosphere, and disturbances in the ionosphere. Other factors like geological processes and human-made magnetic fields can also contribute to magnetic drift.
temporarily magnetic
No, the Earth's magnetic poles are not responsible for continental drift. Continental drift is primarily driven by the movement of tectonic plates in the Earth's lithosphere. The Earth's magnetic field does play a role in plate tectonics through magnetic stripes on the ocean floor, but it is not the primary cause of continental drift.
Magnetic Reversals
Magnetic Reversals
ferromagnetic.
Scientists use the magnetic properties of some minerals as evidence of past changes in Earth's magnetic field. These changes can provide insight into the Earth's geological history, including continental drift and past climates.
The term for the apparent tendency of the north magnetic pole to vary in position over time is magnetic pole drift or magnetic pole wander.
Kazuo Kitao has written: 'Effect of magnetic curvature on density gradient drift instabilities' -- subject(s): Magnetic fields, Plasma instabilities
Cox contributed to continental drift theory by researching and proving that the seafloor spreads and that the Earth has experienced magnetic reversals. He did this by studying the layers of volcanoes and streambeds.
Periodically, the magnetic field of the earth reverses polarity. The direction of the magnetic field is recorded in the magnetic properties of rocks when they are erupted. Rocks are being continuously added at sea floor spreading regions, and thus the magnetic reversals are recorded as pairs of parallel 'stripes' alongside the mid ocean spreading ridge.