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Field and laboratory methods, developed to recover the record of past secular variations of geomagnetic declination and inclination carried by the remanent magnetization of some lake sediments, are described.

Type curves, delineating these parameters through post-Glacial time, have now been constructed for Europe and east-central N. These curves, once established for any region, are useful for dating lake sediments from that region.

The principal inclination features exhibited by the European curves can also be identified along the N.American curves with a delay of some 600 years, on average.This site stores nothing other than an automatically generated session ID in the cookie; no other information is captured.In general, only the information that you provide, or the choices you make while visiting a web site, can be stored in a cookie.For example, the site cannot determine your email name unless you choose to type it.Allowing a website to create a cookie does not give that or any other site access to the rest of your computer, and only the site that created the cookie can read it.