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Commissions have been received from the New York Philharmonic, Cleveland Orchestra, Atlanta Symphony Orchestra, Minnesota Orchestra, Dallas Symphony Orchestra, The Houston Symphony and St.
Archaeomagnetic dating was described in the 1992 publication “Paleomagnetism: Magnetic Domains to Geologic Terranes.” By Robert F. Archaeomagnetic dating requires an undisturbed feature that has a high likelihood of containing a remnant magnetic moment from the last time it had passed through the Curie point.
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The stronger component known as the Earth's poles, reverses direction at irregular intervals.
The weaker variations are the Earth's magnetic map.
Data from this feature is compared to the regional secular variation curve in order to determine the best-fit date range for the feature's last firing event.