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http://www.thisoldearth.net/Geology_Online-1_Subchapters.cfm?Chapter=3&Row=4
Depiction of rock layers showing normal and reversed polarityIn the early 1950s Patrick Blankett thought he could use paleomagnetism to finally prove the theory of Continental Drift. All he would have to do is gather paleomagnetic data from rocks of known ages and he could show how the continents did indeed move across the earth.
https://www.answers.com/Q/How_does_the_theory_of_paleomagnetism_support_the_continental_drift
The study of Paleomagnetism is what finally proved Alfred Wegner's theory of continental drift. Paleomagnetism in short discovered identical polarities on either side of the mid-Atlantic ridge. As Earth's magnetic poles switch, more polarities are added to both sides of the ridge.
https://geologylearn.blogspot.com/2016/02/paleomagnetism-and-proof-of-continental.html
An understanding of paleomagnetism provided proof of continental drift and, contributed to the development of plate tectonics theory. As a foundation for introducing paleomagnetism, we first provide additional detail about the basic nature of the Earth’s magnetic field.
https://link.springer.com/referenceworkentry/10.1007/3-540-31080-0_15
Paleomagnetism is the study of the ancient magnetic field of both rocks and the Earth as a whole. Paleomagnetism has provided very strong quantitative evidence for polar wander and continental drift. It is interesting to note, however, that although this evidence was published in the late 1950s, the concept of continental drift did not gain widespread acceptance until the mid-1960s.
https://study.com/academy/lesson/paleomagnetism-and-hot-spot-evidence-for-plate-tectonics.html
Paleomagnetism is the study of the earth's past magnetic field. It may help you to recall this term if you remember that it is the combination of two words: 'paleo,' which means ancient, and 'magnetism,' which means exhibiting a magnetic field.
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