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Detailed File Information |
Description
The table contains data for magnetic polarities of 6 rock samples taken in New Mexico. These rocks act as a storage device for magnetic field data because they can record the strength and direction of the magnetic field at the time of their formation. They are able to record the magnetic information after the rocks cool below a temperature called the Curie Temperature. The data in the table shows evidence that the magnetic field has reversed throughout history. |
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Geological Age Range and Timescale 0.71 - 1.04 Ma, Pleistocene |
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Location United States, New Mexico |
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Instructions Using the age of the rocks, can you figure out how long it took the magnetic field to reverse? |
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Keywords ERESE, magnetic field reversal data table, magnetic polarity data, magnetic field ages |
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Copyright Owner Enduring Resources for Earth Science Education (ERESE) |
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