Late Quaternary secular variation of geomagnetic declination in western New York

Details Late Quaternary secular variation of geomagnetic declination in western New York Late Quaternary secular variation of geomagnetic declination in western New York

Oct 1984

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1984e%26psl..70..363b&link_type=abstract

Earth and Planetary Science Letters, Volume 70, Issue 2, p. 363-372.

Computer Science

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Scientific paper

A secular variation record of the geomagnetic declination has been obtained from glaciolacustrine varved clays and postglacial sediments, sampled both from outcrop and from piston cores from Lake Ontario. It appears to be uninterrupted and covers the interval 14,000 years B.P. (14C) to the present. The record for the interval 14,000-12,300 years B.P. consists of true declination and was obtained from samples collected from outcrop. The record for the interval 12,500 + years B.P. to the present consists of relative declination and was obtained from piston cores. The secular variation record is internally consistent and is compatible with the chronology of events known to have occurred during and following the deglaciation of western New York. Use of the record for magnetic correlation within the study area is demonstrated.

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