| Abstract: | A heating mechanism for the enhancement of the magnetic susceptibility of soils on archaeological sites is assumed. Data for the iron oxide concentration which is available for conversion to the strongly ferrimagnetic form is presented for soils derived from a wide range of geological strata. These data are then used, in conjunction with the concept of the fractional conversion of the iron oxide that has occurred as a result of fires associated with human habitation, to explain the wide range of soil susceptibilities observed on archaeological sites. The feasibility of employing magnetic surveying techniques for the location of buried features on archaeological sites, situated on the different geological strata, is then discussed. |
